Climate graphs quiz
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GemaThis document describes several different climate types including continental, oceanic, polar, Mediterranean, humid tropical, equatorial, dry tropical, hot desert, and mountain climates. It provides brief definitions and key characteristics for each climate type, such as precipitation levels and seasonal patterns.
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Weather maps and their symbols
The document discusses weather maps and how they are used to predict weather conditions. It provides information on several key topics:
- The atmosphere helps regulate Earth's temperature and creates weather through the movement of air masses. Weather maps show current conditions.
- Weather is influenced by properties like temperature, humidity and pressure. Maps depict systems like cold fronts, warm fronts and stationary fronts to understand weather changes.
- High and low pressure areas circulate clockwise and counterclockwise respectively, affecting wind patterns and whether conditions will be clear or stormy. Weather maps are interpreted to forecast upcoming weather.
AIR MASSES AND FRONT
The document discusses air masses and fronts. It defines air masses as large bodies of air with uniform properties that form over land or water surfaces. There are four main types of air masses classified by their region of formation: maritime/continental and polar/tropical. Fronts are boundaries between unlike air masses. There are three main types of fronts: cold fronts, where cold air overtakes warm air; warm fronts, where warm air overtakes cold air; and occluded fronts, where a warm air mass is overtaken by two cooler air masses.
Thunderstorms
Thunderstorms are formed by cumulonimbus clouds and are characterized by lightning and thunder. They develop when certain atmospheric conditions are met, such as unstable lapse rates and sufficient water vapor. Thunderstorms can be triggered by different mechanisms like surface heating, frontal lifting, orographic lifting, and convergence. There are different types of thunderstorms including single cell, multicell, and supercells. Thunderstorms pose various hazards to aviation like turbulence, icing, hail, wind shear, lightning, tornadoes, and microbursts. Pilots can detect and avoid thunderstorms using weather radar and visual sighting, and recommended distances of avoidance depend on aircraft altitude.
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.
Air Masses
An air mass is a large volume of air that takes on consistent temperature and humidity characteristics based on the region over which it travels. There are four main types of air masses: maritime tropical (warm and humid), continental tropical (warm and dry), maritime polar (cold and humid), and continental polar (cold and dry). Weather patterns change as different air masses are pushed around the Earth by forces like the jet stream, which generally moves air masses from west to east across the United States.
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.
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.
Elements of climate gif
The document discusses the main elements of climate: temperature, precipitation, humidity, atmospheric pressure, and wind. It defines each element and describes tools used to measure them such as rain gauges, hygrometers, barometers, and anemometers. Additional factors that influence climate are also outlined, including latitude, altitude, distribution of land/water, orographic barriers, pressure/wind systems, ocean currents, and storms.
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Weather maps and their symbols
The document discusses weather maps and how they are used to predict weather conditions. It provides information on several key topics:
- The atmosphere helps regulate Earth's temperature and creates weather through the movement of air masses. Weather maps show current conditions.
- Weather is influenced by properties like temperature, humidity and pressure. Maps depict systems like cold fronts, warm fronts and stationary fronts to understand weather changes.
- High and low pressure areas circulate clockwise and counterclockwise respectively, affecting wind patterns and whether conditions will be clear or stormy. Weather maps are interpreted to forecast upcoming weather.
AIR MASSES AND FRONT
The document discusses air masses and fronts. It defines air masses as large bodies of air with uniform properties that form over land or water surfaces. There are four main types of air masses classified by their region of formation: maritime/continental and polar/tropical. Fronts are boundaries between unlike air masses. There are three main types of fronts: cold fronts, where cold air overtakes warm air; warm fronts, where warm air overtakes cold air; and occluded fronts, where a warm air mass is overtaken by two cooler air masses.
Thunderstorms
Thunderstorms are formed by cumulonimbus clouds and are characterized by lightning and thunder. They develop when certain atmospheric conditions are met, such as unstable lapse rates and sufficient water vapor. Thunderstorms can be triggered by different mechanisms like surface heating, frontal lifting, orographic lifting, and convergence. There are different types of thunderstorms including single cell, multicell, and supercells. Thunderstorms pose various hazards to aviation like turbulence, icing, hail, wind shear, lightning, tornadoes, and microbursts. Pilots can detect and avoid thunderstorms using weather radar and visual sighting, and recommended distances of avoidance depend on aircraft altitude.
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.
Air Masses
An air mass is a large volume of air that takes on consistent temperature and humidity characteristics based on the region over which it travels. There are four main types of air masses: maritime tropical (warm and humid), continental tropical (warm and dry), maritime polar (cold and humid), and continental polar (cold and dry). Weather patterns change as different air masses are pushed around the Earth by forces like the jet stream, which generally moves air masses from west to east across the United States.
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.
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.
Elements of climate gif
The document discusses the main elements of climate: temperature, precipitation, humidity, atmospheric pressure, and wind. It defines each element and describes tools used to measure them such as rain gauges, hygrometers, barometers, and anemometers. Additional factors that influence climate are also outlined, including latitude, altitude, distribution of land/water, orographic barriers, pressure/wind systems, ocean currents, and storms.
Weather fronts
The document discusses different types of fronts including warm fronts, cold fronts, occluded fronts, and stationary fronts. It provides details on their formation, identification, and typical associated weather patterns. Warm fronts have a gradual slope and rising warm air overrides cooler air. Cold fronts have a steeper slope and faster movement as colder air advances. An occluded front is formed when a cold front catches up to a warm front. Stationary fronts have little or no movement with gentle precipitation possible.
Fronts and Air Masses
Fronts occur where two different air masses meet but do not mix. There are four main types of fronts: cold fronts, warm fronts, stationary fronts, and occluded fronts. Cold fronts move quickly and bring cooler, drier air behind them, often causing rain and storms. Warm fronts move more slowly and bring cloudy skies and light rain before warmer, more humid air moves in. Stationary fronts occur when neither air mass can push the other, resulting in prolonged wet weather. Occluded fronts form when a warm air mass gets trapped between two cold fronts.
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, 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.
Chapter 11 Weather and Climate lesson slides published
Dear 2C and 2G,
Attached are the lesson slides for Chapter 11 on Weather and Climate.
The Earth is fragile, everyone plays a part!
Mr Tan
Lesson 17: Weather and Climate
TEMPERATURE
COMPOSITION OF THE ATMOSPHERE
Layers of the ATMOSPHERE
WEATHER and CLIMATE
LATITUDINAL ZONES
ELEMENTS & CONTROLS OF WEATHER & CLIMATE
WARM MAJOR CURRENTS OF THE WORLD
Land Breeze & Sea Breeze
Air masses and fronts
Air masses are large bodies of air that maintain consistent temperatures and moisture levels as they move across regions. They are classified by their source location and surface, resulting in four main types: continental polar, continental tropical, maritime polar, and maritime tropical. When two air masses meet, fronts form along the boundary which can cause precipitation. The main front types are warm, cold, stationary, and occluded fronts, which differ based on the advancing air mass temperature and resulting weather impacts.
frigid zone
The document is about the Frigid Zone, which includes:
- The areas from 66.5°N to 90°N in the Northern Hemisphere and 66.5°S to 90°S in the Southern Hemisphere.
- It has cold summers and cold winters, with summers lasting 50-60 days. Winds include nor'easters and polar easterlies in the north, and katabatic winds in the south.
- Vegetation includes mosses, sedges, lichens, bearberry, and diamond leaf willow in the northern tundra regions.
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.
Weather And Climate
1. The document discusses weather elements such as temperature, precipitation, wind speed, and cloud cover. It also describes how these elements are measured using instruments like a thermometer, rain gauge, and anemometer.
2. Common types of clouds are described as cirrus, cumulonimbus, cumulus, and stratus. The Stevenson screen, used to shelter instruments, is also characterized.
3. The difference between weather and climate is explained as weather referring to short term atmospheric conditions while climate describes average conditions over a long period.
Working with climate data
This document discusses the role of Climate Services Information Systems (CSIS) in supporting National Adaptation Plans (NAPs). CSIS provide climate data at various timescales from months to decades, including weather forecasts, climate models and scenarios. They are supported by global and regional climate centers that collect data from observational networks and produce climate information products. CSIS can help NAPs by providing location-specific data on extreme weather events and potential sectoral impacts, as well as establishing climate outlook forums and national frameworks for climate services. The document outlines several examples of climate indicators and indexes that CSIS produce to monitor extremes, such as drought and health impacts, as well as initiatives to strengthen CSIS support for NAPs.
Climate
Climate is defined as the average weather in a region over a long period of time, typically 30 years. It is influenced by factors like latitude, altitude, proximity to bodies of water and oceans, and vegetation. There are several classification systems for climates, most commonly the Köppen system which categorizes climates as tropical, temperate, or polar. Tropical climates have high temperatures year-round, temperate climates have distinct seasons with moderate temperature changes, and polar climates are very cold with no warm summers. Paleoclimatology studies past climates through proxies like sediments and tree rings since direct observations are only available recently.
POLAR REGION
The polar regions have a polar climate characterized by lack of warm summers, with average monthly temperatures below 10°C. They cover over 20% of the Earth's surface and result in treeless tundra, glaciers, or permanent ice layers. Precipitation is also very low due to cold air's inability to hold much water vapor, with some areas receiving under 10 inches annually like subtropical deserts. Housing must be built on poles driven into the frozen permafrost ground, while inhabitants live in igloos or skin tents depending on the season.
Weather and Climate
This document provides an overview of weather and climate concepts. It discusses how weather is caused by differences in temperature and air pressure between locations. It also describes common weather phenomena and how weather is forecasted using various instruments and models. The document outlines different climate zones and variables that influence climate. It explains phenomena like El Niño and hurricanes and how climate change is impacting environments and societies.
Weather Types Of Clouds
Cirrus clouds are very high and wispy ice crystals. Cumulus clouds are mid-level fluffy lumps of condensed vapor. Stratus clouds are layers of condensed vapor. Nimbus clouds are clouds that may cause precipitation. Cumulonimbus clouds are very tall and fluffy clouds that can cause heavy rains. When a cold front collides with a warm front, the warm moist air is pushed upwards.
Weather Maps and Symbols
Different types of weather maps and whay symbols they use to give us diffrent information about how the weather is on a particular day.
Equatorial climate. rainforests
Equatorial rainforests are located near the equator in areas like the Amazon, Central America, Congo, Gulf of Guinea, and Southeast Asia. These regions have high, consistent temperatures averaging 25°C and heavy rainfall exceeding 2,000 mm per year with no distinct dry season. Equatorial rainforests are home to an abundance of plant and animal life including tall trees, snakes, frogs, jaguars, colorful birds, and rare species in Indonesia. However, humans are destroying equatorial rainforest habitats through deforestation to harvest wood and clear land for agriculture.
Comentario De Un Mapa Del Tiempo
Este documento explica el proceso para hacer un comentario de un mapa del tiempo. Primero se identifican elementos como isobaras, centros de acción y frentes. Luego se analizan los datos de estas características para predecir el tiempo, incluyendo precipitaciones, temperaturas, humedad y viento. Finalmente, se discuten situaciones meteorológicas típicas en España como verano, invierno y otoño/primavera.
Thunderstorms
The document discusses thunderstorms and provides safety information. It defines a thunderstorm and explains that they require moisture, unstable air, and lift. Lightning is caused by the buildup of positive and negative charges, while thunder comes from lightning setting off sound waves. The document advises that if thunder roars to go indoors, as being outside is dangerous during a storm. It also provides tips for indoor safety during a thunderstorm and what to do if someone is struck by lightning.
Chapter five
This document summarizes key concepts about atmospheric pressure and global wind patterns from a geography textbook chapter. It defines important terms like isobars, high and low pressure systems, and describes the major wind systems - including the trade winds, westerlies, and polar easterlies - that make up the general circulation of the atmosphere. Specific wind patterns like the Hadley cell and subtropical high are explained in terms of atmospheric pressure gradients and the Coriolis effect.
Climates cards
The document describes several major climate types based on location and characteristics. The equatorial climate has little temperature variation and abundant, regular rainfall, supporting lush rainforests. The tropical climate has higher temperatures than the equatorial and alternates between rainy and dry seasons. Hot desert climates have large daily temperature variations, little irregular rainfall, and almost no vegetation. The Mediterranean climate has hot, dry summers and mild, wet winters, supporting forests and shrublands. The oceanic climate has mild, wet weather year-round, with abundant rainfall supporting forests and grasslands. The continental climate has extreme temperature variations between hot summers and cold winters and low, scattered rainfall, with taiga forests and steppes.
2011 year 8 geography - rainforests - climate graphs
Madang, Papua New Guinea has a tropical climate with high temperatures year-round that average between 24-32 degrees Celsius. Rainfall is heavy throughout the year in Madang, averaging over 200mm per month with the wettest months between December and April when rainfall can exceed 400mm. The climate graph shows Madang has consistent warm temperatures and heavy rainfall without distinct wet and dry seasons.
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Weather fronts
The document discusses different types of fronts including warm fronts, cold fronts, occluded fronts, and stationary fronts. It provides details on their formation, identification, and typical associated weather patterns. Warm fronts have a gradual slope and rising warm air overrides cooler air. Cold fronts have a steeper slope and faster movement as colder air advances. An occluded front is formed when a cold front catches up to a warm front. Stationary fronts have little or no movement with gentle precipitation possible.
Fronts and Air Masses
Fronts occur where two different air masses meet but do not mix. There are four main types of fronts: cold fronts, warm fronts, stationary fronts, and occluded fronts. Cold fronts move quickly and bring cooler, drier air behind them, often causing rain and storms. Warm fronts move more slowly and bring cloudy skies and light rain before warmer, more humid air moves in. Stationary fronts occur when neither air mass can push the other, resulting in prolonged wet weather. Occluded fronts form when a warm air mass gets trapped between two cold fronts.
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, 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.
Chapter 11 Weather and Climate lesson slides published
Dear 2C and 2G,
Attached are the lesson slides for Chapter 11 on Weather and Climate.
The Earth is fragile, everyone plays a part!
Mr Tan
Lesson 17: Weather and Climate
TEMPERATURE
COMPOSITION OF THE ATMOSPHERE
Layers of the ATMOSPHERE
WEATHER and CLIMATE
LATITUDINAL ZONES
ELEMENTS & CONTROLS OF WEATHER & CLIMATE
WARM MAJOR CURRENTS OF THE WORLD
Land Breeze & Sea Breeze
Air masses and fronts
Air masses are large bodies of air that maintain consistent temperatures and moisture levels as they move across regions. They are classified by their source location and surface, resulting in four main types: continental polar, continental tropical, maritime polar, and maritime tropical. When two air masses meet, fronts form along the boundary which can cause precipitation. The main front types are warm, cold, stationary, and occluded fronts, which differ based on the advancing air mass temperature and resulting weather impacts.
frigid zone
The document is about the Frigid Zone, which includes:
- The areas from 66.5°N to 90°N in the Northern Hemisphere and 66.5°S to 90°S in the Southern Hemisphere.
- It has cold summers and cold winters, with summers lasting 50-60 days. Winds include nor'easters and polar easterlies in the north, and katabatic winds in the south.
- Vegetation includes mosses, sedges, lichens, bearberry, and diamond leaf willow in the northern tundra regions.
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.
Weather And Climate
1. The document discusses weather elements such as temperature, precipitation, wind speed, and cloud cover. It also describes how these elements are measured using instruments like a thermometer, rain gauge, and anemometer.
2. Common types of clouds are described as cirrus, cumulonimbus, cumulus, and stratus. The Stevenson screen, used to shelter instruments, is also characterized.
3. The difference between weather and climate is explained as weather referring to short term atmospheric conditions while climate describes average conditions over a long period.
Working with climate data
This document discusses the role of Climate Services Information Systems (CSIS) in supporting National Adaptation Plans (NAPs). CSIS provide climate data at various timescales from months to decades, including weather forecasts, climate models and scenarios. They are supported by global and regional climate centers that collect data from observational networks and produce climate information products. CSIS can help NAPs by providing location-specific data on extreme weather events and potential sectoral impacts, as well as establishing climate outlook forums and national frameworks for climate services. The document outlines several examples of climate indicators and indexes that CSIS produce to monitor extremes, such as drought and health impacts, as well as initiatives to strengthen CSIS support for NAPs.
Climate
Climate is defined as the average weather in a region over a long period of time, typically 30 years. It is influenced by factors like latitude, altitude, proximity to bodies of water and oceans, and vegetation. There are several classification systems for climates, most commonly the Köppen system which categorizes climates as tropical, temperate, or polar. Tropical climates have high temperatures year-round, temperate climates have distinct seasons with moderate temperature changes, and polar climates are very cold with no warm summers. Paleoclimatology studies past climates through proxies like sediments and tree rings since direct observations are only available recently.
POLAR REGION
The polar regions have a polar climate characterized by lack of warm summers, with average monthly temperatures below 10°C. They cover over 20% of the Earth's surface and result in treeless tundra, glaciers, or permanent ice layers. Precipitation is also very low due to cold air's inability to hold much water vapor, with some areas receiving under 10 inches annually like subtropical deserts. Housing must be built on poles driven into the frozen permafrost ground, while inhabitants live in igloos or skin tents depending on the season.
Weather and Climate
This document provides an overview of weather and climate concepts. It discusses how weather is caused by differences in temperature and air pressure between locations. It also describes common weather phenomena and how weather is forecasted using various instruments and models. The document outlines different climate zones and variables that influence climate. It explains phenomena like El Niño and hurricanes and how climate change is impacting environments and societies.
Weather Types Of Clouds
Cirrus clouds are very high and wispy ice crystals. Cumulus clouds are mid-level fluffy lumps of condensed vapor. Stratus clouds are layers of condensed vapor. Nimbus clouds are clouds that may cause precipitation. Cumulonimbus clouds are very tall and fluffy clouds that can cause heavy rains. When a cold front collides with a warm front, the warm moist air is pushed upwards.
Weather Maps and Symbols
Different types of weather maps and whay symbols they use to give us diffrent information about how the weather is on a particular day.
Equatorial climate. rainforests
Equatorial rainforests are located near the equator in areas like the Amazon, Central America, Congo, Gulf of Guinea, and Southeast Asia. These regions have high, consistent temperatures averaging 25°C and heavy rainfall exceeding 2,000 mm per year with no distinct dry season. Equatorial rainforests are home to an abundance of plant and animal life including tall trees, snakes, frogs, jaguars, colorful birds, and rare species in Indonesia. However, humans are destroying equatorial rainforest habitats through deforestation to harvest wood and clear land for agriculture.
Comentario De Un Mapa Del Tiempo
Este documento explica el proceso para hacer un comentario de un mapa del tiempo. Primero se identifican elementos como isobaras, centros de acción y frentes. Luego se analizan los datos de estas características para predecir el tiempo, incluyendo precipitaciones, temperaturas, humedad y viento. Finalmente, se discuten situaciones meteorológicas típicas en España como verano, invierno y otoño/primavera.
Thunderstorms
The document discusses thunderstorms and provides safety information. It defines a thunderstorm and explains that they require moisture, unstable air, and lift. Lightning is caused by the buildup of positive and negative charges, while thunder comes from lightning setting off sound waves. The document advises that if thunder roars to go indoors, as being outside is dangerous during a storm. It also provides tips for indoor safety during a thunderstorm and what to do if someone is struck by lightning.
Chapter five
This document summarizes key concepts about atmospheric pressure and global wind patterns from a geography textbook chapter. It defines important terms like isobars, high and low pressure systems, and describes the major wind systems - including the trade winds, westerlies, and polar easterlies - that make up the general circulation of the atmosphere. Specific wind patterns like the Hadley cell and subtropical high are explained in terms of atmospheric pressure gradients and the Coriolis effect.
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Chapter 11 Weather and Climate lesson slides published
Chapter 11 Weather and Climate lesson slides published
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Climates cards
The document describes several major climate types based on location and characteristics. The equatorial climate has little temperature variation and abundant, regular rainfall, supporting lush rainforests. The tropical climate has higher temperatures than the equatorial and alternates between rainy and dry seasons. Hot desert climates have large daily temperature variations, little irregular rainfall, and almost no vegetation. The Mediterranean climate has hot, dry summers and mild, wet winters, supporting forests and shrublands. The oceanic climate has mild, wet weather year-round, with abundant rainfall supporting forests and grasslands. The continental climate has extreme temperature variations between hot summers and cold winters and low, scattered rainfall, with taiga forests and steppes.
2011 year 8 geography - rainforests - climate graphs
Madang, Papua New Guinea has a tropical climate with high temperatures year-round that average between 24-32 degrees Celsius. Rainfall is heavy throughout the year in Madang, averaging over 200mm per month with the wettest months between December and April when rainfall can exceed 400mm. The climate graph shows Madang has consistent warm temperatures and heavy rainfall without distinct wet and dry seasons.
Climate graph
A climate graph combines a bar graph of monthly rainfall measured in millimeters with a line graph of monthly temperature measured in degrees. It shows these two climate factors on the same graph to illustrate the typical weather patterns over the course of a year for a particular location. An example climate graph is provided for Christchurch that charts rainfall and temperature levels each month.
How to create a climate graph
The tundra biome is characterized by low temperatures and average rainfall. Plants found in the tundra include grasses, shrubs, mosses and lichens. Animals include snow geese, musk oxen, wolves and caribou. Permafrost, a layer of soil that remains frozen all year round, is also mentioned. The document then provides instructions for creating a climate graph, including drawing axes, adding months, temperature, rainfall data and completing the graph.
How to analyze a climate graph
This document provides instructions on how to analyze a climate graph by examining the average and seasonal temperatures, precipitation amounts and distribution, and using that information to deduce the type of climate and related ecosystem. Key parts to analyze are the average and extreme temperatures throughout the year, whether seasons are hot/cold/mild, total precipitation and how it is distributed between wet and dry seasons or months.
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How to create a climate graph
The document provides instructions for creating a climate graph to compare the monthly temperature and rainfall patterns in Nairobi and London. It involves 6 steps: 1) Draw axes for months, temperature, and rainfall. 2) Add the months to the x-axis. 3) Add the temperature scale to the left y-axis. 4) Add the rainfall scale to the right y-axis. 5) Add the monthly rainfall data points. 6) Add the monthly temperature line. Following these 6 steps will result in a completed climate graph.
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The document outlines three major climatic types: tropical, temperate, and polar. Tropical climates near the equator have high rainfall between 1000-2000 mm and temperatures from 20-30°C. Temperate climates between the tropics and polar circles experience summer highs of 34°C and winter lows below 0°C with rainfall of 300-1000 mm. Polar climates within the polar circles have low rainfall and temperatures.
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A trivia presentation to boggle the mind of the sleepy training/seminar participants. Can be given before or during the lecture or session. I usually use this in my session on Copyreading and Headline Writing in Journalism. It is also usable to other topics. This is my personal presentation I gathered from an old Reader's Digest. Here are the answers for this presentation: 1. Moscow 2. Manila 3. Budapest 4.Bogota 5. Canberra 6. Santiago 7. London 8. Wellington 9.Tripoli 10. Helsinki 11. Ankara 12. Ottawa 13. Cape Town
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Word Game: Fire up your brain
A trivia presentation to boggle the mind of the sleepy training/seminar participants. Can be given before or during the lecture or session. I usually use this during my lecture in Copyreading and Headline Writing session. This is a personal presentation I gathered from an old Reader's Digest.
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The document provides information on how to write an editorial or opinion piece. It discusses that an editorial presents the official view of a paper and is composed by an editorial board. It should deal with a current issue in an objective manner while potentially influencing readers. When writing an editorial or opinion piece, it is important to state the problem, express an opinion, offer a solution, and conclude by emphasizing the main issue. The opposition view should also be presented and refuted in a balanced manner.
Word Game: Reading Between Lines
A trivia presentation to boggle the mind of the sleepy training/seminar participants. Can be given before or during the lecture or session. This is my personal presentation I gathered from an old Reader's Digest. Answers are 1. seal 2. gorilla 3. dog 4. owl 5. rat 6. ape 7.deer 8.goat 9.cat 10.hen 11.goat 12.horse 13.ant/cat 14.rabbit 15.monkey 16.dog 17.kitten 18.wasp 19.snake 20.hen
Optical Illusion: Can you trust your own eyes
A trivia presentation to boggle the mind of the sleepy training participants. Can be given before or during the lecture or session. This is my personal presentation I gathered from an old Reader's Digest.
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Different climatic regions of the world
The document identifies and describes the five major climate zones on Earth: tropical, temperate, polar, dry, and highland/mountain. Tropical climates occur near the equator and are characterized by warm, rainy weather year-round with temperatures around 80°F. Temperate climates occur in middle latitudes and have distinct seasons, with warm summers and cold, snowy winters. Polar climates are located near the poles and have extremely cold weather year-round. Dry and highland climates can occur in many latitudes and depend on elevation, with temperatures and plant life varying with altitude.
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A trivia presentation to boggle the mind of the sleepy training participants. Can be given before or during the lecture or session. This is my personal presentation I gathered from an old Reader's Digest.
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2011 year 8 geography - rainforests - climate graphs
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إضغ بين إيديكم من أقوى الملازم التي صممتها
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1- مُترجمة ترجمة تُناسب جميع المستويات
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Syllabus
Chapter-1
Introduction to objective, scope and outcome the subject
Chapter 2
Introduction: Scope and Specialization of Civil Engineering, Role of civil Engineer in Society, Impact of infrastructural development on economy of country.
Chapter 3
Surveying: Object Principles & Types of Surveying; Site Plans, Plans & Maps; Scales & Unit of different Measurements.
Linear Measurements: Instruments used. Linear Measurement by Tape, Ranging out Survey Lines and overcoming Obstructions; Measurements on sloping ground; Tape corrections, conventional symbols. Angular Measurements: Instruments used; Introduction to Compass Surveying, Bearings and Longitude & Latitude of a Line, Introduction to total station.
Levelling: Instrument used Object of levelling, Methods of levelling in brief, and Contour maps.
Chapter 4
Buildings: Selection of site for Buildings, Layout of Building Plan, Types of buildings, Plinth area, carpet area, floor space index, Introduction to building byelaws, concept of sun light & ventilation. Components of Buildings & their functions, Basic concept of R.C.C., Introduction to types of foundation
Chapter 5
Transportation: Introduction to Transportation Engineering; Traffic and Road Safety: Types and Characteristics of Various Modes of Transportation; Various Road Traffic Signs, Causes of Accidents and Road Safety Measures.
Chapter 6
Environmental Engineering: Environmental Pollution, Environmental Acts and Regulations, Functional Concepts of Ecology, Basics of Species, Biodiversity, Ecosystem, Hydrological Cycle; Chemical Cycles: Carbon, Nitrogen & Phosphorus; Energy Flow in Ecosystems.
Water Pollution: Water Quality standards, Introduction to Treatment & Disposal of Waste Water. Reuse and Saving of Water, Rain Water Harvesting. Solid Waste Management: Classification of Solid Waste, Collection, Transportation and Disposal of Solid. Recycling of Solid Waste: Energy Recovery, Sanitary Landfill, On-Site Sanitation. Air & Noise Pollution: Primary and Secondary air pollutants, Harmful effects of Air Pollution, Control of Air Pollution. . Noise Pollution Harmful Effects of noise pollution, control of noise pollution, Global warming & Climate Change, Ozone depletion, Greenhouse effect
Text Books:
1. Palancharmy, Basic Civil Engineering, McGraw Hill publishers.
2. Satheesh Gopi, Basic Civil Engineering, Pearson Publishers.
3. Ketki Rangwala Dalal, Essentials of Civil Engineering, Charotar Publishing House.
4. BCP, Surveying volume 1
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- 17. Humid Tropical Climate (Monsoon Climate)Humid Tropical Climate (Monsoon Climate)
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- 19. Dry Tropical ClimateDry Tropical Climate Precip: more than 250 mm – less than 1500 mm
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