РефератыИностранный языкClClouded Atmosphere Essay Research Paper Clouded AtmosphereThe

Clouded Atmosphere Essay Research Paper Clouded AtmosphereThe

Clouded Atmosphere Essay, Research Paper


Clouded Atmosphere


The concentration of the atmosphere’s main greenhouse gases specifically, carbon


dioxide, methane, nitrous oxide, and water vapor, have increased significantly during the


industrial age. These high concentrations are predicted to continue in the atmosphere for


thousands of years to come. This increase in specially carbon dioxide, increases the


infrared energy taken in by the atmosphere, and warming the earth’s surface. The Global


mean temperature over the past 150 years has risen between 0.3 degrees C and 0.6


degrees C. Climate changes that have been predicted are based on the continual rise in


Green House Gases. These changes include changes in: increase in mean surface air


temperature, increase in global mean rates of precipitation and evaporation, rising sea


level, and changes in the biosphere.


There are many causes to the rise in Green House Gases in the atmosphere. The


rise in carbon dioxide in the atmosphere is largely related to the combustion of fossil fuels


and cement production (Hansen). The increase in methane is do to rice cultivation, animal


husbandry, biomass burning, and landfills (Kattenberg). Nitrous oxide is on the rise


because of industrial sources like adipic acid and nitric acid production (Kattenberg).


Other gases not mentioned above that have a small impact on the Green House Gas


proposed problem, is CFC-11 and CFC-12, these Gases are know to the public as being a


big source of warming, although catalyzing decomposition of stratospheric ozone, they


do not pose a great threat. Since the public was notified of these compounds in


refrigerants, spray propellants, and foam blowing; the atmospheric concentrations have


decreased greatly (Prather).


The danger that all these Green House Gases put to the atmosphere is the increase


in the infrared energy absorbed by the atmosphere. This extra energy absorbed although


thought to only warm the earth also has a cooling tendency on the stratosphere (Peixoto


and Oort). The affect the radiation has by this increase of Green House Gases


concentration is also known as “Infrared Flux” at the tropopause (Wang). The models


used to predict this information can also closely mimic the other layers of the atmosphere


as well as the surface. Worldwide temperature measurements are carefully taken with


many variables in mind. Such variables would be urbanization of a region, aerosols,


precipitation, and changes in temperature and clouds (Hansen). Usually the temperature is


the first variable that is considered when assessments of the world climate change are


taken, it is also very important to consider other data that is part of the climate system


along the line of time and space. Some other sources of information are: tree rings, bore


hole temperature measurements in the soil, permafrost, and ice sheets, and measurements


of the mass of valley glaciers and ice caps. By looking at this material for the past 600


years it has been determined that the warming in the twentieth century is greater over this


time period (Briffa).


From paleoclimate studies it has been concluded that the Earth’s climate has been


altered by more than just Green House Gases, but Inorder to find the effects of the Green


House Gases specifically, a study of records from the periods when the changes in the


atmospheric carbon dioxide were much larger than those of our century. Large natural


variation in the atmosphere’s carbon dioxide were found in the observation and analysis of


gas bubbles trapped in glacier ice cores, are correlated with glacial (ice age) and


interglacial climate change of the latest Pleistocene and Holocene epochs. These glacial


periods are associated with low carbon dioxide concentrations, and the interglacial periods


with high concentrations. When looking at methane concentrations within these cores,


there was a similar correlation (Chappellaz).


Some of the predicted changes to the Earth’s climate due to this continual rise in


Green House Gases are: increase in mean surface air temperature, in

crease in global mean


rates of precipitation and evaporation, rising of sea levels. An increase in the surface air


temperature would cause rates of evaporation to increase, causing the water vapor in the


air to rise. The positive feedback to the surface temperature increase is that is will lead to


a more intense hydrological cycle, with more precipitation events (Kattenberg). Another


possible consequence of greenhouse gas induced climate change is elevated sea levels.


The main cause for sea level fluctuation is due to thermal expansion and the melting of


glaciers, both are responses to higher air temperatures. Measurements taken from 93′ to


98′ indicate a melt rate from Greenland’s ice sheet of 1 meter a year (Krabill). There have


been measurements of the sea levels also, they indicate a rise of about 10 – 25 cm a year


(Douglas).


All of these predictions were made by constructing models that help scientist


predict the climate change if the Green House Gases continue to rise at a steady rate.


Although scientist are fairly confident in these models there is room for error in these


models. Despite the gains there are a number of features of the climate system that are


still crudely represented in climate models. The models are restricted in their ability to


accurately represent terrain effects and to simulate processes that occur on a smaller scale.


Other shortcomings in the climate models is their inability to actually portray the effects of


aerosols, precipitation, and clouds and changes in solar irradiance. For these and other


reasons there remains scientific uncertainties in model predictions, including uncertainties


in the predictions of local effects of climate change, occurrence of extreme weather


events, effects of aerosols, changes in clouds, shifts in precipitation, and even changes in


ocean circulation (Hansen).


Aerosols are a big concern for model analysts, because aerosols are a principle


source of uncertainty in modeling climate changes during the industrial period. Aerosols


scatter and absorb short wave (solar) radiation and modify the reflectivity of clouds. Both


effects are thought to decrease the abortion of short wave radiation by the Earth, cooling


the climate, even though the troposphere aerosols only last a day in the atmosphere


(Charlson).


Green House Gases are related to the warming of the Earth, but the future of the


climate is not yet know, or predicted. So many variables make up the atmosphere and it’s


climate, no model can accurately predict the future. Natural Earth warmers like water


vapor and clouds also contribute to the warming trend. The Earth’s records of ice ages


and tree rings can only paint a very small piece of this huge picture. scientist are at a


disadvantage because they are not able to see the Earth’s full past, as an instructor of mine


once said- they cannot predict the future of climate patterns when they have only been


studding the atmosphere for the last 100 years.


Bibliography


References


Briffa, K. R. “Influence of volcanic eruptions on Northern Hemisphere summer


temperature over past 600 years.” Nature, 393, 1998.


Chappellaz, J. “Ice- core record of atmospheric methane over the past 160,000 years.”


Nature, 345, 1990.


Charlson, R. J. “Climate forcing by anthropogenic aerosols.” Science 255, 1992.


Douglas B. C. Global sea level rise, J. geophys. Res., 96 (C4), 6981-6992, 1991.


Hansen, J. E. (1998). Climate forcings in the industrial era. Livermore: Willams Press.


Kattenberg, A. (1996). Climate Change 1995: The Science of Climate Change.Cambridge:


Cambridge University Press.


Krabill. W. “Rapid thinning of parts of the southern Greenland ice sheet.” Science 283,


1999.


Peixoto, J. P., and A. H. Oort (1992). Physics of Climate. New York: American Institute


of Physics.


Prather, M. P. “The ozone layer: The road not taken.” Nature 381, 1996.


Wang, W. C. “Inadequacy of affective CO2 as a proxy in simulating the greenhouse effect


of other radiatively active gases.” Nature 350, 1991.

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