7th Grade Chapter 5 Lesson 3 Slideshare
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1. The document discusses properties of air and gas laws including Boyle's law, Charles' law, and the combined gas law. 2. Boyle's law states that if temperature is constant, volume and pressure of a gas are inversely related. Charles' law states that if pressure is constant, volume and temperature of a gas are directly related. 3. The combined gas law incorporates both, stating that if volume is constant, pressure and temperature are directly related. Air pressure and how it is measured is also discussed.
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![Ocean of Air ,[object Object],Pressure is in the ocean and in the sky. Air pressure is the force of air pushing down on you.](data:image/gif;base64,R0lGODlhAQABAIAAAAAAAP///yH5BAEAAAAALAAAAAABAAEAAAIBRAA7)
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Isobars that are close together indicate strong winds due to a large pressure difference over a small area, while isobars farther apart show gentler winds from a smaller pressure change. Isobars also show locations of high and low pressure areas. Air pressure decreases with increasing altitude as there are fewer air molecules, and high and low pressure systems affect incoming weather, with high pressure typically bringing cooler and clearer conditions and low pressure often accompanying warmer temperatures, storms and rain.
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The document discusses atmospheric pressure and different ways of measuring it. It describes how pressure decreases with increasing altitude and defines standard atmospheric pressure at sea level as 101,325 Pa. It also explains different pressure units like bars, pascals, atmospheres and torrs that are used to measure pressure. Common instruments for measuring pressure include mercury barometers, aneroid barometers, and digital barometers.
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Atmospheric pressure can be measured using a barometer. The first mercury barometer was developed in 1643 by Evangelista Torricelli. Later, an aneroid barometer was invented in 1843 that functions without liquids. In 2004, Cold Energy obtained a patent for a device that generates electricity by exploiting differences in atmospheric pressure between geographic locations using a pressurized air pipeline. This concept could generate enough renewable energy to power 250,000 homes.
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The document summarizes the thermal structure and composition of Earth's atmosphere. It describes that Earth's atmosphere is composed primarily of nitrogen (78%) and oxygen (21%), with smaller amounts of gases like carbon dioxide and water vapor. It also outlines the main layers of the atmosphere - the troposphere, stratosphere, mesosphere, and thermosphere - defining their varying temperature profiles and roles in weather, protection from UV radiation, and absorption of solar energy. Atmospheric pressure is also addressed, noting that standard atmospheric pressure at sea level is approximately 1013 hPa.
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earth is being cover with the blanket of gases called atmosphere which is further divided into 4 layers troposphere, stratosphere, mesosphere and thermospere
each layer is made up of some chemical constituents which could be water molecule traces of gases etc, Japan has done research and send a satellite in space to observe it as describe in this presentation
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The document discusses the four layers of the atmosphere:
1. The troposphere is the lowest layer that varies in height from 8 km at the poles to 16 km at the equator. Temperature decreases with height in the troposphere.
2. The stratosphere extends from the top of the troposphere to about 50 km above sea level. Temperature remains constant with increasing height in the lower stratosphere.
3. The mesosphere extends from 50-80 km above sea level. Temperature decreases from -83 to -100 degrees Celsius with increasing height in the mesosphere.
4. The thermosphere extends from 80-400 km above the earth. Temperature increases abruptly in the thermosphere.
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Isobars that are close together indicate strong winds due to a large pressure difference over a small area, while isobars farther apart show gentler winds from a smaller pressure change. Isobars also show locations of high and low pressure areas. Air pressure decreases with increasing altitude as there are fewer air molecules, and high and low pressure systems affect incoming weather, with high pressure typically bringing cooler and clearer conditions and low pressure often accompanying warmer temperatures, storms and rain.
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The document discusses atmospheric pressure and different ways of measuring it. It describes how pressure decreases with increasing altitude and defines standard atmospheric pressure at sea level as 101,325 Pa. It also explains different pressure units like bars, pascals, atmospheres and torrs that are used to measure pressure. Common instruments for measuring pressure include mercury barometers, aneroid barometers, and digital barometers.
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Atmospheric pressure can be measured using a barometer. The first mercury barometer was developed in 1643 by Evangelista Torricelli. Later, an aneroid barometer was invented in 1843 that functions without liquids. In 2004, Cold Energy obtained a patent for a device that generates electricity by exploiting differences in atmospheric pressure between geographic locations using a pressurized air pipeline. This concept could generate enough renewable energy to power 250,000 homes.
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The document summarizes key concepts about the atmosphere. It is composed primarily of nitrogen and oxygen. It describes atmospheric layers from closest to farthest as the troposphere, stratosphere, mesosphere, and thermosphere. The greenhouse effect and global warming are discussed as well as atmospheric heating processes of radiation, conduction, and convection. Wind patterns like trade winds and westerlies are influenced by pressure belts and the Coriolis effect. Air pollution sources include vehicles, power plants, and industries. Secondary pollutants form from chemical reactions between primary pollutants and substances.
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The document summarizes the thermal structure and composition of Earth's atmosphere. It describes that Earth's atmosphere is composed primarily of nitrogen (78%) and oxygen (21%), with smaller amounts of gases like carbon dioxide and water vapor. It also outlines the main layers of the atmosphere - the troposphere, stratosphere, mesosphere, and thermosphere - defining their varying temperature profiles and roles in weather, protection from UV radiation, and absorption of solar energy. Atmospheric pressure is also addressed, noting that standard atmospheric pressure at sea level is approximately 1013 hPa.
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2) Air masses and fronts that form boundaries between different air masses including cold fronts and warm fronts.
3) Severe weather such as thunderstorms, hurricanes, and tornadoes.
4) Tools used in weather forecasting like thermometers, barometers, weather balloons, radar, and satellites that provide data to predict weather conditions.
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earth is being cover with the blanket of gases called atmosphere which is further divided into 4 layers troposphere, stratosphere, mesosphere and thermospere
each layer is made up of some chemical constituents which could be water molecule traces of gases etc, Japan has done research and send a satellite in space to observe it as describe in this presentation
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The document discusses the four layers of the atmosphere:
1. The troposphere is the lowest layer that varies in height from 8 km at the poles to 16 km at the equator. Temperature decreases with height in the troposphere.
2. The stratosphere extends from the top of the troposphere to about 50 km above sea level. Temperature remains constant with increasing height in the lower stratosphere.
3. The mesosphere extends from 50-80 km above sea level. Temperature decreases from -83 to -100 degrees Celsius with increasing height in the mesosphere.
4. The thermosphere extends from 80-400 km above the earth. Temperature increases abruptly in the thermosphere.
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The document describes the structure and composition of Earth's atmosphere. It is divided into four main layers based on temperature - the troposphere, stratosphere, mesosphere, and thermosphere. The troposphere contains around 90% of the atmosphere's mass and is where weather occurs. Above this is the stratosphere, where temperature increases with altitude due to ozone absorbing UV light. The mesosphere is the coldest region and the thermosphere contains extremely high temperatures but little heat due to solar radiation. The atmosphere also protects the surface from radiation through the ozone and ionosphere layers.
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The document summarizes key aspects of Earth's atmosphere in three layers:
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The document discusses the layers of Earth's atmosphere. It is composed primarily of nitrogen and oxygen. The main layers are:
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The document describes the layers of Earth's atmosphere:
- The troposphere is the lowest layer where weather occurs and contains 75% of the atmosphere's mass. It extends from Earth's surface to around 12 km.
- The stratosphere is above the troposphere, extending from around 12 km to 40-48 km. Temperature remains constant or increases with height due to ozone absorption.
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3) When the Atlantic is warmer, it favors milder springs, summers, and autumns for England and Europe, along with more rainfall than usual for Northern and Central Europe.
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2) It explains atmospheric phenomena like air masses, fronts, humidity, wind patterns, and how solar radiation and the greenhouse effect impact weather and climate.
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Lecture4 sep16-bb
No, the brick resting on flat ground is in a stable state. A slight push would not cause it to move away from its original position. It would return to where it was pushed from.
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The airplane's ground speed is:
500 + 150 = 650 km/h
The airplane's air speed is still 500 km/h. The jet stream adds 150 km/h to the airplane's ground speed but does not affect its air speed.
Therefore, the best answer is 650 km/h.
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Standardized Test Preparation
Chapter I1
2. A weather balloon is rising at a rate of 5 m/s. It is currently at an altitude of 2,000 m. How long will it take the balloon to reach an altitude of 3,000 m?
Weather
Weather is affected by temperature, humidity, air pressure, and wind. These factors are interrelated. A change in one can impact the others. Temperature and air pressure have an inverse relationship - higher temperatures mean lower air pressures as the air expands. Higher temperatures also mean higher humidity as warm air holds more water vapor. Relative humidity decreases with increasing temperature. Wind blows from high to low pressure as air moves to equalize differences. Global wind patterns are caused by uneven heating and pressure differences.
Layers of the atmosphere
The document discusses the relationship between altitude and temperature in Earth's atmosphere. It describes how the atmosphere is made up of different layers - the troposphere, stratosphere, mesosphere, and thermosphere. The main points are:
1) Temperature decreases with increasing altitude in the troposphere and mesosphere, but increases with altitude in the stratosphere and thermosphere.
2) Air pressure decreases with increasing altitude, as there is less air above to exert pressure. The troposphere experiences all weather phenomena and contains almost all air.
3) The atmosphere regulates temperature and protects the Earth, providing gases for life and shielding from radiation and meteors.
No Title
This document provides an introduction to a self-directed learning module on diving medicine and decompression sickness for medical students. It begins by explaining how to navigate the slideshow presentation and lists the learning objectives. These include understanding the basic physics of diving, different types of diving and how physical laws apply, the pathophysiology of decompression sickness, and principles of managing decompression sickness. The document then outlines the contents of the slideshow, which will cover the physics of diving, types of diving, decompression sickness, and management of decompression sickness.
No Title
This document provides an introduction to a self-directed learning module on diving medicine and decompression sickness for medical students. It begins by explaining how to navigate the slideshow presentation and lists the learning objectives. These include understanding the basic physics of diving, different types of diving and how physical laws apply, the pathophysiology of decompression sickness, and principles of managing decompression sickness. The document then outlines the contents of the slideshow, which will cover the physics of diving, types of diving, decompression sickness, and management of decompression sickness.
Environmental .chemistry 2041 by Muhammad Moon Rao
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Editor's Notes
- [ Note to trainer : For detailed help in customizing this template, see the very last slide. Also, look for additional lesson text in the notes pane of some slides.]