Please forward this error screen to sharedip-1071802084. Nitrogen and introduction to modern climate change dessler pdf gases are transparent to both incoming solar radiation and outgoing longwave radiation from the earth’s surface.

Therefore, these gases do not play a role in establishing atmospheric temperature. The answer depends on the time frame being considered. 2: CO2 concentration of the atmosphere vs. 6a: Concentration of carbon dioxide vs. The influence of a factor that can cause climate change, such as a greenhouse gas, is often evaluated in terms of its radiative forcing. Radiative forcing is a measure of how the energy balance of the Earth-atmosphere system is influenced when factors that affect climate are altered.

Earth’s atmosphere do not absorb outgoing longwave radiation so these gases cannot keep the atmosphere warm. CO2 is preventing LW radiation from escaping the atmosphere and this decreasing LW radiation is accurately being predicted by models. Watch this video to learn about the role of water vapor in the atmosphere. 5oC with a best estimate of about 3oC, and is very unlikely to be less than 1. Humanity today, collectively, must face the uncomfortable fact that industrial civilization itself has become the principal driver of global climate.

If we stay our present course, using fossil fuels to feed a growing appetite for energy-intensive life styles, we will soon leave the climate of the Holocene, the world of prior human history. The eventual response to doubling preindustrial atmospheric CO2 likely would be a nearly ice-free planet. 2100 if greenhouse gas emissions are not reduced. 2100 if the current proposals were enacted. Our hellish future: Definitive NOAA-led report on U.

F warming over most of inland U. Without significant mitigation, the report says global mean warming could reach as high as 7 degrees Celsius by 2100. Increasing greenhouse gases should result in a warmer troposphere and a cooler stratosphere. The tropopause heights varies between 8 km and 18 km due to latitude and season.

Cooler latitudes and seasons result in a lower tropopause height. The greatest ozone density is around 20-25 km because the ozone destruction processes are slower there. Ozone also acts as a greenhouse gas. 15: Stratospheric cooling rates: The picture shows how water, carbon dioxide and ozone contribute to longwave cooling in the stratosphere. Colors from blue through red, yellow and to green show increasing cooling, grey areas show warming of the stratosphere. This suggests that the portion of stratospheric cooling caused by ozone depletion should have ended and warming would result in the absence of other forcing mechanisms because of the increased absorption of incoming SW radiation from the sun. The results indicate that natural forcing mechanisms cannot cause stratospheric cooling while increased CO2 would be responsible for most of the cooling in the upper stratosphere and a significant portion of the lower region of the statosphere.

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