How does the increasing abundance of co2




















Bureau of Plant Industry Bull. A Review of the Literature. Relative water requirements of plants. Chang, J. Climate and Agriculture, An Ecological Survey. Chicago: Aldine Publishing Co. Curry, R. Simulation as a tool for analyzing crop response to climate change. ASAE Response of crop yield to predicted changes in climate and atmospheric CO 2 using simulation. De Wit, C. Transpiration and Crop Yields.

Dickson, R. The climate of Tennessee. Doorenbos, J. Yield Responses to Water. Crop Water Requirements. Dudek, D. Climate change impacts upon agriculture and resources: a case study of California. Enoch, H. I and II. Geraghty, J. Miller, F. Troise, M. Pinther, and R. Water Atlas of the United States. Gleick, P. Vulnerability of water systems. Waggoner, ed. Water Resources. New York: John Wiley and Sons. Grotch, S. Guinn, G. Analysis of CO 2 exchange assumptions: feedback control. Hesketh and J.

Jones, eds. Hanks, R. Gardner, and R. Plant growth-evapotranspiration relationships for several crops in the Great Plains. Hansen, J. Lacis, D. Rind, G. Russell, P. Stone, I. Fund, R. Ruedy, and J. Climate sensitivity: analysis of feedback mechanisms. Hansen and T. Takahashi, eds. Fung, A. Lacis, S. Lebedeff, D. Rind, R. Ruedy, G. Russell, and P. Idso, S. Kimball, M. Anderson, and J.

Effects of atmospheric CO 2 enrichment on plant growth: the interactive role of air temperature. Ecosystems Environ. Jensen, M. Empirical methods of estimating or predicting evapotranspiration using radiation. Estimating evapotranspiration from solar radiation.

Jones, C. Kiniry, eds. Jones, J. Boote, S. Jagtap, and J. Soybean development. Chapter 5 in R. Hanks and J. Ritchie, eds. Madison, Wisconsin: American Society of Agronomy. Boote, and W. Soybean canopy growth, photosynthesis, and transpiration responses to whole-season carbon dioxide enrichment. Responses of soybean canopy photosynthesis and transpiration to whole-day temperature changes in different CO 2 environments.

Jones, and R. Photosynthesis and transpiration responses of soybean canopies to short-and long-term CO 2 treatments. Jones, and L. Seasonal canopy CO 2 exchange, water use, and yield components in soybean grown under differing CO 2 and water stress conditions. Jouzel, J. Lorius, J.

Petit, C. Genthon, N. Barkov, V. Kotlyakov, and V. Vostok ice core: a continuous isotope temperature record over the last climatic cycle , years.

Keeling, C. Bacastow, A. Carter, S. Piper, T. Whorf, M. Heinmann, W. Mook, and H. A three dimensional model of atmospheric CO 2 transport based on observed winds: Analysis of data. Peterson, ed. Geophysical Monograph Kimball, B. Carbon dioxide and agricultural yield: an assemblage and analysis of prior observations. Increasing atmospheric CO 2 : effects on crop yield, water use, and climate. Water Management Mauney, G. Guinn, F. Nakayama, P. Pinter, Jr.

Clawson, R. Reginato, and S. Response of Vegetation to Carbon Dioxide, Ser. Joint program of the U. Department of Energy and the U. Department of Agriculture, U. Water Conservation Lab, and U. Western Cotton Research Lab. Phoenix, Arizona: U. King, G. DeVelice, R. Neilson, and R. Knisel, W. Yates, J. Sheridan, T. Woody, L. Report ARS Landers, H. The climate of South Carolina. Lorius, C. Jouzel, D. Raynaud, J. Hansen, and H.

Le Treut. The ice core record: climate sensitivity and future greenhouse warming. Manabe, S. Reduction in summer soil wetness induced by an increase in atmospheric carbon dioxide.

Science Large-scale changes of soil wetness induced by an increase in atmospheric carbon dioxide. Mearns, L. Climate variability. Miller, Barbara A. Report No. Norris, Tennessee: Tennessee Valley Authority. Miller, Barbara. Global climate change: implications for the Tennessee Valley Authority reservoir system. Topping, Jr. Mitchell, J. The "greenhouse" effect and climate change. Reviews of Geophysics Morison, J. Intercellular CO 2 concentration and stomatal response to CO 2.

Zeiger, G. Farquhar, and I. Cowan, eds. Stanford, California: Stanford University. Plant growth and water use with limited water supply in high CO 2 concentrations: I. Australian J. Pearcy, R. Physiological effects. Lemon, ed. Boulder, Colorado: Westview Press. Peart, R. Curry, K.

Impact of climate change on crop yield in the Southeastern USA: a simulation study. Penning de Vries, F. Jansen, H. Revelle, R. Effects of a carbon dioxide induced climatic change on water supplies in the Western United States. Ritchie, J. Baer, and T. Effect of global climate change on agriculture: Great Lakes region. Rosenberg, N. Kimball, P. Martin, and C. From climate and CO 2 enrichment to evapotranspiration. Rosenzweig, C. Potential effects of climate change on agricultural production in the Great Plains: a simulation study.

Smith and. Schlesinger, M. Climate model simulation of CO 2 -induced climate change. Saltzman, ed. New York: Academic Press. Shawcraft, R. Lemon, L. Stewart, and S. The soil-plant-atmosphere model and some of its predictions.

Smith, J. Because the seasons in the northern and southern hemispheres are opposite, carbon dioxide in the atmosphere is increasing in the north while decreasing in the south, and vice versa.

The cycle is more clearly present in the northern hemisphere; because it has relatively more land mass and terrestrial vegetation. Oceans dominate the southern hemisphere.

Carbon dioxide can change the pH of water. The troposphere is the lower part of the atmosphere, of about kilometres thick. Within the troposphere there are gasses called greenhouse gasses. When sunlight reaches the earth, some of it is converted to heat. Greenhouse gasses absorb some of the heat and trap it near the earth's surface, so that the earth is warmed up.

This process, commonly known as the greenhouse effect , has been discovered many years ago and was later confirmed by means of laboratory experiments and atmospheric measurements. Life as we know it exists only because of this natural greenhouse effect, because this process regulates the earth's temperature. When the greenhouse effect would not exist, the whole earth would be covered in ice.

The amount of heat trapped in the troposphere determines the temperature on earth. The amount of heat in the troposphere depends on concentrations of atmospheric greenhouse gasses and the amount of time these gasses remain in the atmosphere. Since the industrial revolution in began, human processes have been causing emissions of greenhouse gasses, such as CFC's and carbon dioxide. This has caused an environmental problem: the amounts of greenhouse gasses grew so extensively, that the earth's climate is changing because the temperatures are rising.

This unnatural addition to the greenhouse effect is known as global warming. It is suspected that global warming may cause increases in storm activity, Melting of ice caps on the poles, which will cause flooding of the inhabited continents, and other environmental problems.

Together with hydrogen , carbon dioxide is the main greenhouse gas. The modern record of atmospheric carbon dioxide levels began with observations recorded at Mauna Loa Observatory in Hawaii. This graph shows the station's monthly average carbon dioxide measurements since in parts per million ppm.

The seasonal cycle of highs and lows small peaks and valleys is driven by summertime growth and winter decay of Northern Hemisphere vegetation. The long-term trend of rising carbon dioxide levels is driven by human activities. NOAA Climate. Carbon dioxide levels today are higher than at any point in at least the past , years. Global atmospheric carbon dioxide concentrations CO 2 in parts per million ppm for the past , years.

The peaks and valleys track ice ages low CO 2 and warmer interglacials higher CO 2. During these cycles, CO 2 was never higher than ppm. On the geologic time scale, the increase orange dashed line looks virtually instantaneous.

An earlier version of this image had an error in the time scaling on the X axis. This affected the apparent duration and timing of the most recent ice ages, but did not affect the modern or paleoclimate carbon dioxide values. Carbon dioxide concentrations are rising mostly because of the fossil fuels that people are burning for energy.

Fossil fuels like coal and oil contain carbon that plants pulled out of the atmosphere through photosynthesis over many millions of years; we are returning that carbon to the atmosphere in just a few hundred years.

Each year we put more carbon dioxide into the atmosphere than natural processes can remove, which means the net global amount of carbon dioxide rises. The more we overshoot what natural processes remove, the faster the annual growth rate. In the s, the global growth rate of atmospheric carbon dioxide was roughly 0. Between , however, the growth rate has been 2. The annual rate of increase in atmospheric carbon dioxide over the past 60 years is about times faster than previous natural increases, such as those that occurred at the end of the last ice age 11,, years ago.

Carbon dioxide is a greenhouse gas : a gas that absorbs and radiates heat. Unlike oxygen or nitrogen which make up most of our atmosphere , greenhouse gases absorb that heat and release it gradually over time, like bricks in a fireplace after the fire goes out. But increases in greenhouse gases have tipped the Earth's energy budget out of balance, trapping additional heat and raising Earth's average temperature. Increases in atmospheric carbon dioxide are responsible for about two-thirds of the total energy imbalance that is causing Earth's temperature to rise.

Another reason carbon dioxide is important in the Earth system is that it dissolves into the ocean like the fizz in a can of soda. In fact, the only time we see significant absorption of carbon dioxide in the tropics is in Africa during June, July and August. One possible explanation for this is that the growing season is getting longer. Our space-based measurements are beginning to change our understanding of how the carbon cycle works and are providing new tools to allow us to monitor changes in the future in response to climate change.

Impacts from agricultural activities also seem to be changing, he says. During summer in the U. The same thing is being observed in Eastern and Southern Asia. The strong absorption of carbon dioxide across China is erasing all but a thin strip of fossil fuel emissions along the coast, with Central China now functioning as a net absorber of carbon dioxide during the growing season.

The system would include a series of spacecraft making coordinated measurements to monitor these changes. The system would be complemented by ground-based and aerial research.



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