Wiki2Web Studio

Create complete, beautiful interactive educational materials in less than 5 minutes.

Print flashcards, homework worksheets, exams/quizzes, study guides, & more.

Export your learner materials as an interactive game, a webpage, or FAQ style cheatsheet.

Unsaved Work Found!

It looks like you have unsaved work from a previous session. Would you like to restore it?


Atmospheric Pressure: Fundamentals, Variations, and Applications

At a Glance

Title: Atmospheric Pressure: Fundamentals, Variations, and Applications

Total Categories: 4

Category Stats

  • Defining Atmospheric Pressure and Units: 13 flashcards, 22 questions
  • Altitude-Dependent Pressure Dynamics: 18 flashcards, 25 questions
  • Global and Regional Pressure Extremes and Variations: 12 flashcards, 18 questions
  • Applied Meteorology and Engineering: 11 flashcards, 11 questions

Total Stats

  • Total Flashcards: 54
  • True/False Questions: 38
  • Multiple Choice Questions: 38
  • Total Questions: 76

Instructions

Click the button to expand the instructions for how to use the Wiki2Web Teacher studio in order to print, edit, and export data about Atmospheric Pressure: Fundamentals, Variations, and Applications

Welcome to Your Curriculum Command Center

This guide will turn you into a Wiki2web Studio power user. Let's unlock the features designed to give you back your weekends.

The Core Concept: What is a "Kit"?

Think of a Kit as your all-in-one digital lesson plan. It's a single, portable file that contains every piece of content for a topic: your subject categories, a central image, all your flashcards, and all your questions. The true power of the Studio is speed—once a kit is made (or you import one), you are just minutes away from printing an entire set of coursework.

Getting Started is Simple:

  • Create New Kit: Start with a clean slate. Perfect for a brand-new lesson idea.
  • Import & Edit Existing Kit: Load a .json kit file from your computer to continue your work or to modify a kit created by a colleague.
  • Restore Session: The Studio automatically saves your progress in your browser. If you get interrupted, you can restore your unsaved work with one click.

Step 1: Laying the Foundation (The Authoring Tools)

This is where you build the core knowledge of your Kit. Use the left-side navigation panel to switch between these powerful authoring modules.

⚙️ Kit Manager: Your Kit's Identity

This is the high-level control panel for your project.

  • Kit Name: Give your Kit a clear title. This will appear on all your printed materials.
  • Master Image: Upload a custom cover image for your Kit. This is essential for giving your content a professional visual identity, and it's used as the main graphic when you export your Kit as an interactive game.
  • Topics: Create the structure for your lesson. Add topics like "Chapter 1," "Vocabulary," or "Key Formulas." All flashcards and questions will be organized under these topics.

🃏 Flashcard Author: Building the Knowledge Blocks

Flashcards are the fundamental concepts of your Kit. Create them here to define terms, list facts, or pose simple questions.

  • Click "➕ Add New Flashcard" to open the editor.
  • Fill in the term/question and the definition/answer.
  • Assign the flashcard to one of your pre-defined topics.
  • To edit or remove a flashcard, simply use the ✏️ (Edit) or ❌ (Delete) icons next to any entry in the list.

✍️ Question Author: Assessing Understanding

Create a bank of questions to test knowledge. These questions are the engine for your worksheets and exams.

  • Click "➕ Add New Question".
  • Choose a Type: True/False for quick checks or Multiple Choice for more complex assessments.
  • To edit an existing question, click the ✏️ icon. You can change the question text, options, correct answer, and explanation at any time.
  • The Explanation field is a powerful tool: the text you enter here will automatically appear on the teacher's answer key and on the Smart Study Guide, providing instant feedback.

🔗 Intelligent Mapper: The Smart Connection

This is the secret sauce of the Studio. The Mapper transforms your content from a simple list into an interconnected web of knowledge, automating the creation of amazing study guides.

  • Step 1: Select a question from the list on the left.
  • Step 2: In the right panel, click on every flashcard that contains a concept required to answer that question. They will turn green, indicating a successful link.
  • The Payoff: When you generate a Smart Study Guide, these linked flashcards will automatically appear under each question as "Related Concepts."

Step 2: The Magic (The Generator Suite)

You've built your content. Now, with a few clicks, turn it into a full suite of professional, ready-to-use materials. What used to take hours of formatting and copying-and-pasting can now be done in seconds.

🎓 Smart Study Guide Maker

Instantly create the ultimate review document. It combines your questions, the correct answers, your detailed explanations, and all the "Related Concepts" you linked in the Mapper into one cohesive, printable guide.

📝 Worksheet & 📄 Exam Builder

Generate unique assessments every time. The questions and multiple-choice options are randomized automatically. Simply select your topics, choose how many questions you need, and generate:

  • A Student Version, clean and ready for quizzing.
  • A Teacher Version, complete with a detailed answer key and the explanations you wrote.

🖨️ Flashcard Printer

Forget wrestling with table layouts in a word processor. Select a topic, choose a cards-per-page layout, and instantly generate perfectly formatted, print-ready flashcard sheets.

Step 3: Saving and Collaborating

  • 💾 Export & Save Kit: This is your primary save function. It downloads the entire Kit (content, images, and all) to your computer as a single .json file. Use this to create permanent backups and share your work with others.
  • ➕ Import & Merge Kit: Combine your work. You can merge a colleague's Kit into your own or combine two of your lessons into a larger review Kit.

You're now ready to reclaim your time.

You're not just a teacher; you're a curriculum designer, and this is your Studio.

This page is an interactive visualization based on the Wikipedia article "Atmospheric pressure" (opens in new tab) and its cited references.

Text content is available under the Creative Commons Attribution-ShareAlike 4.0 License (opens in new tab). Additional terms may apply.

Disclaimer: This website is for informational purposes only and does not constitute any kind of advice. The information is not a substitute for consulting official sources or records or seeking advice from qualified professionals.


Owned and operated by Artificial General Intelligence LLC, a Michigan Registered LLC
Prompt engineering done with Gracekits.com
All rights reserved
Sitemaps | Contact

Export Options





Study Guide: Atmospheric Pressure: Fundamentals, Variations, and Applications

Study Guide: Atmospheric Pressure: Fundamentals, Variations, and Applications

Defining Atmospheric Pressure and Units

Atmospheric pressure is exclusively caused by the planet's rotation, with gravitational attraction playing a minor role.

Answer: False

Atmospheric pressure is fundamentally caused by the gravitational attraction of the planet on its atmospheric gases, while planetary rotation is a modifying factor, not the exclusive cause.

Related Concepts:

  • What are the fundamental causes of atmospheric pressure?: The fundamental cause of atmospheric pressure is the gravitational attraction exerted by the planet on its atmospheric gases. This pressure is a complex function of the planet's mass, surface radius, the total quantity and composition of atmospheric gases, and their vertical distribution.
  • What local and planetary factors can modify atmospheric pressure?: Atmospheric pressure can be modified by planetary rotation and local effects such as wind velocity, variations in density due to temperature changes, and variations in the composition of the atmospheric gases.

The standard atmosphere (atm) is defined as 101,325 Pascals, which is equivalent to 760 millimeters of mercury.

Answer: True

The standard atmosphere (atm) is indeed defined as 101,325 Pascals and is equivalent to 760 millimeters of mercury, among other units.

Related Concepts:

  • How is the standard atmosphere (atm) unit defined, and what are its common equivalents?: The standard atmosphere (atm) is a unit of pressure defined as 101,325 Pascals (Pa). It is equivalent to 1,013.25 hectopascals (hPa), 1,013.25 millibars, 760 millimeters of mercury (mmHg), 29.9212 inches of mercury (inHg), or 14.696 pounds per square inch (psi). This unit serves as a fundamental reference for atmospheric pressure.
  • What is the approximate atmospheric pressure at mean sea level on Earth?: The Earth's atmospheric pressure at mean sea level is approximately 1 standard atmosphere (atm), which translates to roughly 101,325 Pascals or 1,013.25 hectopascals.

The SI unit for pressure is the Pascal, defined as one newton per square meter.

Answer: True

The Pascal (Pa) is the SI unit for pressure, defined as one newton per square meter (1 N/m²).

Related Concepts:

  • What are the SI units for pressure, and how is pressure defined in these units?: The International System of Units (SI) for pressure is the Pascal (Pa). One Pascal is defined as one newton per square meter (1 N/m²), representing force applied perpendicularly to a surface per unit area.
  • How is the standard atmosphere (atm) unit defined, and what are its common equivalents?: The standard atmosphere (atm) is a unit of pressure defined as 101,325 Pascals (Pa). It is equivalent to 1,013.25 hectopascals (hPa), 1,013.25 millibars, 760 millimeters of mercury (mmHg), 29.9212 inches of mercury (inHg), or 14.696 pounds per square inch (psi). This unit serves as a fundamental reference for atmospheric pressure.

A column of air with a cross-sectional area of 1 square inch at mean sea level exerts a pressure of approximately 14.7 pounds per square inch (psi).

Answer: True

A column of air with a cross-sectional area of 1 square inch at mean sea level exerts a weight of about 14.7 pounds-force, resulting in a pressure of 14.7 psi.

Related Concepts:

  • What is the approximate weight and pressure exerted by a column of air with a cross-sectional area of 1 square inch?: A column of air with a cross-sectional area of 1 square inch (in²) would have a weight of about 14.7 pounds-force (lbf), resulting in a pressure of 14.7 lbf/in² (pounds per square inch).
  • What is the approximate mass and force exerted by a column of air with a cross-sectional area of 1 square centimeter at mean sea level?: On average, a column of air with a cross-sectional area of 1 square centimeter (cm²) from mean sea level to the top of Earth's atmosphere has a mass of about 1.03 kilograms and exerts a force or 'weight' of approximately 10.1 newtons. This results in a pressure of 10.1 N/cm² or 101 kilopascals (kPa).

Surface pressure is directly proportional to the total mass of air situated above a particular location.

Answer: True

Surface pressure is directly proportional to the total mass of the air column situated vertically above that particular location, as described by the formula P = (m*g)/A.

Related Concepts:

  • What is surface pressure, and what is it directly proportional to?: Surface pressure refers to the atmospheric pressure at a specific point on Earth's surface, whether land or ocean. It is directly proportional to the total mass of the air column situated vertically above that particular location.
  • What is the relationship between pressure, mass, and acceleration due to gravity?: The relationship between pressure (P), mass (m), and acceleration due to gravity (g) is expressed by the formula P = F/A = (m*g)/A, where F is force and A is the surface area. This equation highlights that atmospheric pressure is equivalent to the weight per unit area of the atmospheric mass above a given point.

The average value of surface pressure on Earth is 1,013.25 hPa, which is identical to the mean sea-level pressure in the International Standard Atmosphere.

Answer: False

The average value of surface pressure on Earth is approximately 985 hPa, which differs from the theoretical mean sea-level pressure of 1,013.25 hPa in the International Standard Atmosphere.

Related Concepts:

  • What is the average value of surface pressure on Earth, and how does it compare to mean sea-level pressure in the International Standard Atmosphere?: The global average surface pressure on Earth is approximately 985 hPa. This differs from the mean sea-level pressure in the International Standard Atmosphere (ISA), which is a theoretical 1,013.25 hPa (1 atmosphere or 29.92 inches of mercury), as MSLP involves a standardized extrapolation to sea level for all locations.
  • What is the approximate atmospheric pressure at mean sea level on Earth?: The Earth's atmospheric pressure at mean sea level is approximately 1 standard atmosphere (atm), which translates to roughly 101,325 Pascals or 1,013.25 hectopascals.
  • How is the standard atmosphere (atm) unit defined, and what are its common equivalents?: The standard atmosphere (atm) is a unit of pressure defined as 101,325 Pascals (Pa). It is equivalent to 1,013.25 hectopascals (hPa), 1,013.25 millibars, 760 millimeters of mercury (mmHg), 29.9212 inches of mercury (inHg), or 14.696 pounds per square inch (psi). This unit serves as a fundamental reference for atmospheric pressure.

Pressure, mass, and acceleration due to gravity are related by the formula P = (m*g)/A, where A is the surface area.

Answer: True

The formula P = (m*g)/A correctly expresses the relationship between pressure, mass, acceleration due to gravity, and surface area.

Related Concepts:

  • What is the relationship between pressure, mass, and acceleration due to gravity?: The relationship between pressure (P), mass (m), and acceleration due to gravity (g) is expressed by the formula P = F/A = (m*g)/A, where F is force and A is the surface area. This equation highlights that atmospheric pressure is equivalent to the weight per unit area of the atmospheric mass above a given point.

Atmospheric pressure is also known as air pressure or barometric pressure, with barometric pressure specifically referencing the barometer.

Answer: True

Atmospheric pressure is indeed known as air pressure or barometric pressure, with the latter term specifically referring to the use of a barometer for measurement.

Related Concepts:

  • What is atmospheric pressure, and what are its alternative names?: Atmospheric pressure, also known as air pressure or barometric pressure, is the force exerted by the Earth's atmosphere. The term 'barometric pressure' specifically refers to measurements made with a barometer.

The Earth's atmospheric pressure at mean sea level is approximately 101,325 hectopascals.

Answer: False

The Earth's atmospheric pressure at mean sea level is approximately 101,325 Pascals, which is equivalent to 1,013.25 hectopascals, not 101,325 hectopascals.

Related Concepts:

  • What is the approximate atmospheric pressure at mean sea level on Earth?: The Earth's atmospheric pressure at mean sea level is approximately 1 standard atmosphere (atm), which translates to roughly 101,325 Pascals or 1,013.25 hectopascals.
  • How is the standard atmosphere (atm) unit defined, and what are its common equivalents?: The standard atmosphere (atm) is a unit of pressure defined as 101,325 Pascals (Pa). It is equivalent to 1,013.25 hectopascals (hPa), 1,013.25 millibars, 760 millimeters of mercury (mmHg), 29.9212 inches of mercury (inHg), or 14.696 pounds per square inch (psi). This unit serves as a fundamental reference for atmospheric pressure.

In most situations, atmospheric pressure is closely approximated by the hydrostatic pressure, which is the pressure caused by the weight of the column of air directly above the measurement point.

Answer: True

Atmospheric pressure is closely approximated by the hydrostatic pressure, which is the pressure caused by the weight of the column of air directly above the measurement point.

Related Concepts:

  • How is atmospheric pressure generally approximated in most circumstances?: In most meteorological contexts, atmospheric pressure is accurately approximated by hydrostatic pressure, which is the pressure generated by the weight of the column of air directly above the measurement point. This principle is crucial for understanding pressure variations with altitude.
  • What is atmospheric pressure, and what are its alternative names?: Atmospheric pressure, also known as air pressure or barometric pressure, is the force exerted by the Earth's atmosphere. The term 'barometric pressure' specifically refers to measurements made with a barometer.

Which of the following is NOT an alternative name for atmospheric pressure mentioned in the source?

Answer: Environmental pressure

The source identifies 'air pressure' and 'barometric pressure' as alternative names for atmospheric pressure. 'Hydrostatic pressure' is a concept that approximates atmospheric pressure, but not an alternative name for it in the same sense. 'Environmental pressure' is not mentioned.

Related Concepts:

  • What is atmospheric pressure, and what are its alternative names?: Atmospheric pressure, also known as air pressure or barometric pressure, is the force exerted by the Earth's atmosphere. The term 'barometric pressure' specifically refers to measurements made with a barometer.

How many Pascals (Pa) are equivalent to one standard atmosphere (atm)?

Answer: 101,325 Pa

One standard atmosphere (atm) is defined as 101,325 Pascals (Pa).

Related Concepts:

  • How is the standard atmosphere (atm) unit defined, and what are its common equivalents?: The standard atmosphere (atm) is a unit of pressure defined as 101,325 Pascals (Pa). It is equivalent to 1,013.25 hectopascals (hPa), 1,013.25 millibars, 760 millimeters of mercury (mmHg), 29.9212 inches of mercury (inHg), or 14.696 pounds per square inch (psi). This unit serves as a fundamental reference for atmospheric pressure.
  • What is the approximate atmospheric pressure at mean sea level on Earth?: The Earth's atmospheric pressure at mean sea level is approximately 1 standard atmosphere (atm), which translates to roughly 101,325 Pascals or 1,013.25 hectopascals.
  • What are the SI units for pressure, and how is pressure defined in these units?: The International System of Units (SI) for pressure is the Pascal (Pa). One Pascal is defined as one newton per square meter (1 N/m²), representing force applied perpendicularly to a surface per unit area.

What is the approximate atmospheric pressure at mean sea level on Earth in hectopascals?

Answer: 1,013.25 hPa

The Earth's atmospheric pressure at mean sea level is approximately 1,013.25 hectopascals.

Related Concepts:

  • What is the approximate atmospheric pressure at mean sea level on Earth?: The Earth's atmospheric pressure at mean sea level is approximately 1 standard atmosphere (atm), which translates to roughly 101,325 Pascals or 1,013.25 hectopascals.
  • What is the average value of surface pressure on Earth, and how does it compare to mean sea-level pressure in the International Standard Atmosphere?: The global average surface pressure on Earth is approximately 985 hPa. This differs from the mean sea-level pressure in the International Standard Atmosphere (ISA), which is a theoretical 1,013.25 hPa (1 atmosphere or 29.92 inches of mercury), as MSLP involves a standardized extrapolation to sea level for all locations.
  • What is the average sea-level pressure, and what are its values in common units?: The average sea-level pressure is 1,013.25 hPa (hectopascals), which is equivalent to 29.921 inches of mercury (inHg) or 760.00 millimeters of mercury (mmHg). These values represent the standard atmospheric pressure at sea level.

What concept closely approximates atmospheric pressure in most situations?

Answer: Hydrostatic pressure, caused by the weight of the air column above.

In most situations, atmospheric pressure is closely approximated by the hydrostatic pressure, which is the pressure caused by the weight of the air column directly above the measurement point.

Related Concepts:

  • How is atmospheric pressure generally approximated in most circumstances?: In most meteorological contexts, atmospheric pressure is accurately approximated by hydrostatic pressure, which is the pressure generated by the weight of the column of air directly above the measurement point. This principle is crucial for understanding pressure variations with altitude.

What is the SI unit for pressure, and how is it defined?

Answer: Pascal (Pa), defined as 1 newton per square meter.

The SI unit for pressure is the Pascal (Pa), which is defined as one newton per square meter (1 N/m²).

Related Concepts:

  • What are the SI units for pressure, and how is pressure defined in these units?: The International System of Units (SI) for pressure is the Pascal (Pa). One Pascal is defined as one newton per square meter (1 N/m²), representing force applied perpendicularly to a surface per unit area.

What is the approximate mass of a column of air with a cross-sectional area of 1 square centimeter from mean sea level to the top of Earth's atmosphere?

Answer: 1.03 kilograms

A column of air with a cross-sectional area of 1 square centimeter from mean sea level to the top of Earth's atmosphere has an approximate mass of 1.03 kilograms.

Related Concepts:

  • What is the approximate mass and force exerted by a column of air with a cross-sectional area of 1 square centimeter at mean sea level?: On average, a column of air with a cross-sectional area of 1 square centimeter (cm²) from mean sea level to the top of Earth's atmosphere has a mass of about 1.03 kilograms and exerts a force or 'weight' of approximately 10.1 newtons. This results in a pressure of 10.1 N/cm² or 101 kilopascals (kPa).

What is the fundamental cause of atmospheric pressure?

Answer: The gravitational attraction of the planet on atmospheric gases.

Atmospheric pressure is fundamentally caused by the gravitational attraction of the planet on its atmospheric gases.

Related Concepts:

  • What are the fundamental causes of atmospheric pressure?: The fundamental cause of atmospheric pressure is the gravitational attraction exerted by the planet on its atmospheric gases. This pressure is a complex function of the planet's mass, surface radius, the total quantity and composition of atmospheric gases, and their vertical distribution.

Which of the following is NOT listed as a factor that can modify atmospheric pressure?

Answer: Ocean currents

The source lists planetary rotation, wind velocity, and variations in density due to temperature changes as factors that can modify atmospheric pressure, but not ocean currents.

Related Concepts:

  • What local and planetary factors can modify atmospheric pressure?: Atmospheric pressure can be modified by planetary rotation and local effects such as wind velocity, variations in density due to temperature changes, and variations in the composition of the atmospheric gases.

What is the average sea-level pressure in inches of mercury (inHg)?

Answer: 29.921 inHg

The average sea-level pressure is 29.921 inches of mercury (inHg).

Related Concepts:

  • What is the average sea-level pressure, and what are its values in common units?: The average sea-level pressure is 1,013.25 hPa (hectopascals), which is equivalent to 29.921 inches of mercury (inHg) or 760.00 millimeters of mercury (mmHg). These values represent the standard atmospheric pressure at sea level.
  • What is the average value of surface pressure on Earth, and how does it compare to mean sea-level pressure in the International Standard Atmosphere?: The global average surface pressure on Earth is approximately 985 hPa. This differs from the mean sea-level pressure in the International Standard Atmosphere (ISA), which is a theoretical 1,013.25 hPa (1 atmosphere or 29.92 inches of mercury), as MSLP involves a standardized extrapolation to sea level for all locations.
  • What is the approximate atmospheric pressure at mean sea level on Earth?: The Earth's atmospheric pressure at mean sea level is approximately 1 standard atmosphere (atm), which translates to roughly 101,325 Pascals or 1,013.25 hectopascals.

What is surface pressure directly proportional to?

Answer: The total mass of air situated above that particular location.

Surface pressure is directly proportional to the total mass of the air column situated vertically above that particular location.

Related Concepts:

  • What is surface pressure, and what is it directly proportional to?: Surface pressure refers to the atmospheric pressure at a specific point on Earth's surface, whether land or ocean. It is directly proportional to the total mass of the air column situated vertically above that particular location.
  • What is the relationship between pressure, mass, and acceleration due to gravity?: The relationship between pressure (P), mass (m), and acceleration due to gravity (g) is expressed by the formula P = F/A = (m*g)/A, where F is force and A is the surface area. This equation highlights that atmospheric pressure is equivalent to the weight per unit area of the atmospheric mass above a given point.

What is the average value of surface pressure on Earth?

Answer: 985 hPa

The average value of surface pressure on Earth is approximately 985 hPa.

Related Concepts:

  • What is the average value of surface pressure on Earth, and how does it compare to mean sea-level pressure in the International Standard Atmosphere?: The global average surface pressure on Earth is approximately 985 hPa. This differs from the mean sea-level pressure in the International Standard Atmosphere (ISA), which is a theoretical 1,013.25 hPa (1 atmosphere or 29.92 inches of mercury), as MSLP involves a standardized extrapolation to sea level for all locations.

What is the approximate force exerted by a column of air with a cross-sectional area of 1 square centimeter at mean sea level?

Answer: 10.1 Newtons

A column of air with a cross-sectional area of 1 square centimeter at mean sea level exerts a force of approximately 10.1 newtons.

Related Concepts:

  • What is the approximate mass and force exerted by a column of air with a cross-sectional area of 1 square centimeter at mean sea level?: On average, a column of air with a cross-sectional area of 1 square centimeter (cm²) from mean sea level to the top of Earth's atmosphere has a mass of about 1.03 kilograms and exerts a force or 'weight' of approximately 10.1 newtons. This results in a pressure of 10.1 N/cm² or 101 kilopascals (kPa).

Altitude-Dependent Pressure Dynamics

As elevation increases, atmospheric pressure generally increases due to a greater column of air above the measurement point.

Answer: False

Atmospheric pressure generally decreases with increasing elevation because there is less overlying atmospheric mass, not more.

Related Concepts:

  • How does atmospheric pressure change with increasing elevation?: As elevation increases, the mass of the overlying atmosphere diminishes, leading to a corresponding decrease in atmospheric pressure. This inverse relationship is a fundamental aspect of atmospheric physics.
  • How is atmospheric pressure generally approximated in most circumstances?: In most meteorological contexts, atmospheric pressure is accurately approximated by hydrostatic pressure, which is the pressure generated by the weight of the column of air directly above the measurement point. This principle is crucial for understanding pressure variations with altitude.
  • What does the graph illustrating the variation in atmospheric pressure with altitude show?: The provided graph visually demonstrates the variation of atmospheric pressure with altitude, specifically calculated for a temperature of 15 °C and 0% relative humidity, highlighting the consistent decrease in pressure at higher elevations.

Air pressure on mountains is generally higher than at sea level because there is more air mass above them.

Answer: False

Air pressure on mountains is generally lower than at sea level because there is less overlying air mass at higher elevations.

Related Concepts:

  • How does air pressure on mountains compare to air pressure at sea level?: Air pressure on mountains is typically lower than air pressure at sea level. This is because pressure is inversely proportional to the altitude of the surface, meaning higher elevations have a smaller column of air above them.
  • How does atmospheric pressure change with increasing elevation?: As elevation increases, the mass of the overlying atmosphere diminishes, leading to a corresponding decrease in atmospheric pressure. This inverse relationship is a fundamental aspect of atmospheric physics.
  • What is surface pressure, and what is it directly proportional to?: Surface pressure refers to the atmospheric pressure at a specific point on Earth's surface, whether land or ocean. It is directly proportional to the total mass of the air column situated vertically above that particular location.

Atmospheric pressure varies smoothly from the Earth's surface up to the top of the mesosphere, showing a continuous increase with altitude.

Answer: False

Atmospheric pressure varies smoothly with altitude, but it shows a continuous decrease, not increase, with increasing altitude.

Related Concepts:

  • How does atmospheric pressure vary from the Earth's surface to the top of the mesosphere?: Atmospheric pressure exhibits a continuous and smooth decrease with increasing altitude from the Earth's surface up to the top of the mesosphere, reflecting the diminishing density of air at higher elevations.
  • What does the graph illustrating the variation in atmospheric pressure with altitude show?: The provided graph visually demonstrates the variation of atmospheric pressure with altitude, specifically calculated for a temperature of 15 °C and 0% relative humidity, highlighting the consistent decrease in pressure at higher elevations.
  • How does atmospheric pressure change with increasing elevation?: As elevation increases, the mass of the overlying atmosphere diminishes, leading to a corresponding decrease in atmospheric pressure. This inverse relationship is a fundamental aspect of atmospheric physics.

Temperature and humidity are irrelevant for computing accurate atmospheric pressure figures.

Answer: False

Temperature and humidity are crucial for computing accurate atmospheric pressure figures because they influence air density.

Related Concepts:

  • What factors, besides altitude, affect atmospheric pressure, and why are they important for accurate calculations?: Beyond altitude, temperature and humidity are critical factors influencing atmospheric pressure. These variables affect air density, with pressure being proportional to temperature and inversely related to humidity, necessitating their inclusion for accurate pressure computations.

At low altitudes, pressure decreases by approximately 1.2 kPa for every 100 meters of ascent.

Answer: True

At low altitudes above sea level, pressure decreases by about 1.2 kPa (12 hPa) for every 100 meters of ascent.

Related Concepts:

  • What is the approximate rate at which pressure decreases at low altitudes above sea level?: At low altitudes above sea level, the pressure decreases by about 1.2 kilopascals (kPa) or 12 hectopascals (hPa) for every 100 meters of ascent.
  • What does the graph illustrating the variation in atmospheric pressure with altitude show?: The provided graph visually demonstrates the variation of atmospheric pressure with altitude, specifically calculated for a temperature of 15 °C and 0% relative humidity, highlighting the consistent decrease in pressure at higher elevations.
  • How does air pressure on mountains compare to air pressure at sea level?: Air pressure on mountains is typically lower than air pressure at sea level. This is because pressure is inversely proportional to the altitude of the surface, meaning higher elevations have a smaller column of air above them.

The barometric formula is used to relate atmospheric pressure to altitude for all altitudes, including those beyond the troposphere.

Answer: False

The barometric formula is used to mathematically relate atmospheric pressure to altitude specifically within the troposphere, not for all altitudes.

Related Concepts:

  • What is the purpose of the barometric formula in relation to altitude and atmospheric pressure?: The barometric formula is a mathematical model used to relate atmospheric pressure (p) to altitude (h) specifically within the troposphere. It enables the calculation of pressure at various heights based on standard atmospheric properties.

One atmosphere of pressure is equivalent to the pressure exerted by a column of freshwater approximately 33.8 feet deep.

Answer: True

One atmosphere of pressure is equivalent to the pressure exerted by a column of freshwater approximately 10.3 meters (33.8 ft) deep.

Related Concepts:

  • How does one atmosphere of pressure relate to the depth of freshwater?: One standard atmosphere (101.325 kPa or 14.7 psi) is equivalent to the pressure exerted by a column of freshwater approximately 10.3 meters (33.8 ft) deep. This analogy provides a tangible understanding of atmospheric pressure.

A diver at 10.3 meters underwater experiences a total pressure of one atmosphere.

Answer: False

A diver 10.3 meters underwater experiences a total pressure of approximately two atmospheres (one from the air and one from the water column).

Related Concepts:

  • What pressure does a diver experience at 10.3 meters underwater?: A diver submerged 10.3 meters underwater experiences a total pressure of approximately 2 atmospheres: one from the overlying air and an additional atmosphere from the weight of the water column, effectively doubling the ambient pressure.

The maximum height to which water can be raised using suction under standard atmospheric conditions is 10.3 meters.

Answer: True

Under standard atmospheric conditions, 10.3 meters is the maximum height to which water can be raised using suction, as this height corresponds to the pressure of one atmosphere.

Related Concepts:

  • What is the maximum height to which water can be raised using suction under standard atmospheric conditions?: Under standard atmospheric conditions, the maximum theoretical height to which water can be raised using suction is 10.3 meters. This limit is determined by the pressure of one atmosphere, which can push water into a vacuum.

Pure water boils at 212 °F at Earth's standard atmospheric pressure.

Answer: True

Pure water boils at 100 °C (212 °F) at Earth's standard atmospheric pressure.

Related Concepts:

  • At what temperature does pure water boil at Earth's standard atmospheric pressure?: Pure water boils at 100 °C (212 °F) at Earth's standard atmospheric pressure.
  • What does the image of boiling water represent in the context of atmospheric pressure?: This image of boiling water visually represents the physical phenomenon where atmospheric pressure directly affects the temperature at which water reaches its boiling point, typically 100 °C under standard conditions.

The boiling point of a liquid is defined as the temperature at which its vapor pressure becomes lower than the surrounding atmospheric pressure.

Answer: False

The boiling point of a liquid is defined as the temperature at which its vapor pressure becomes equal to the surrounding atmospheric pressure.

Related Concepts:

  • How is the boiling point of a liquid defined in relation to atmospheric pressure?: The boiling point of a liquid is precisely defined as the temperature at which its vapor pressure becomes equal to the surrounding atmospheric pressure, enabling the formation of vapor bubbles throughout the liquid.
  • What does the image of boiling water represent in the context of atmospheric pressure?: This image of boiling water visually represents the physical phenomenon where atmospheric pressure directly affects the temperature at which water reaches its boiling point, typically 100 °C under standard conditions.
  • How does atmospheric pressure affect the boiling point of liquids, and what are the practical implications?: Atmospheric pressure significantly influences the boiling point of liquids: lower pressures result in lower boiling points, and higher pressures lead to higher boiling points. This principle necessitates adjustments to cooking recipes at high elevations (where water boils at lower temperatures) and underpins the operation of pressure cookers (which raise boiling points for faster cooking).

To evaporate a liquid at a lower temperature, such as in distillation, atmospheric pressure can be increased using a vacuum pump.

Answer: False

To evaporate a liquid at a lower temperature, such as in distillation, atmospheric pressure must be lowered using a vacuum pump.

Related Concepts:

  • How can atmospheric pressure be manipulated to evaporate a liquid at a lower temperature, for example, in distillation?: If one wishes to evaporate a liquid at a reduced temperature, for instance in distillation processes, the atmospheric pressure can be lowered by using a vacuum pump, as exemplified by devices like rotary evaporators, which effectively decrease the liquid's boiling point.

In the mid-19th century, explorers used the boiling temperature of water to estimate elevation, as boiling point decreases predictably with altitude.

Answer: True

Explorers in the mid-19th century indeed used the boiling temperature of water to estimate elevation, leveraging the predictable decrease in boiling point with altitude due to lower atmospheric pressure.

Related Concepts:

  • How can the boiling temperature of water be used to estimate elevation?: During the mid-19th century, explorers utilized the predictable decrease in water's boiling point with increasing altitude (due to lower atmospheric pressure) as a method for roughly estimating elevation.

How does atmospheric pressure change with increasing elevation?

Answer: It decreases due to less overlying atmospheric mass.

As elevation increases, there is less overlying atmospheric mass, causing atmospheric pressure to decrease.

Related Concepts:

  • How does atmospheric pressure change with increasing elevation?: As elevation increases, the mass of the overlying atmosphere diminishes, leading to a corresponding decrease in atmospheric pressure. This inverse relationship is a fundamental aspect of atmospheric physics.
  • What does the graph illustrating the variation in atmospheric pressure with altitude show?: The provided graph visually demonstrates the variation of atmospheric pressure with altitude, specifically calculated for a temperature of 15 °C and 0% relative humidity, highlighting the consistent decrease in pressure at higher elevations.
  • How is atmospheric pressure generally approximated in most circumstances?: In most meteorological contexts, atmospheric pressure is accurately approximated by hydrostatic pressure, which is the pressure generated by the weight of the column of air directly above the measurement point. This principle is crucial for understanding pressure variations with altitude.

How does air pressure on mountains compare to air pressure at sea level?

Answer: It is generally lower due to less overlying air mass.

Air pressure on mountains is generally lower than at sea level because there is less overlying air mass at higher elevations.

Related Concepts:

  • How does air pressure on mountains compare to air pressure at sea level?: Air pressure on mountains is typically lower than air pressure at sea level. This is because pressure is inversely proportional to the altitude of the surface, meaning higher elevations have a smaller column of air above them.
  • What is the approximate rate at which pressure decreases at low altitudes above sea level?: At low altitudes above sea level, the pressure decreases by about 1.2 kilopascals (kPa) or 12 hectopascals (hPa) for every 100 meters of ascent.
  • How does atmospheric pressure change with increasing elevation?: As elevation increases, the mass of the overlying atmosphere diminishes, leading to a corresponding decrease in atmospheric pressure. This inverse relationship is a fundamental aspect of atmospheric physics.

What two additional factors, besides altitude, are necessary to compute an accurate atmospheric pressure figure?

Answer: Temperature and humidity

Temperature and humidity are necessary factors, in addition to altitude, for computing an accurate atmospheric pressure figure because they influence air density.

Related Concepts:

  • What factors, besides altitude, affect atmospheric pressure, and why are they important for accurate calculations?: Beyond altitude, temperature and humidity are critical factors influencing atmospheric pressure. These variables affect air density, with pressure being proportional to temperature and inversely related to humidity, necessitating their inclusion for accurate pressure computations.

At low altitudes above sea level, by approximately how much does pressure decrease for every 100 meters of ascent?

Answer: 12 hPa

At low altitudes above sea level, pressure decreases by approximately 1.2 kPa (12 hPa) for every 100 meters of ascent.

Related Concepts:

  • What is the approximate rate at which pressure decreases at low altitudes above sea level?: At low altitudes above sea level, the pressure decreases by about 1.2 kilopascals (kPa) or 12 hectopascals (hPa) for every 100 meters of ascent.

What is the primary purpose of the barometric formula?

Answer: To mathematically relate atmospheric pressure to altitude within the troposphere.

The barometric formula is primarily used to mathematically relate atmospheric pressure to altitude specifically within the troposphere.

Related Concepts:

  • What is the purpose of the barometric formula in relation to altitude and atmospheric pressure?: The barometric formula is a mathematical model used to relate atmospheric pressure (p) to altitude (h) specifically within the troposphere. It enables the calculation of pressure at various heights based on standard atmospheric properties.

How deep would a column of freshwater need to be to exert a pressure equivalent to one atmosphere?

Answer: Approximately 10.3 meters

One atmosphere of pressure is equivalent to the pressure exerted by a column of freshwater approximately 10.3 meters deep.

Related Concepts:

  • How does one atmosphere of pressure relate to the depth of freshwater?: One standard atmosphere (101.325 kPa or 14.7 psi) is equivalent to the pressure exerted by a column of freshwater approximately 10.3 meters (33.8 ft) deep. This analogy provides a tangible understanding of atmospheric pressure.

What total pressure does a diver experience at 10.3 meters underwater?

Answer: 2 atmospheres

A diver 10.3 meters underwater experiences a total pressure of approximately 2 atmospheres (one from the air and one from the water column).

Related Concepts:

  • What pressure does a diver experience at 10.3 meters underwater?: A diver submerged 10.3 meters underwater experiences a total pressure of approximately 2 atmospheres: one from the overlying air and an additional atmosphere from the weight of the water column, effectively doubling the ambient pressure.

What is the maximum height to which water can be raised using suction under standard atmospheric conditions?

Answer: 10.3 meters

Under standard atmospheric conditions, the maximum height to which water can be raised using suction is 10.3 meters.

Related Concepts:

  • What is the maximum height to which water can be raised using suction under standard atmospheric conditions?: Under standard atmospheric conditions, the maximum theoretical height to which water can be raised using suction is 10.3 meters. This limit is determined by the pressure of one atmosphere, which can push water into a vacuum.

At what temperature does pure water boil at Earth's standard atmospheric pressure?

Answer: 100 °C (212 °F)

Pure water boils at 100 °C (212 °F) at Earth's standard atmospheric pressure.

Related Concepts:

  • At what temperature does pure water boil at Earth's standard atmospheric pressure?: Pure water boils at 100 °C (212 °F) at Earth's standard atmospheric pressure.
  • What does the image of boiling water represent in the context of atmospheric pressure?: This image of boiling water visually represents the physical phenomenon where atmospheric pressure directly affects the temperature at which water reaches its boiling point, typically 100 °C under standard conditions.

How is the boiling point of a liquid defined in relation to atmospheric pressure?

Answer: The temperature at which its vapor pressure becomes equal to the surrounding atmospheric pressure.

The boiling point of a liquid is defined as the temperature at which its vapor pressure becomes equal to the surrounding atmospheric pressure.

Related Concepts:

  • How is the boiling point of a liquid defined in relation to atmospheric pressure?: The boiling point of a liquid is precisely defined as the temperature at which its vapor pressure becomes equal to the surrounding atmospheric pressure, enabling the formation of vapor bubbles throughout the liquid.
  • What does the image of boiling water represent in the context of atmospheric pressure?: This image of boiling water visually represents the physical phenomenon where atmospheric pressure directly affects the temperature at which water reaches its boiling point, typically 100 °C under standard conditions.
  • How does atmospheric pressure affect the boiling point of liquids, and what are the practical implications?: Atmospheric pressure significantly influences the boiling point of liquids: lower pressures result in lower boiling points, and higher pressures lead to higher boiling points. This principle necessitates adjustments to cooking recipes at high elevations (where water boils at lower temperatures) and underpins the operation of pressure cookers (which raise boiling points for faster cooking).

What is a practical implication of atmospheric pressure affecting the boiling point of liquids?

Answer: Recipes for cooking at high elevations need adjustments because water boils at a lower temperature.

A practical implication is that recipes for cooking at high elevations need adjustments because water boils at a lower temperature due to reduced atmospheric pressure.

Related Concepts:

  • How does atmospheric pressure affect the boiling point of liquids, and what are the practical implications?: Atmospheric pressure significantly influences the boiling point of liquids: lower pressures result in lower boiling points, and higher pressures lead to higher boiling points. This principle necessitates adjustments to cooking recipes at high elevations (where water boils at lower temperatures) and underpins the operation of pressure cookers (which raise boiling points for faster cooking).
  • What does the image of boiling water represent in the context of atmospheric pressure?: This image of boiling water visually represents the physical phenomenon where atmospheric pressure directly affects the temperature at which water reaches its boiling point, typically 100 °C under standard conditions.

How can atmospheric pressure be manipulated to evaporate a liquid at a lower temperature, such as during distillation?

Answer: By lowering the atmospheric pressure using a vacuum pump.

To evaporate a liquid at a lower temperature, such as during distillation, atmospheric pressure can be lowered using a vacuum pump.

Related Concepts:

  • How can atmospheric pressure be manipulated to evaporate a liquid at a lower temperature, for example, in distillation?: If one wishes to evaporate a liquid at a reduced temperature, for instance in distillation processes, the atmospheric pressure can be lowered by using a vacuum pump, as exemplified by devices like rotary evaporators, which effectively decrease the liquid's boiling point.

Global and Regional Pressure Extremes and Variations

The highest sea-level pressure on Earth typically occurs in the Amazon basin due to its dense rainforests.

Answer: False

The highest sea-level pressure on Earth typically occurs in Siberia, not the Amazon basin.

Related Concepts:

  • Where on Earth does the highest sea-level pressure typically occur, and what are its record highs?: The highest sea-level pressure on Earth is typically observed in Siberia, particularly within the Siberian High, where values frequently exceed 1,050 hPa (15.2 psi or 31 inHg). Record highs have approached 1,085 hPa (15.74 psi or 32.0 inHg).

The lowest measurable sea-level pressure is exclusively found at the centers of tornadoes.

Answer: False

The lowest measurable sea-level pressure is found at the centers of both tropical cyclones and tornadoes.

Related Concepts:

  • Where is the lowest measurable sea-level pressure found, and what was a record low?: The lowest measurable sea-level pressure occurs at the centers of intense tropical cyclones and tornadoes. A non-tornadic record low of 870 hPa (12.6 psi or 26 inHg) has been documented.

Atmospheric pressure exhibits a diurnal or semidiurnal cycle due to global atmospheric tides driven by solar heating.

Answer: True

Atmospheric pressure does exhibit diurnal or semidiurnal cycles, which are caused by global atmospheric tides driven by solar heating.

Related Concepts:

  • How does atmospheric pressure exhibit local variations, and what causes these cycles?: Atmospheric pressure exhibits significant local and global variations, including a pronounced diurnal or semidiurnal (twice-daily) cycle. These oscillations are primarily driven by global atmospheric tides, which are large-scale atmospheric responses to solar heating.
  • What two superimposed cycles characterize local atmospheric pressure variations?: Local atmospheric pressure variations are characterized by the superposition of two primary cycles: a circadian (24-hour) cycle and a semi-circadian (12-hour) cycle, reflecting daily and twice-daily patterns influenced by solar radiation.

The effects of atmospheric tides are strongest in polar areas and weakest in tropical zones.

Answer: False

The effects of atmospheric tides are strongest in tropical zones and almost zero in polar areas.

Related Concepts:

  • Where are the atmospheric tide effects strongest and weakest?: The effects of atmospheric tides are most pronounced in tropical zones, where their amplitude can reach several hectopascals. Conversely, these effects are nearly negligible in polar areas due to distinct atmospheric dynamics.

Local atmospheric pressure variations are characterized by a single 24-hour circadian cycle.

Answer: False

Local atmospheric pressure variations are characterized by two superimposed cycles: a circadian (24-hour) cycle and a semi-circadian (12-hour) cycle.

Related Concepts:

  • What two superimposed cycles characterize local atmospheric pressure variations?: Local atmospheric pressure variations are characterized by the superposition of two primary cycles: a circadian (24-hour) cycle and a semi-circadian (12-hour) cycle, reflecting daily and twice-daily patterns influenced by solar radiation.
  • How does atmospheric pressure exhibit local variations, and what causes these cycles?: Atmospheric pressure exhibits significant local and global variations, including a pronounced diurnal or semidiurnal (twice-daily) cycle. These oscillations are primarily driven by global atmospheric tides, which are large-scale atmospheric responses to solar heating.

The highest adjusted-to-sea level barometric pressure ever recorded above 750 meters occurred in Tosontsengel, Mongolia, in 2001.

Answer: True

The highest adjusted-to-sea level barometric pressure ever recorded above 750 meters was 1,084.8 hPa in Tosontsengel, Mongolia, on December 19, 2001.

Related Concepts:

  • What was the highest adjusted-to-sea level barometric pressure ever recorded on Earth above 750 meters, and where and when did it occur?: The highest adjusted-to-sea level barometric pressure ever recorded on Earth at an elevation above 750 meters was 1,084.8 hPa (32.03 inHg), observed in Tosontsengel, Mongolia, on December 19, 2001.
  • What was the highest adjusted-to-sea level barometric pressure ever recorded on Earth below 750 meters, and where and when did it occur?: The highest adjusted-to-sea level barometric pressure recorded at an elevation below 750 meters was 1,083.8 hPa (32.005 inHg), measured at Agata in Evenk Autonomous Okrug, Russia (at 261 m or 856 ft) on December 31, 1968.

The discrimination in reporting highest barometric pressure records based on elevation is primarily for historical archiving purposes.

Answer: False

The discrimination in reporting highest barometric pressure records based on elevation is due to problematic assumptions associated with reducing sea level pressure from high elevations, which can introduce inaccuracies.

Related Concepts:

  • Why is there a discrimination in the reporting of highest barometric pressure records based on elevation?: The practice of discriminating between highest barometric pressure records based on elevation (above or below 750 meters) stems from the inherent inaccuracies and problematic assumptions, such as a standard lapse rate, involved in reducing high-elevation pressure readings to sea level.

The Dead Sea has a notably high atmospheric pressure of 1,065 hPa because it is the lowest place on Earth, resulting in a greater column of air above it.

Answer: True

The Dead Sea, being the lowest place on Earth, has a greater column of air above it, leading to its notably high atmospheric pressure of 1,065 hPa.

Related Concepts:

  • What is the typical atmospheric pressure at the Dead Sea, and why is it notably high?: The Dead Sea, situated at 430 meters (1,410 ft) below sea level, holds the distinction of being the lowest terrestrial point on Earth. Consequently, it experiences a notably high typical atmospheric pressure of 1,065 hPa, due to the greater column of air above it compared to locations at or above sea level.

The lowest non-tornadic atmospheric pressure ever measured was 870 hPa, recorded during Hurricane Wilma in 2005.

Answer: False

The lowest non-tornadic atmospheric pressure ever measured was 870 hPa, but it was recorded during Typhoon Tip in 1979, not Hurricane Wilma.

Related Concepts:

  • What does the image of Hurricane Wilma illustrate regarding atmospheric pressure?: This image of Hurricane Wilma on October 19, 2005, visually highlights the extremely low pressure (882 hPa or 12.79 psi) observed in the eye of the storm at the time of capture, illustrating the intense pressure gradients within severe weather systems.
  • What was the lowest non-tornadic atmospheric pressure ever measured, and during which event did it occur?: The lowest non-tornadic atmospheric pressure ever instrumentally measured was 870 hPa (0.858 atm or 25.69 inHg), recorded on October 12, 1979, during Typhoon Tip in the western Pacific Ocean by a reconnaissance aircraft.
  • Where is the lowest measurable sea-level pressure found, and what was a record low?: The lowest measurable sea-level pressure occurs at the centers of intense tropical cyclones and tornadoes. A non-tornadic record low of 870 hPa (12.6 psi or 26 inHg) has been documented.

Where on Earth does the highest sea-level pressure typically occur?

Answer: In Siberia

The highest sea-level pressure on Earth typically occurs in Siberia.

Related Concepts:

  • Where on Earth does the highest sea-level pressure typically occur, and what are its record highs?: The highest sea-level pressure on Earth is typically observed in Siberia, particularly within the Siberian High, where values frequently exceed 1,050 hPa (15.2 psi or 31 inHg). Record highs have approached 1,085 hPa (15.74 psi or 32.0 inHg).

What is the lowest measurable sea-level pressure typically found?

Answer: At the centers of tropical cyclones and tornadoes

The lowest measurable sea-level pressure is found at the centers of tropical cyclones and tornadoes.

Related Concepts:

  • Where is the lowest measurable sea-level pressure found, and what was a record low?: The lowest measurable sea-level pressure occurs at the centers of intense tropical cyclones and tornadoes. A non-tornadic record low of 870 hPa (12.6 psi or 26 inHg) has been documented.
  • What was the lowest non-tornadic atmospheric pressure ever measured, and during which event did it occur?: The lowest non-tornadic atmospheric pressure ever instrumentally measured was 870 hPa (0.858 atm or 25.69 inHg), recorded on October 12, 1979, during Typhoon Tip in the western Pacific Ocean by a reconnaissance aircraft.

What causes the diurnal or semidiurnal cycle in atmospheric pressure variations on Earth?

Answer: Global atmospheric tides driven by solar heating.

The diurnal or semidiurnal cycle in atmospheric pressure variations is caused by global atmospheric tides driven by solar heating.

Related Concepts:

  • How does atmospheric pressure exhibit local variations, and what causes these cycles?: Atmospheric pressure exhibits significant local and global variations, including a pronounced diurnal or semidiurnal (twice-daily) cycle. These oscillations are primarily driven by global atmospheric tides, which are large-scale atmospheric responses to solar heating.
  • What two superimposed cycles characterize local atmospheric pressure variations?: Local atmospheric pressure variations are characterized by the superposition of two primary cycles: a circadian (24-hour) cycle and a semi-circadian (12-hour) cycle, reflecting daily and twice-daily patterns influenced by solar radiation.

Where are the effects of atmospheric tides strongest?

Answer: In tropical zones

The effects of atmospheric tides are strongest in tropical zones.

Related Concepts:

  • Where are the atmospheric tide effects strongest and weakest?: The effects of atmospheric tides are most pronounced in tropical zones, where their amplitude can reach several hectopascals. Conversely, these effects are nearly negligible in polar areas due to distinct atmospheric dynamics.

What two superimposed cycles characterize local atmospheric pressure variations?

Answer: Circadian and semi-circadian cycles

Local atmospheric pressure variations are characterized by two superimposed cycles: a circadian (24-hour) cycle and a semi-circadian (12-hour) cycle.

Related Concepts:

  • What two superimposed cycles characterize local atmospheric pressure variations?: Local atmospheric pressure variations are characterized by the superposition of two primary cycles: a circadian (24-hour) cycle and a semi-circadian (12-hour) cycle, reflecting daily and twice-daily patterns influenced by solar radiation.
  • How does atmospheric pressure exhibit local variations, and what causes these cycles?: Atmospheric pressure exhibits significant local and global variations, including a pronounced diurnal or semidiurnal (twice-daily) cycle. These oscillations are primarily driven by global atmospheric tides, which are large-scale atmospheric responses to solar heating.

What was the highest adjusted-to-sea level barometric pressure ever recorded on Earth above 750 meters?

Answer: 1,084.8 hPa

The highest adjusted-to-sea level barometric pressure ever recorded above 750 meters was 1,084.8 hPa.

Related Concepts:

  • What was the highest adjusted-to-sea level barometric pressure ever recorded on Earth above 750 meters, and where and when did it occur?: The highest adjusted-to-sea level barometric pressure ever recorded on Earth at an elevation above 750 meters was 1,084.8 hPa (32.03 inHg), observed in Tosontsengel, Mongolia, on December 19, 2001.

Why is there a discrimination in reporting highest barometric pressure records based on elevation (above or below 750 meters)?

Answer: Due to problematic assumptions in reducing sea level pressure from high elevations.

The discrimination in reporting highest barometric pressure records based on elevation is due to problematic assumptions, such as assuming a standard lapse rate, associated with reducing sea level pressure from high elevations.

Related Concepts:

  • Why is there a discrimination in the reporting of highest barometric pressure records based on elevation?: The practice of discriminating between highest barometric pressure records based on elevation (above or below 750 meters) stems from the inherent inaccuracies and problematic assumptions, such as a standard lapse rate, involved in reducing high-elevation pressure readings to sea level.

What is the typical atmospheric pressure at the Dead Sea, and why is it high?

Answer: 1,065 hPa, due to a greater column of air above it as the lowest place on Earth.

The Dead Sea, being the lowest place on Earth, has a greater column of air above it, leading to its notably high atmospheric pressure of 1,065 hPa.

Related Concepts:

  • What is the typical atmospheric pressure at the Dead Sea, and why is it notably high?: The Dead Sea, situated at 430 meters (1,410 ft) below sea level, holds the distinction of being the lowest terrestrial point on Earth. Consequently, it experiences a notably high typical atmospheric pressure of 1,065 hPa, due to the greater column of air above it compared to locations at or above sea level.

What was the lowest non-tornadic atmospheric pressure ever measured, and during which event did it occur?

Answer: 870 hPa during Typhoon Tip.

The lowest non-tornadic atmospheric pressure ever measured was 870 hPa, recorded during Typhoon Tip in 1979.

Related Concepts:

  • What was the lowest non-tornadic atmospheric pressure ever measured, and during which event did it occur?: The lowest non-tornadic atmospheric pressure ever instrumentally measured was 870 hPa (0.858 atm or 25.69 inHg), recorded on October 12, 1979, during Typhoon Tip in the western Pacific Ocean by a reconnaissance aircraft.
  • Where is the lowest measurable sea-level pressure found, and what was a record low?: The lowest measurable sea-level pressure occurs at the centers of intense tropical cyclones and tornadoes. A non-tornadic record low of 870 hPa (12.6 psi or 26 inHg) has been documented.

Applied Meteorology and Engineering

Mean Sea-Level Pressure (MSLP) is primarily used by pilots to calibrate altimeters, not commonly provided in general weather reports.

Answer: False

Mean Sea-Level Pressure (MSLP) is the atmospheric pressure value commonly provided in general weather reports by meteorologists, while altimeter settings (QNH) are used by pilots.

Related Concepts:

  • What is Mean Sea-Level Pressure (MSLP), and how is it used in everyday life?: Mean Sea-Level Pressure (MSLP) is the atmospheric pressure adjusted to mean sea level. This standardized value is routinely reported in weather forecasts via various media, serving as a common reference for meteorological conditions.

In aviation weather reports (METAR), QNH is transmitted globally in inches of mercury, except in the United States, Canada, and Japan where it's in hectopascals.

Answer: False

In METAR reports, QNH is transmitted globally in hectopascals or millibars, but in the United States, Canada, and Japan, it is reported in inches of mercury.

Related Concepts:

  • How is QNH transmitted in aviation weather reports globally, and how does this differ in the United States, Canada, and Japan?: In aviation weather reports (METAR), QNH, which is the altimeter setting, is transmitted globally in hectopascals or millibars. However, in the United States, Canada, and Japan, the altimeter setting is reported in inches of mercury, typically to two decimal places.

Atmospheric models like GCMs typically predict the non-dimensional logarithm of surface pressure for numerical stability.

Answer: True

For computational stability and efficiency, atmospheric models like General Circulation Models (GCMs) typically predict the non-dimensional logarithm of surface pressure.

Related Concepts:

  • How do atmospheric models, such as general circulation models (GCMs), typically predict surface pressure?: For computational stability and efficiency, atmospheric models like General Circulation Models (GCMs), typically predict the non-dimensional logarithm of surface pressure rather than the raw pressure values.

Low pressures in natural gas lines are sometimes specified in 'inches of mercury' gauge.

Answer: False

Low pressures in natural gas lines are sometimes specified in 'inches of water' gauge (w.c. or w.g.), not inches of mercury.

Related Concepts:

  • How are low pressures, such as those in natural gas lines, sometimes specified?: Low pressures, like those found in natural gas lines, are frequently specified in 'inches of water,' denoted as w.c. (water column) gauge or w.g. (inches water) gauge. These units are based on the height of a water column.

Nevil Maskelyne and William Roy used barometric pressure to confirm height determinations during the Schiehallion experiment in 1774, with their results agreeing within one meter.

Answer: True

During the 1774 Schiehallion experiment, William Roy used barometric pressure to confirm Nevil Maskelyne's height determinations, achieving agreement within one meter.

Related Concepts:

  • Who were Nevil Maskelyne and William Roy, and how did they use barometric pressure in the Schiehallion experiment?: In 1774, during the Schiehallion experiment in Scotland, Nevil Maskelyne conducted gravitational measurements that required precise elevation data. William Roy corroborated Maskelyne's height determinations using barometric pressure, with their results agreeing within one meter, underscoring the accuracy of this method for surveying.

An altimeter setting in aviation is used to adjust altimeters for accurate altitude readings relative to a specific reference point, but not sea level.

Answer: False

An altimeter setting in aviation is used to adjust altimeters for accurate altitude readings relative to sea level or a specific reference point.

Related Concepts:

  • What is an altimeter setting in aviation?: In aviation, the altimeter setting (QNH) is a crucial atmospheric pressure value used by pilots to calibrate their altimeters. This calibration ensures accurate altitude readings relative to sea level or a designated reference point, vital for flight safety.

How is the altimeter setting (QNH) reported in aviation weather reports (METAR) in the United States, Canada, and Japan?

Answer: In inches of mercury

In the United States, Canada, and Japan, the altimeter setting (QNH) in METAR reports is reported in inches of mercury.

Related Concepts:

  • How is QNH transmitted in aviation weather reports globally, and how does this differ in the United States, Canada, and Japan?: In aviation weather reports (METAR), QNH, which is the altimeter setting, is transmitted globally in hectopascals or millibars. However, in the United States, Canada, and Japan, the altimeter setting is reported in inches of mercury, typically to two decimal places.

Why do atmospheric models like General Circulation Models (GCMs) typically predict the non-dimensional logarithm of surface pressure?

Answer: To improve model stability and simplify calculations.

Atmospheric models like GCMs typically predict the non-dimensional logarithm of surface pressure for numerical reasons, specifically to simplify calculations and improve model stability.

Related Concepts:

  • How do atmospheric models, such as general circulation models (GCMs), typically predict surface pressure?: For computational stability and efficiency, atmospheric models like General Circulation Models (GCMs), typically predict the non-dimensional logarithm of surface pressure rather than the raw pressure values.

How are low pressures in natural gas lines sometimes specified?

Answer: In inches of water gauge (w.g.)

Low pressures in natural gas lines are sometimes specified in 'inches of water' gauge (w.g.).

Related Concepts:

  • How are low pressures, such as those in natural gas lines, sometimes specified?: Low pressures, like those found in natural gas lines, are frequently specified in 'inches of water,' denoted as w.c. (water column) gauge or w.g. (inches water) gauge. These units are based on the height of a water column.

In 1774, who used barometric pressure to confirm height determinations during the Schiehallion experiment?

Answer: William Roy

In 1774, William Roy used barometric pressure to confirm height determinations during the Schiehallion experiment.

Related Concepts:

  • Who were Nevil Maskelyne and William Roy, and how did they use barometric pressure in the Schiehallion experiment?: In 1774, during the Schiehallion experiment in Scotland, Nevil Maskelyne conducted gravitational measurements that required precise elevation data. William Roy corroborated Maskelyne's height determinations using barometric pressure, with their results agreeing within one meter, underscoring the accuracy of this method for surveying.

In the United States and Canada, how is sea-level pressure (SLP) reported in weather code remarks?

Answer: In hectopascals or millibars, with decimal points and most significant digits omitted.

In the United States and Canada, sea-level pressure (SLP) is reported in weather code remarks in hectopascals or millibars, with decimal points and most significant digits omitted.

Related Concepts:

  • How do the United States and Canada report sea-level pressure (SLP) in weather code remarks?: In the United States and Canada, sea-level pressure (SLP) is included in the remarks section of weather codes, distinct from the internationally transmitted portion. This SLP is adjusted to sea level using specific regional methods and is expressed in hectopascals or millibars, with decimal points and leading digits often omitted (e.g., 1,013.2 hPa as 132, 1,000 hPa as 000).

Home | Sitemaps | Contact | Terms | Privacy