There are three ways the sun's heat and energy are transferred throughout the atmosphere: radiation, conduction and convection. The sun's radiation heats the surface of the earth and the resulting heat is transferred to the atmosphere primarily by convection. Conduction is a minor contributor to the overall process since the transfer of heat via the air is a slow, inefficient process. Convection is the vertical process that carries warm air up from the ground to be replaced by cooler air, which in turn is warmed, and cycles upward again. On a global scale, convection is responsible for the atmospheric circulation which redistributes heat from the warm equatorial regions to the poles. The Coriolis effect, the apparent curvature of winds and ocean currents due to the earth's rotation, causes the atmospheric circulation to be divided into three convective zones per hemisphere: Hadley cells (tropical), Ferrell cell (temperate) and the Polar cell (UXL Encyclopedia of Weather and Natural Disasters). These convection cells along with horizontal advection are responsible for global wind patterns. On a smaller, local scale, convection currents are linked to the development of deep convective clouds and local storm systems. Because precipitation is central to the earth's energy balance, circulation, and water cycle, atmospheric scientists have focused their efforts on understanding how pollution effects the development and intensity of convection currents, cloud cover, precipitation, and thunderstorms.
The development of cumulonimbus or thunderhead clouds is an example of a convective cell. In order for a thunderstorm to develop, the sun warms the earth's surface which likewise warms the air above it. As the air rises it is transf...
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...fication of rain from the tropics to the mid-latitudes." Nature Geoscience, (2012): Print.
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Tornadoes form from wind shears. Wind shears form from warm air that is found at ground level; when it’s raised, the updraft meets a down draft of cooler air that is moved in the opposite direction of the warm air. When both are pushed towards the Earth, this creates wind shear. A spinning tube of air, created from wind shear; tilts upward into a vertical position, as the updraft sucks up moisture from the ground and into the sky. As the warm air cools high in the sky; this produces condensation. The condensation then produces thunderclouds, which rise to 30,000+ feet. The spinning formations of air are then trapped and lifted into the thundercloud. This begins as swirling motion and as continued (if the winds remained viable), a supercell will form. Mesocyclones as they are known are a rotating cloud. If these rotating clouds run into humid air it will spi...
As evening approached, several thunderstorms began to take on the characteristics of a supercell thunderstorm. Supercells, which are intense, broadly rotating thunderstorms, are the most v...
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...verage Weather History, Rainfall/ Precipitation, Sunshine." World Weather and Climate Graphs, Average Climate Charts, Guide to Precipitation, Temperatures, Best, Friendly, Holiday Climate. Web. 25 May 2010. .
First is a description of the greenhouse effect. The earth’s atmosphere has four layers, or zones, with each having distinct differences in temperature. The troposphere is the first layer surrounding the earth. Within this layer air is continually circulating and moving heat and moisture around the earth. The troposphere is denser than the other layers due to the fact that gravity keeps the majority of air molecules near the earth. This is about 75 percent of all the atmospheric mass. It is also the warmest layer (Cunningham & Cunningham, ...
Once upon a time high above the earth, fluffy white clouds drifted through the atmosphere. In the clouds lived a family Droplet of water, round and content with life. For as long as I could remember, I spent my days lying on my back, relaxing and soaking up the sun's warm rays. One day, I took my usual place in the sun but the light didn't seem to be as bright. In fact, as the day went on, it grew darker and darker, loud claps of thunder shook the cloud, and the Droplet felt as if he were getting so heavy he could hardly move. This is called precipitation.
A thunderstorm can produce some soothing sounds as it passes overhead. The light rain tapping at one’s window provides a comforting pattern for resting. The sound of thunder sounds like volleys of cannons being fired repeatedly in the distance. One knows the fire is hard at work by the crackling of the flames. One can hear the whistling wind sweeping the corners of your house repeatedly.
Climate change is evidenced through shifts in the weather patterns such as winds, humidity and temperatures over certain durations. Natural climate changes occur less frequently and they are triggered by factors related to geographical aspects as well as solar radiation. The earth’s movement on the orbit triggers changes in climate, causing some areas to have higher temperatures than usual, while others are significantly cold depending on the position of the earth on the orbit. The heat from the sun causes changes in the stratospheric ozone and it increases the amount of greenhouse gases. Heat from the oceanic crust also contributes to warming as a result of episodic hydrothermal venting (Liao & Sandeberg, 2012).
Global warming is an increase in the earth's temperature due to fossil fuels, industry, and agricultural processes caused by human, natural, and other gas emissions. This results in an increased evacuation of greenhouse gases. “Short-wave solar radiation sinks into the Earth's atmosphere and warms its surface while long-wave infrared radiation emitted by earth's surface is absorbed, and then re-emitted by trace gases.” (2)
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