Geo: Chapter Three, Section One
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The document discusses the causes of seasons and weather patterns around the world. It explains that the Earth's 23.5 degree tilt and revolution around the sun cause the seasons as different parts of the Earth experience more or less direct sunlight throughout the year. It also defines key weather terminology like climate, weather, precipitation types, and extreme weather events like hurricanes, tornadoes, blizzards, droughts, and floods. Seasons and weather are influenced by many atmospheric and environmental factors.
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3. Anticyclones
Anticyclones bring settled weather to the UK, with dry, bright conditions that can last for several days. In summer, anticyclones result in hot and sunny weather due to clear skies and a high sun. In winter, anticyclones lead to cold, clear nights that allow frost and fog to form as the sun is low and days are short. The weather associated with anticyclones is explained by the sinking air within the high pressure system, which warms and picks up moisture, preventing cloud and precipitation.
What Affects Weather Patterns
1) A place's latitude and proximity to oceans or large bodies of water help determine its climate and weather patterns. Locations closer to the equator tend to be warmer, while areas farther from the equator experience more distinct seasons.
2) Climate zones like polar, temperate, and tropical regions exist depending on latitude. Hemispheres also influence seasons, with the northern and southern hemispheres experiencing opposite seasonal changes at the same time.
3) Geography such as mountains and bodies of water further impact local weather. Mountains can create rain shadows - dry areas on their leeward sides. Meanwhile, coastal areas tend to have milder temperatures regulated by the moderating effect of oceans.
Air Masses
There are several major air masses that influence weather patterns:
1) Continental Arctic (cA) air masses are very cold and dry, originating north of the Arctic Circle.
2) Continental polar (cP) air masses are cold and dry, originating in northern Canada and influencing northern US weather.
3) Maritime polar (mP) air masses are cool and moist, originating over the North Atlantic and Pacific and influencing the Pacific Northwest and Northeast.
4) Maritime tropical (mT) air masses are warm and moist, originating in the Gulf of Mexico and influencing the eastern US.
Air Masses and Fronts
Maritime tropical air masses form over warm waters and bring warm, moist air into parts of the United States. Continental polar air masses form over snow-covered northern Canada and bring cold, dry air into central and eastern portions of the country. When warm and cold air masses meet, fronts are formed. Cold fronts have steep slopes that can produce heavy precipitation like thunderstorms and hail, while warm fronts have more gentle slopes and cause lighter, longer-lasting precipitation from nimbostratus clouds. Occluded fronts occur when a cold front catches up to a warm front.
16. movement of air notes
Wind is caused by uneven heating of the Earth's surface and atmosphere, creating areas of high and low pressure. Warm air rises and cold air sinks, driving wind from high to low pressure areas. Additional factors like the rotation of the Earth and differences in how land and water absorb and release heat cause global wind patterns like trade winds and jet streams to form and influence weather.
Air Masses, Global Winds, and Fronts
This document discusses key concepts in meteorology including:
1. Meteorology is the study of atmospheric phenomena like weather and climate. Different types of atmospheric "meteors" include clouds, rain, fog, and rainbows.
2. Weather describes current atmospheric conditions while climate refers to long-term average conditions in an area.
3. Air masses form over large areas and take on the characteristics of those regions, like continental polar (cP) air masses which are cold and dry.
4. Global wind systems like the trade winds and prevailing westerlies circulate air globally due to the Coriolis effect from Earth's rotation. Fronts form where different air masses collide.
Physical Geography Lecture 08 - Precipitation, Air Masses, and Storms 110216
The formation of precipitation. Types of precipitation. Global and U.S. precipitation. Air masses, source regions, classification. Air masses of North America. Fronts. Warm front, cold front, stationary front, occluded front. Life-cycle of a midlatitude cyclone. Weather changes with the passage of a cold front. Midlatitude anticyclones. Lightning, thunder. Tornadoes. Hurricanes. Storm surge.
Weather Systems Revision 2014
The document discusses weather and climate. It defines weather as short-term atmospheric conditions over days or weeks involving factors like temperature and precipitation. Climate is defined as generalized conditions over 30+ years, averaging temperature and precipitation patterns. Weather involves changes in atmospheric conditions, while climate involves long-term changes.
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3. Anticyclones
Anticyclones bring settled weather to the UK, with dry, bright conditions that can last for several days. In summer, anticyclones result in hot and sunny weather due to clear skies and a high sun. In winter, anticyclones lead to cold, clear nights that allow frost and fog to form as the sun is low and days are short. The weather associated with anticyclones is explained by the sinking air within the high pressure system, which warms and picks up moisture, preventing cloud and precipitation.
What Affects Weather Patterns
1) A place's latitude and proximity to oceans or large bodies of water help determine its climate and weather patterns. Locations closer to the equator tend to be warmer, while areas farther from the equator experience more distinct seasons.
2) Climate zones like polar, temperate, and tropical regions exist depending on latitude. Hemispheres also influence seasons, with the northern and southern hemispheres experiencing opposite seasonal changes at the same time.
3) Geography such as mountains and bodies of water further impact local weather. Mountains can create rain shadows - dry areas on their leeward sides. Meanwhile, coastal areas tend to have milder temperatures regulated by the moderating effect of oceans.
Air Masses
There are several major air masses that influence weather patterns:
1) Continental Arctic (cA) air masses are very cold and dry, originating north of the Arctic Circle.
2) Continental polar (cP) air masses are cold and dry, originating in northern Canada and influencing northern US weather.
3) Maritime polar (mP) air masses are cool and moist, originating over the North Atlantic and Pacific and influencing the Pacific Northwest and Northeast.
4) Maritime tropical (mT) air masses are warm and moist, originating in the Gulf of Mexico and influencing the eastern US.
Air Masses and Fronts
Maritime tropical air masses form over warm waters and bring warm, moist air into parts of the United States. Continental polar air masses form over snow-covered northern Canada and bring cold, dry air into central and eastern portions of the country. When warm and cold air masses meet, fronts are formed. Cold fronts have steep slopes that can produce heavy precipitation like thunderstorms and hail, while warm fronts have more gentle slopes and cause lighter, longer-lasting precipitation from nimbostratus clouds. Occluded fronts occur when a cold front catches up to a warm front.
16. movement of air notes
Wind is caused by uneven heating of the Earth's surface and atmosphere, creating areas of high and low pressure. Warm air rises and cold air sinks, driving wind from high to low pressure areas. Additional factors like the rotation of the Earth and differences in how land and water absorb and release heat cause global wind patterns like trade winds and jet streams to form and influence weather.
Air Masses, Global Winds, and Fronts
This document discusses key concepts in meteorology including:
1. Meteorology is the study of atmospheric phenomena like weather and climate. Different types of atmospheric "meteors" include clouds, rain, fog, and rainbows.
2. Weather describes current atmospheric conditions while climate refers to long-term average conditions in an area.
3. Air masses form over large areas and take on the characteristics of those regions, like continental polar (cP) air masses which are cold and dry.
4. Global wind systems like the trade winds and prevailing westerlies circulate air globally due to the Coriolis effect from Earth's rotation. Fronts form where different air masses collide.
Physical Geography Lecture 08 - Precipitation, Air Masses, and Storms 110216
The formation of precipitation. Types of precipitation. Global and U.S. precipitation. Air masses, source regions, classification. Air masses of North America. Fronts. Warm front, cold front, stationary front, occluded front. Life-cycle of a midlatitude cyclone. Weather changes with the passage of a cold front. Midlatitude anticyclones. Lightning, thunder. Tornadoes. Hurricanes. Storm surge.
Weather Systems Revision 2014
The document discusses weather and climate. It defines weather as short-term atmospheric conditions over days or weeks involving factors like temperature and precipitation. Climate is defined as generalized conditions over 30+ years, averaging temperature and precipitation patterns. Weather involves changes in atmospheric conditions, while climate involves long-term changes.
Global and Local Winds
Winds are caused by differences in air pressure due to uneven heating of the atmosphere. Global wind patterns form large convection cells that circulate air from the equator to the poles. Local winds include sea breezes and land breezes, which occur when air over land or water is heated and cooled more quickly than the adjacent surface, causing pressure differences and winds to flow from the cooler to warmer surface during the day and night.
Cloud Development & Classification
The document discusses several key topics about the atmosphere:
1) The main gases in the atmosphere are nitrogen, oxygen, water vapor and carbon dioxide. Water vapor can range from 0-4% and carbon dioxide is under 1%.
2) Temperature measures molecular motion, while heat is the transfer of thermal energy. Temperature can be measured in Fahrenheit, Celsius or Kelvin.
3) Clouds form through convection when warm air rises and cools, orographic lifting when air rises over mountains, and when warm and cold air masses collide. Latent heat is released when water vapor condenses.
4) Clouds are classified by height as low, middle, or high, and by
Common atmospheric phenomena
winds
local winds and global winds
sea breeze and land breeze
monsoons 'amihan and habagat'
intertropical convergence zone(itcz)
1.5 Air Pressure_Ch10_L6
This document discusses various concepts related to air pressure and wind, including:
1. Different types of winds such as sea breezes and land breezes that are caused by differences in air temperature over land and water.
2. The Coriolis effect which causes winds to curve due to the rotation of the Earth, curving right in the Northern Hemisphere and left in the Southern Hemisphere.
3. Isobars which are lines connecting places with equal air pressure on a weather map, and how differences in air pressure and temperature can cause winds.
Chpt 3 and 4
Chapter 3 discusses how the Earth's tilt and rotation cause seasons and affect the amount of sunlight different places receive throughout the year. Chapter 4 discusses factors that influence weather like solar energy, water vapor, elevation, and air movement. It also describes extreme weather events like hurricanes, tornadoes, blizzards, droughts, and floods. Additionally, it explains how wind currents, ocean currents, and latitude zones impact climate globally.
Rainfall ppt
The document discusses the three main types of rainfall: convectional, orographic, and frontal/cyclonic. Convectional rainfall occurs when warm air near the surface rises vertically due to heating from the sun, cools and condenses to form cumulonimbus clouds and rain. Orographic rainfall occurs when moist air is forced to rise over mountains, cooling and condensing on mountain slopes. Frontal/cyclonic rainfall occurs along boundaries where warm and cold air masses meet, with the warm air forced aloft over the cold air, cooling and producing precipitation along the frontal zone. Diagrams are provided to illustrate each type.
Air mass
An air mass is a large body of air with similar temperature and moisture properties that can cover hundreds of thousands of square miles. Air masses originate over land or water source regions and take on the characteristics of the surface below over time. There are four main types of air masses defined by their source region in tropical or polar latitudes and whether that region is over land or water. When polar air meets warmer air over the United States, it causes the formation of the polar jet stream, a narrow belt of strong winds near the top of the troposphere that influences weather patterns and temperatures in the US.
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The document provides an overview of the climate of the Maltese islands, describing key climate variables such as temperature, rainfall, wind, humidity and sunlight. It notes that the climate is Mediterranean with hot, dry summers and mild, wetter winters. Specifically, it reports that July and August are the hottest and driest months while December and January are the coolest and wettest months. Thunderstorms are most common between October and February. The document also includes diagrams of average monthly climate readings.
Tornadoes
Tornadoes form from thunderstorms when warm, moist air meets cool, dry air, creating instability. This causes the rotating air to tilt from horizontal to vertical, forming a violent rotating column extending from the thunderstorm to the ground. Tornadoes are most common in the central US, known as Tornado Alley, and occur most frequently between May and September in the southern US. Modern tornado detection uses weather radar rather than relying on visual sightings.
How do fronts & air masses change the
This document discusses how air masses and fronts influence weather patterns. It explains that air masses are large bodies of air with uniform temperature and moisture content that form over land or water. Fronts are boundaries between differing air masses. There are three main types of fronts: cold fronts, which bring storms and precipitation; warm fronts, which produce steady rain and clearing weather; and stationary fronts, which can cause prolonged storms and flooding. The document also outlines weather map symbols and provides safety tips for severe weather like tornadoes, blizzards, and hurricanes.
Air masses and fronts
- Air masses are large bodies of air with uniform temperature and moisture characteristics that form over source regions. The main types are continental polar (CP), maritime polar (MP), continental tropical (CT), and maritime tropical (MT).
- Fronts occur at boundaries between converging air masses. The main types are cold fronts, warm fronts, stationary fronts, and occluded fronts. Cold fronts bring strong winds and thunderstorms while warm fronts bring gentle rain.
- Frontogenesis is the formation of fronts while frontolysis is the dissipation of fronts. Mid-latitude cyclones form due to frontogenesis between air masses.
Notes - Air Masses, Fronts, Global Winds
Meteorology is the study of atmospheric phenomena including weather and climate. Weather refers to current atmospheric conditions while climate describes average conditions over time for a particular region. Air masses form over large areas and take on characteristics of that region, later influencing other areas as the air mass moves horizontally. Global wind patterns called zones transport air masses. Weather systems form as air masses with different properties interact, such as through fronts which occur at boundaries between air masses.
The Restless Atmosphere
The document discusses how the atmosphere and winds are created. It explains that the sun unevenly heats the Earth's surface, causing air to rise in some areas and fall in others. This difference in air pressure creates winds that blow from high to low pressure areas. It also describes how latitude affects temperature, with areas near the equator being warmer, and how the Earth's rotation causes air currents to bend into circular storm patterns.
Air masses And FRonts
This document discusses air masses and fronts. It defines air masses as large bodies of air that extend thousands of kilometers and have uniform temperature and humidity. Air masses form over source regions and are classified as either tropical or polar, and continental or maritime. Fronts occur at the boundary between differing air masses and can be cold, warm, stationary or occluded fronts. Each front type brings characteristic weather conditions from rain to thunderstorms as the warmer air is displaced.
Fronts
A cold front brings brief heavy storms with thunderstorms and strong winds. After the storm, the weather is usually cooler and drier. A warm front brings light steady rain or snow that may last for days with usually light winds. It can also bring fog. Afterward, the weather is usually warmer and more humid.
Common atmospheric phenomena
The document discusses several common atmospheric phenomena including sea breezes, land breezes, monsoons, and the Intertropical Convergence Zone (ITCZ). It explains that land heats up faster than water and cools down faster, leading to sea breezes during the day and land breezes at night. Monsoons are seasonal winds that blow from the northeast as the Northeast Monsoon from October to March and from the southwest as the Southwest Monsoon from July to September. The ITCZ is a zone where winds converge near the equator, causing rising air and thunderstorms during parts of the year.
Chapter 16 2 Air Masses, Fronts And Weather Maps Andie
An air mass is a large volume of air that has uniform temperature and humidity characteristics based on the region it forms over. There are four main types of air masses: maritime tropical, continental tropical, maritime polar, and continental polar. Weather fronts occur when different air masses meet, with warm fronts and cold fronts creating different weather conditions based on whether the warmer or colder air is overriding the other. Weather maps use symbols like isotherms, isobars, and frontal boundaries to depict these air mass interactions and the resulting weather patterns.
Winds cscope
Winds are caused by differences in air pressure resulting from uneven heating of the Earth's surface by the sun. Warm air at the equator rises and cooler air from the poles moves in to replace it, creating global convection currents. These convection currents form circular wind patterns called prevailing winds, with easterly winds near the equator and westerly winds at mid-latitudes blowing toward the poles. The rotation of the Earth causes these winds to curve due to the Coriolis effect.
Marine - Energy in the Atmosphere Notes
This document discusses various topics relating to energy in the atmosphere, including:
- Heat energy and how it relates to the movement of atoms
- Different types of radiation that make up the electromagnetic spectrum
- How solar radiation interacts with layers of the atmosphere and is absorbed by certain gases
- Processes like scattering, reflection, and the greenhouse effect that redistribute heat energy
What factors affect different types of weather (the whole lesson)
The document describes the water cycle, which is the continuous movement of water on, above, and below the surface of the Earth. It explains that the sun heats water in the oceans causing evaporation into water vapor which forms clouds. As air rises, it cools and condenses into rain, snow, or other precipitation which falls back to Earth's surface and collects in lakes, rivers, and oceans - completing the cycle. The document also covers related topics like humidity, cloud types, precipitation types, thunderstorms, tornadoes, and hurricanes.
Antartica seasons etc
The document discusses seasons, temperature, precipitation, and days/nights in Antarctica. It notes that because of the Earth's tilt and orbit, the poles receive less sunlight, resulting in only two seasons - summer and winter. In summer at the poles, the sun does not set and in winter the sun does not rise. Interior temperatures average -57°C with coastal areas between -10°C to -30°C in winter occasionally rising to freezing. The coldest recorded temperature on Earth was -89.2°C at Vostok station. Precipitation is mainly snow with coastal areas receiving about 200mm annually and mountainous/plateau areas less than 50mm due to cold temperatures preventing evaporation. Much
The Seasons
The document discusses the earth's tilt and its impact on seasons. It explains that without the tilt, there would be no seasons. It then lists the months that fall under each season in the United States: Winter (January, February, middle of March), Spring (April, May, middle of June), Summer (July, August, middle of September), Fall (October, November, middle of December).
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Global and Local Winds
Winds are caused by differences in air pressure due to uneven heating of the atmosphere. Global wind patterns form large convection cells that circulate air from the equator to the poles. Local winds include sea breezes and land breezes, which occur when air over land or water is heated and cooled more quickly than the adjacent surface, causing pressure differences and winds to flow from the cooler to warmer surface during the day and night.
Cloud Development & Classification
The document discusses several key topics about the atmosphere:
1) The main gases in the atmosphere are nitrogen, oxygen, water vapor and carbon dioxide. Water vapor can range from 0-4% and carbon dioxide is under 1%.
2) Temperature measures molecular motion, while heat is the transfer of thermal energy. Temperature can be measured in Fahrenheit, Celsius or Kelvin.
3) Clouds form through convection when warm air rises and cools, orographic lifting when air rises over mountains, and when warm and cold air masses collide. Latent heat is released when water vapor condenses.
4) Clouds are classified by height as low, middle, or high, and by
Common atmospheric phenomena
winds
local winds and global winds
sea breeze and land breeze
monsoons 'amihan and habagat'
intertropical convergence zone(itcz)
1.5 Air Pressure_Ch10_L6
This document discusses various concepts related to air pressure and wind, including:
1. Different types of winds such as sea breezes and land breezes that are caused by differences in air temperature over land and water.
2. The Coriolis effect which causes winds to curve due to the rotation of the Earth, curving right in the Northern Hemisphere and left in the Southern Hemisphere.
3. Isobars which are lines connecting places with equal air pressure on a weather map, and how differences in air pressure and temperature can cause winds.
Chpt 3 and 4
Chapter 3 discusses how the Earth's tilt and rotation cause seasons and affect the amount of sunlight different places receive throughout the year. Chapter 4 discusses factors that influence weather like solar energy, water vapor, elevation, and air movement. It also describes extreme weather events like hurricanes, tornadoes, blizzards, droughts, and floods. Additionally, it explains how wind currents, ocean currents, and latitude zones impact climate globally.
Rainfall ppt
The document discusses the three main types of rainfall: convectional, orographic, and frontal/cyclonic. Convectional rainfall occurs when warm air near the surface rises vertically due to heating from the sun, cools and condenses to form cumulonimbus clouds and rain. Orographic rainfall occurs when moist air is forced to rise over mountains, cooling and condensing on mountain slopes. Frontal/cyclonic rainfall occurs along boundaries where warm and cold air masses meet, with the warm air forced aloft over the cold air, cooling and producing precipitation along the frontal zone. Diagrams are provided to illustrate each type.
Air mass
An air mass is a large body of air with similar temperature and moisture properties that can cover hundreds of thousands of square miles. Air masses originate over land or water source regions and take on the characteristics of the surface below over time. There are four main types of air masses defined by their source region in tropical or polar latitudes and whether that region is over land or water. When polar air meets warmer air over the United States, it causes the formation of the polar jet stream, a narrow belt of strong winds near the top of the troposphere that influences weather patterns and temperatures in the US.
Lesson 5: Climate of the Maltese Islands
The document provides an overview of the climate of the Maltese islands, describing key climate variables such as temperature, rainfall, wind, humidity and sunlight. It notes that the climate is Mediterranean with hot, dry summers and mild, wetter winters. Specifically, it reports that July and August are the hottest and driest months while December and January are the coolest and wettest months. Thunderstorms are most common between October and February. The document also includes diagrams of average monthly climate readings.
Tornadoes
Tornadoes form from thunderstorms when warm, moist air meets cool, dry air, creating instability. This causes the rotating air to tilt from horizontal to vertical, forming a violent rotating column extending from the thunderstorm to the ground. Tornadoes are most common in the central US, known as Tornado Alley, and occur most frequently between May and September in the southern US. Modern tornado detection uses weather radar rather than relying on visual sightings.
How do fronts & air masses change the
This document discusses how air masses and fronts influence weather patterns. It explains that air masses are large bodies of air with uniform temperature and moisture content that form over land or water. Fronts are boundaries between differing air masses. There are three main types of fronts: cold fronts, which bring storms and precipitation; warm fronts, which produce steady rain and clearing weather; and stationary fronts, which can cause prolonged storms and flooding. The document also outlines weather map symbols and provides safety tips for severe weather like tornadoes, blizzards, and hurricanes.
Air masses and fronts
- Air masses are large bodies of air with uniform temperature and moisture characteristics that form over source regions. The main types are continental polar (CP), maritime polar (MP), continental tropical (CT), and maritime tropical (MT).
- Fronts occur at boundaries between converging air masses. The main types are cold fronts, warm fronts, stationary fronts, and occluded fronts. Cold fronts bring strong winds and thunderstorms while warm fronts bring gentle rain.
- Frontogenesis is the formation of fronts while frontolysis is the dissipation of fronts. Mid-latitude cyclones form due to frontogenesis between air masses.
Notes - Air Masses, Fronts, Global Winds
Meteorology is the study of atmospheric phenomena including weather and climate. Weather refers to current atmospheric conditions while climate describes average conditions over time for a particular region. Air masses form over large areas and take on characteristics of that region, later influencing other areas as the air mass moves horizontally. Global wind patterns called zones transport air masses. Weather systems form as air masses with different properties interact, such as through fronts which occur at boundaries between air masses.
The Restless Atmosphere
The document discusses how the atmosphere and winds are created. It explains that the sun unevenly heats the Earth's surface, causing air to rise in some areas and fall in others. This difference in air pressure creates winds that blow from high to low pressure areas. It also describes how latitude affects temperature, with areas near the equator being warmer, and how the Earth's rotation causes air currents to bend into circular storm patterns.
Air masses And FRonts
This document discusses air masses and fronts. It defines air masses as large bodies of air that extend thousands of kilometers and have uniform temperature and humidity. Air masses form over source regions and are classified as either tropical or polar, and continental or maritime. Fronts occur at the boundary between differing air masses and can be cold, warm, stationary or occluded fronts. Each front type brings characteristic weather conditions from rain to thunderstorms as the warmer air is displaced.
Fronts
A cold front brings brief heavy storms with thunderstorms and strong winds. After the storm, the weather is usually cooler and drier. A warm front brings light steady rain or snow that may last for days with usually light winds. It can also bring fog. Afterward, the weather is usually warmer and more humid.
Common atmospheric phenomena
The document discusses several common atmospheric phenomena including sea breezes, land breezes, monsoons, and the Intertropical Convergence Zone (ITCZ). It explains that land heats up faster than water and cools down faster, leading to sea breezes during the day and land breezes at night. Monsoons are seasonal winds that blow from the northeast as the Northeast Monsoon from October to March and from the southwest as the Southwest Monsoon from July to September. The ITCZ is a zone where winds converge near the equator, causing rising air and thunderstorms during parts of the year.
Chapter 16 2 Air Masses, Fronts And Weather Maps Andie
An air mass is a large volume of air that has uniform temperature and humidity characteristics based on the region it forms over. There are four main types of air masses: maritime tropical, continental tropical, maritime polar, and continental polar. Weather fronts occur when different air masses meet, with warm fronts and cold fronts creating different weather conditions based on whether the warmer or colder air is overriding the other. Weather maps use symbols like isotherms, isobars, and frontal boundaries to depict these air mass interactions and the resulting weather patterns.
Winds cscope
Winds are caused by differences in air pressure resulting from uneven heating of the Earth's surface by the sun. Warm air at the equator rises and cooler air from the poles moves in to replace it, creating global convection currents. These convection currents form circular wind patterns called prevailing winds, with easterly winds near the equator and westerly winds at mid-latitudes blowing toward the poles. The rotation of the Earth causes these winds to curve due to the Coriolis effect.
Marine - Energy in the Atmosphere Notes
This document discusses various topics relating to energy in the atmosphere, including:
- Heat energy and how it relates to the movement of atoms
- Different types of radiation that make up the electromagnetic spectrum
- How solar radiation interacts with layers of the atmosphere and is absorbed by certain gases
- Processes like scattering, reflection, and the greenhouse effect that redistribute heat energy
What factors affect different types of weather (the whole lesson)
The document describes the water cycle, which is the continuous movement of water on, above, and below the surface of the Earth. It explains that the sun heats water in the oceans causing evaporation into water vapor which forms clouds. As air rises, it cools and condenses into rain, snow, or other precipitation which falls back to Earth's surface and collects in lakes, rivers, and oceans - completing the cycle. The document also covers related topics like humidity, cloud types, precipitation types, thunderstorms, tornadoes, and hurricanes.
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Chapter 16 2 Air Masses, Fronts And Weather Maps Andie
Chapter 16 2 Air Masses, Fronts And Weather Maps Andie
What factors affect different types of weather (the whole lesson)
What factors affect different types of weather (the whole lesson)
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Antartica seasons etc
The document discusses seasons, temperature, precipitation, and days/nights in Antarctica. It notes that because of the Earth's tilt and orbit, the poles receive less sunlight, resulting in only two seasons - summer and winter. In summer at the poles, the sun does not set and in winter the sun does not rise. Interior temperatures average -57°C with coastal areas between -10°C to -30°C in winter occasionally rising to freezing. The coldest recorded temperature on Earth was -89.2°C at Vostok station. Precipitation is mainly snow with coastal areas receiving about 200mm annually and mountainous/plateau areas less than 50mm due to cold temperatures preventing evaporation. Much
The Seasons
The document discusses the earth's tilt and its impact on seasons. It explains that without the tilt, there would be no seasons. It then lists the months that fall under each season in the United States: Winter (January, February, middle of March), Spring (April, May, middle of June), Summer (July, August, middle of September), Fall (October, November, middle of December).
The atmosphere and the oceans
The document discusses the composition and structure of Earth's atmosphere. It describes the different layers of the atmosphere, including the troposphere, stratosphere, mesosphere, thermosphere, and exosphere. It explains how solar energy is transferred throughout the atmosphere using radiation, conduction, and convection. The document also mentions clouds and the water cycle.
Seasons
Earth's seasons are caused by its revolution around the sun and the tilt of its 23.5 degree axis. During summer, the northern hemisphere tilts toward the sun, receiving direct sunlight and warmer temperatures. In winter, the northern hemisphere tilts away from the sun and receives indirect sunlight, resulting in cooler temperatures. Spring and fall occur when both hemispheres receive equal amounts of indirect sunlight. The equator experiences no seasons as it always receives direct sunlight.
Physical Geography Lecture 04 - Earth's Energy and Seasons 10.03.16
The document discusses Earth's orientation in space and how its axial tilt, precession, and elliptical orbit affect seasonal changes in insolation levels. It explains that Earth's axial tilt varies between 21.5-24.5 degrees over tens of thousands of years, causing variations in seasonal temperatures. The tilt creates solstices when the sun is directly overhead at one of the Tropics, and equinoxes when it is overhead at the equator. Regions receive different levels of solar radiation depending on latitude and season, with implications for Earth's global heat balance.
3.1 - Seasons And Weather
The document summarizes different types of seasons, weather phenomena, and natural disasters:
1) Seasons are caused by the Earth's tilt and revolve around the summer and winter solstices when the sun is directly overhead either the Tropic of Cancer or Capricorn.
2) Weather is influenced by factors like water vapor, landforms, elevation, and air movement. It involves different types of precipitation including snow, rain, and hurricanes.
3) Natural disasters discussed include hurricanes which form over warm ocean waters, tornadoes which can have wind speeds over 300 mph, blizzards with heavy snow and winds, droughts with little rain, and floods from excess rain or runoff.
How did Atmosphere Form
This is a ppt on the formation of the earth's atmosphere stage by stage. It tells about how the formation of different kinds atmosphere took place.
Seasons, Earth, Axial Tilt Lesson PowerPoint
This PowerPoint is one small part of the Astronomy Topics unit from www.sciencepowerpoint.com. This unit consists of a five part 3000+ slide PowerPoint roadmap, 12 page bundled homework package, modified homework, detailed answer keys, 8 pages of unit notes for students who may require assistance, follow along worksheets, and many review games. The homework and lesson notes chronologically follow the PowerPoint slideshow. The answer keys and unit notes are great for support professionals. The activities and discussion questions in the slideshow and meaningful. The PowerPoint includes built-in instructions, visuals, and follow up questions. Also included are critical class notes (color coded red), project ideas, video links, and review games. This unit also includes four PowerPoint review games (110+ slides each with Answers), 38+ video links, lab handouts, activity sheets, rubrics, materials list, templates, guides, and much more. Also included is a 190 slide first day of school PowerPoint presentation. Teaching Duration = 5+ weeks. Areas of Focus in the Astronomy Topics Unit: The Solar System and the Sun, Order of the Planets, Our Sun, Life Cycle of a Star, Size of Stars, Solar Eclipse, Lunar Eclipse, The Inner Planets, Mercury, Venus, Earth, Moon, Craters, Tides, Phases of the Moon, Mars and Moons, Rocketry, Asteroid Belt, NEOs, The Torino Scale, The Outer Planets and Gas Giants, Jupiter / Moons, Saturn / Moons, Uranus / Moons, Neptune / Moons, Pluto's Demotion, The Kuiper Belt, Oort Cloud, Comets / Other, Beyond the Solar System, Types of Galaxies, Blackholes, Extrasolar Planets, The Big Bang, Dark Matter, Dark Energy, The Special Theory of Relativity, Hubble Space Telescope, Constellations, Spacetime and much more. If you have any questions please feel free to contact me. Thanks again and best wishes. Sincerely, Ryan Murphy M.Ed www.sciencepowerpoint@gmail.com
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Physical Geography Lecture 04 - Earth's Energy and Seasons 10.03.16
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Similar to Geo: Chapter Three, Section One
Weather and climate
The atmosphere can be summarized as follows:
1) The atmosphere is the layer of gases surrounding the Earth that makes life possible. It is mainly composed of nitrogen and oxygen and extends thousands of kilometers above the Earth's surface.
2) The atmosphere is divided into layers with different temperatures, thicknesses, and compositions including the troposphere, stratosphere, mesosphere, thermosphere, and exosphere.
3) Key components of the atmosphere include temperature, air pressure, precipitation, and wind, which are all influenced by global and local geographic factors and help determine the weather and climate of different regions.
Weather and climate- CSEC Geography
This document looks at the factors that affect weather and climate. The weather systems that also affect the Caribbean is also examined. These include ITCZ, Hurricanes, Cold Fronts, Easterly waves, Anticyclones
Weather
The atmosphere is divided into layers including the troposphere, stratosphere, mesosphere, thermosphere and exosphere. It extends thousands of kilometres and is composed primarily of nitrogen and oxygen but also contains argon, carbon dioxide and other gases. The temperature, thickness and composition varies between each atmospheric layer.
Weather
The atmosphere is the layer of gases surrounding the Earth that makes life possible. It extends thousands of kilometres and is composed primarily of nitrogen and oxygen, along with other gases. The atmosphere is divided into layers with varying temperatures, thicknesses, and compositions, including the troposphere, stratosphere, mesosphere, thermosphere, and exosphere closest to Earth's surface. Weather describes short-term atmospheric conditions in a particular place, while climate refers to average weather conditions over a longer period of time.
The Weather
The document discusses various topics related to weather including:
1. It defines weather as the short-term state of the atmosphere varying from minutes to weeks and is influenced by factors like temperature, precipitation and wind.
2. It explains key weather phenomena like the water cycle, air masses, jet streams, weather fronts, and how different types of precipitation like rain, snow and hail are formed.
3. It discusses tropical weather patterns including the intertropical convergence zone and how typhoons are formed, and also explains storm surge and the factors that influence its height.
Weather.Climate.Notes.ppt
The document provides an overview of various weather and climate topics:
- It defines weather as the short-term atmospheric conditions in an area and climate as long-term weather patterns over 100+ years.
- Four main factors that influence weather and climate are discussed: the sun, water cycle, atmosphere, and oceans.
- Various weather phenomena are described such as air masses, fronts, pressure systems, winds, humidity, and precipitation.
- Extreme weather events like thunderstorms, tornadoes, lightning, and tropical cyclones are also summarized, along with safety guidelines.
Ch. 20 Notes
Air masses are large bodies of air that bring consistent weather conditions as they move across regions. The US is influenced by continental polar (cP) and maritime tropical (mT) air masses. cP air masses originate in Canada and bring fair weather, while mT air masses originate in the Gulf of Mexico and bring heavy precipitation and humidity to eastern parts of the country. When different air masses meet, they form fronts that are usually accompanied by some form of precipitation. Middle-latitude cyclones are low pressure systems that form along fronts and are the main weather producers in the US, bringing heavy precipitation and winds.
Ea 3.1 weather fronts and storms
Air masses take on the characteristics of the land or water over which they form, bringing moisture and temperatures with them as they move. There are four main types of air masses in North America - polar and tropical, which form far from and near the equator, and continental and maritime, which gain moisture over land and water. Weather fronts occur when different air masses meet, and can be cold, warm, or stationary. Cold fronts move quickly and bring rising air, condensation, and storms, while warm fronts rise more slowly and bring steady precipitation.
Weather and climate 7C
The document discusses various topics related to weather and climate. It defines weather as short-term atmospheric conditions while climate refers to long-term weather patterns. It then covers factors that affect weather like temperature, precipitation, air pressure, wind and humidity. It explains how these factors are measured and discusses different cloud types, pressure systems, rainfall types, atmospheric layers and microclimates.
Introduction to GCSE Weather
Low pressure systems such as depressions and cyclones bring changeable weather with clouds, rain, and strong winds as warm and cold air masses interact. They form as warm air is drawn northward by the jet stream and meets cold polar air, causing condensation. Three types of fronts separate the air masses: warm, cold, and occluded. High pressure systems such as anticyclones bring more stable weather with clear skies. Over land in summer they result in warm, sunny conditions and in winter they bring cold temperatures and frost at night.
Meterology
Meteorology is the study of atmospheric processes and weather events. Weather describes current atmospheric conditions that change daily, while climate refers to long-term weather patterns over large areas. Air masses form over different surfaces and interact, causing weather systems like cold fronts, warm fronts, and pressure systems that produce clouds, precipitation, and storms. Thunderstorms occur when moist air rises and cools, allowing water to condense and fall as rain. Extreme weather events include tornadoes, which form during clashes of air masses, and tropical cyclones over warm oceans. Meteorologists use tools like thermometers, barometers, and radar to analyze weather data and make forecasts.
Weather And Climate
The document provides an overview of weather and climate concepts. It discusses the water cycle, factors that affect weather like the sun, atmosphere, oceans, and how weather occurs in the troposphere. It also defines climate as the long-term patterns over large areas, and describes the three main climate zones: polar, temperate, and tropical. Storms like thunderstorms, hurricanes, and tornadoes are also summarized.
Weather Powerpoint for Mr Thomas's Class
Thunderstorms form through convection, where warm air rises and cold air sinks. A thunderstorm involves an updraft of warm air carrying water droplets that freeze to form hail, and a downdraft of cold air that brings rain and can produce strong winds. Thunderstorms occur along weather fronts, where warm and cold air masses meet, or in areas with unstable atmospheric conditions. Accurately predicting thunderstorms and their impacts is challenging due to the complex equations governing atmospheric processes.
MAST_-_Introduction2MET.ppt
This document provides an overview of an introductory meteorology course. It discusses key weather elements like temperature, pressure, humidity and clouds. It also covers weather phenomena like storms, fronts and maps. Satellite images are used to view weather patterns. The document outlines different types of storms and careers in meteorology. Weather and climate are explored in how they impact our lives and environment.
Ch 16 weather
Weather refers to the current state of the atmosphere regarding elements like temperature, wind, and moisture. Various factors influence weather, including the sun heating the air and evaporating water from surfaces, which forms clouds and can lead to precipitation when the water condenses. Weather patterns result from the movement of air masses with different properties interacting, such as cold fronts where colder air advances under warmer air. Meteorologists study weather to make forecasts by analyzing weather maps, temperature and pressure readings, and storm conditions.
Global-Circulation-of-the-Atmosphere.pptx
The document discusses the global atmospheric circulation system and how it influences climate around the world. It is divided into three main circulation cells: the Hadley cell near the equator where air rises and sinks, creating tropical climates; the Ferrel cell in mid-latitudes where polar and tropical air interact, producing temperate climates; and the Polar cell where cold air sinks at the poles and flows poleward, resulting in polar climates. Together these cells drive wind and air pressure patterns that determine the distribution of the main climate zones across the Earth.
Weather elements and factors
This chapter discusses weather and climate. It defines weather as short-term atmospheric conditions, while climate refers to longer-term patterns over 30-35 years. Weather is described by temperature, humidity, precipitation, pressure and winds. Temperature is influenced by factors like latitude, altitude, distance from the sea, and cloud cover. Humidity refers to water vapor in the air. Precipitation forms as rain or snow depending on temperature. Air pressure decreases with altitude as air molecules are farther apart. Winds blow from high to low pressure areas. Sea and land breezes are influenced by differences in how land and sea absorb heat.
Air and Sea Interactions Notes
1. Global wind patterns are driven by uneven heating of the Earth's surface and the Coriolis effect.
2. Thermal convection cycles move warm, moist air upwards and polewards, creating deserts at 30 degrees latitude.
3. El Nino events occur when warm water spreads in the Pacific, weakening trade winds and altering weather worldwide.
Chapter 2 Weather Su09
This document summarizes information about hurricanes, weather, climate, and atmospheric conditions. It discusses Hurricane Bertha in 1996 that caused damage in the Caribbean and eastern US. It then provides an overview of typical weather phenomena and how extreme events occasionally emerge. It describes how weather is recorded and climate is characterized. It explains that the troposphere is the lowest layer of the atmosphere. It discusses objectives to understand the lower atmosphere and how weather affects climate. It outlines factors that influence air temperature like solar radiation, water vapor, cloud cover, surface type, elevation, and air movement.
Weather
This document discusses various weather and climate concepts including:
- The difference between weather (short term changes) and climate (long term changes)
- Key weather variables like temperature, air pressure, precipitation, clouds, and how they are measured
- The water cycle and key terms like evaporation, transpiration, condensation, and dew point
- How cloud base height is determined using a sling psychrometer and dew point charts
- Different air masses and their source regions
- Types of precipitation and the factors that determine whether it will be rain, snow, sleet, hail
- Extreme weather events like hurricanes, tornadoes, blizzards caused by lake effect and nor'east
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