Aviation Weather Ppt Iii
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The document discusses the origins and classification of Earth's climate and surface properties. It begins by explaining how the early atmosphere was inhospitable but cooled over hundreds of millions of years. It then describes the Koppen climate classification system which categorizes climates based on temperature and precipitation. The document also notes that the Earth's surface is comprised of shifting tectonic plates beneath a crust, and that factors like water and wind also influence surface changes over time.
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The document provides an overview of relief and water on Earth. It discusses the structure of the Earth and how tectonic plate movements have shaped the continents over hundreds of millions of years. It also describes the main types of continental and oceanic relief that have been formed through internal forces like earthquakes and volcanoes, as well as external forces like erosion. Finally, it examines the distribution of water on Earth, including the characteristics and movements of oceans, seas, and continental freshwater sources.
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The document provides an overview of relief and water on Earth. It discusses the structure of the Earth and how tectonic plate movements have shaped the continents over hundreds of millions of years. It also describes the main types of continental and oceanic relief that have been formed through internal forces like earthquakes and volcanoes, as well as external forces like erosion. Finally, it examines the distribution of water on Earth, including the characteristics and movements of oceans, seas, and continental freshwater sources.
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1) The document is an activity worksheet about relief and water on Earth. It contains questions about diagrams of Earth's interior, tectonic plates, volcanoes and earthquakes.
2) It also asks students to identify features of rivers and coastlines like deltas, tributaries, and meanders on a diagram.
3) Students are tasked with describing a picture using coastal and river terminology.
4) The document provides a reading on issues around access to clean water and asks related questions to assess comprehension. Key points are the health impacts of contaminated water, efforts to expand access, and proposed solutions like more efficient agriculture.
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2) Fahrenheit uses 32°F as the freezing point of water and 212°F as the boiling point. Celsius uses 0°C as the freezing point and 100°C as the boiling point. Kelvin uses 0K as absolute zero. Water freezes at 273.15K and boils at 373.15K.
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This document provides an overview of the structure and composition of Earth. It discusses:
1) Earth's surface dimensions, relief, and ocean floors. The surface varies from high mountains to ocean depths of over 11km. Ocean floors have been mapped using seismic methods.
2) The solid interior of Earth, which can be studied directly to depths of a few km and extrapolated to greater depths. Temperature increases downward, and the core is composed of iron and nickel.
3) Earth is divided into spheres - the atmosphere, hydrosphere, biosphere, and geosphere. The geosphere includes the crust, mantle, and core layers. The crust and upper mantle form the lithosphere.
Weather basics
1) Earth's climate system is driven by solar radiation and the interactions between the atmosphere, oceans, and their circulation patterns.
2) The atmosphere consists mostly of nitrogen and oxygen and varies in temperature, humidity, and pressure with latitude and altitude. Uneven heating from the sun causes variations in these factors across Earth's surface.
3) Oceans are made of water and dissolved salts. Ocean circulation is driven by winds, temperature/salinity differences, and upwelling, and helps redistribute heat globally.
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Details of the Earth–Moon system, showing the radius of each object and the Earth–Moon barycenter. The Moon's axis is located by Cassini's third law.
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The document discusses the structure and relief of the Earth. It describes how the Earth is divided into layers including the crust, mantle, and core. It explains how plate tectonics has shaped the Earth's geography over millions of years, including forming continents and oceans. Specifically, it notes that around 200 million years ago all the continents were joined together in a supercontinent called Pangaea, which has since broken apart due to plate movement.
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Grade 6. chapter 5. realms of the earth..
The Earth divided into 4 realms which are interconnected.
The names of the 4 spheres have been derived from Greek words for stone (litho), air (atmo), water (hydro), and life (bio)
The layer of the gas that surrounds the Earth is called atmosphere.
The atmosphere protects Earth from absorbing the harmful ultraviolet rays of the Sun.
It also acts as a blanket around the Earth.
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The document describes the four major realms that make up the Earth - the lithosphere, hydrosphere, atmosphere, and biosphere. It provides details on each realm:
The lithosphere includes the crust and upper mantle of the Earth. It is the rigid outer shell. The hydrosphere is all the water on, under, and over the Earth's surface, including oceans, lakes, rivers, groundwater, and atmospheric water. The atmosphere is a layer of gases surrounding the planet, composed primarily of nitrogen, oxygen, and trace amounts of other gases like carbon dioxide. It is divided into four layers - troposphere, stratosphere, mesosphere, and thermosphere. The biosphere encompasses all
Unit 2 activities
1) The document is an activity worksheet about relief and water on Earth. It contains questions about diagrams of Earth's interior, tectonic plates, volcanoes and earthquakes.
2) It also asks students to identify features of rivers and coastlines like deltas, tributaries, and meanders on a diagram.
3) Students are tasked with describing a picture using coastal and river terminology.
4) The document provides a reading on issues around access to clean water and asks related questions to assess comprehension. Key points are the health impacts of contaminated water, efforts to expand access, and proposed solutions like more efficient agriculture.
Intro to Meteorology: Our Atmosphere
Here are the key points about heat and temperature scales:
1) Heat is the total amount of thermal energy in an object or system. Temperature is a measure of how hot or cold something is compared to a reference point.
2) Fahrenheit uses 32°F as the freezing point of water and 212°F as the boiling point. Celsius uses 0°C as the freezing point and 100°C as the boiling point. Kelvin uses 0K as absolute zero. Water freezes at 273.15K and boils at 373.15K.
3) Dew point is the temperature at which water vapor in air will condense into liquid water. Condensation occurs when air reaches saturation point and can hold no
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The document discusses the composition and structure of Earth's atmosphere. It is composed primarily of nitrogen and oxygen, with smaller amounts of gases like carbon dioxide, argon, and methane. The atmosphere is divided into four layers - the troposphere closest to Earth's surface where weather occurs, the stratosphere above it where ozone absorbs UV light, the mesosphere where temperatures decrease with altitude, and the thermosphere where temperatures increase with altitude. The greenhouse effect describes how certain gases in the atmosphere trap heat radiating from Earth's surface, maintaining a climate suitable for life.
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Few global trends have been as controversial as climate change and the Earth’s warming. The Earth has gone through many shifts in cooling and warming driven by natural factors like the sun’s energy or variations in its orbit, but the trend scientists have seen over the past 50 years is unmistakable.
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This document provides an overview of the structure and composition of Earth. It discusses:
1) Earth's surface dimensions, relief, and ocean floors. The surface varies from high mountains to ocean depths of over 11km. Ocean floors have been mapped using seismic methods.
2) The solid interior of Earth, which can be studied directly to depths of a few km and extrapolated to greater depths. Temperature increases downward, and the core is composed of iron and nickel.
3) Earth is divided into spheres - the atmosphere, hydrosphere, biosphere, and geosphere. The geosphere includes the crust, mantle, and core layers. The crust and upper mantle form the lithosphere.
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1) Earth's climate system is driven by solar radiation and the interactions between the atmosphere, oceans, and their circulation patterns.
2) The atmosphere consists mostly of nitrogen and oxygen and varies in temperature, humidity, and pressure with latitude and altitude. Uneven heating from the sun causes variations in these factors across Earth's surface.
3) Oceans are made of water and dissolved salts. Ocean circulation is driven by winds, temperature/salinity differences, and upwelling, and helps redistribute heat globally.
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This document provides a summary of key topics related to air, weather, and climate:
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Climate is determined by temperature and precipitation, which are affected by various natural factors. Latitude affects temperature, with warmer temperatures closer to the equator and colder temperatures farther from the equator. Elevation also impacts temperature, with higher elevations experiencing cooler temperatures due to less dense air. Ocean currents influence nearby land temperatures, with warm or cold currents causing temperature variations. Precipitation is impacted by prevailing winds and mountain ranges, with windward sides of mountains receiving more rain and leeward sides receiving less. The world's climates can be divided into polar, temperate, and tropical zones based on average temperatures.
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Climatology is the scientific study of climate and a major branch of meteorology. There are three approaches to climatology: physical, descriptive, and dynamic. Physical climatology seeks to explain climate differences based on physical processes influencing climate. Descriptive climatology orients itself geographically and describes climates regionally without causal explanations. Dynamic climatology relates atmospheric circulation to climate. Climate is influenced by various physical and biological processes in the oceans and atmosphere.
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Climatology is the scientific study of climate and a major branch of meteorology. There are three approaches to climatology: physical, descriptive, and dynamic. Physical climatology seeks to explain climate differences based on physical processes. Descriptive climatology orients itself geographically and describes climates regionally without causes. Dynamic climatology relates atmospheric circulation to climate. Climate is influenced by both physical processes like ocean currents and heat transport, and biological processes in the oceans like the biological pump. Changes in elements like temperature, precipitation, wind and others are driven by factors like latitude, land-sea distribution, and topography.
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The atmosphere can be summarized as follows:
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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.
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This document discusses the Earth's atmosphere and climate. It begins by describing the different layers of the atmosphere, including the troposphere, stratosphere, mesosphere, thermosphere, and exosphere. It then discusses the key properties of air, such as its composition, temperature, atmospheric pressure, and relative humidity. Next, it differentiates between weather and climate, and lists some factors that influence weather like atmospheric pressure, temperature, wind, and humidity/precipitation. Finally, it outlines the Earth's major climate zones of cold, hot, and temperate, and provides examples of different climate types within those zones, like Mediterranean, continental, oceanic, equatorial, tropical, and polar climates. Maps and diagrams
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Climate refers to average weather conditions over long periods of time and is defined by patterns of temperature and precipitation. It is shaped by factors like solar energy, latitude, and wind and ocean currents. Solar energy heats the Earth's surface unevenly based on latitude, creating different climate zones. Greenhouse gases in the atmosphere, like carbon dioxide and methane, trap heat and control the planet's average temperature through the greenhouse effect. Wind and ocean currents also transport heat from warmer to cooler regions around the globe.
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The document summarizes how various physical factors influence Earth's climate:
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The document discusses several key topics related to climate change:
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