Weather and Climate Extremes pp 327-339 | Cite as
Conceptual Framework for Changes of Extremes of the Hydrological Cycle With Climate Change
Abstract
A physically based conceptual framework is put forward that explains why an increase in heavy precipitation events should be a primary manifestation of the climate change that accompanies increases in greenhouse gases in the atmosphere. Increased concentrations of greenhouse gases in the atmosphere increase downwelling infrared radiation, and this global heating at the surface not only acts to increase temperatures but also increases evaporation which enhances the atmospheric moisture content. Consequently all weather systems, ranging from individual clouds and thunderstorms to extratropical cyclones, which feed on the available moisture through storm-scale moisture convergence, are likely to produce correspondingly enhanced precipitation rates. Increases in heavy rainfall at the expense of more moderate rainfall are the conseqUence along with increased runoff and risk of flooding. However, because of constraints in the surface energy budget, there are also implications for the frequency and/or efficiency of precipitation. It follows that increased attention should be given to trends in atmospheric moisture content, and datasets on hourly precipitation rates and frequency need to be developed and analyzed as well as total accumulation.
Keywords
Hydrological Cycle Precipitation Rate Storm Track Rain Rate Precipitable WaterPreview
Unable to display preview. Download preview PDF.
References
- Boer, G. J.: 1993, ‘Climate change and the regulation of the surface moisture and energy budgets.’ Clim. Dyn. 8, 225–239.CrossRefGoogle Scholar
- Brubaker, K. L., Entehabi, D., and Eagleson, P. S.: 1993, ‘Estimation of continental precipitation recycling.’ J. Clim. 6, 1077–1089.CrossRefGoogle Scholar
- Byers, H. R.: 1948, ‘The use of radar in determining the amount of rain over a small area.’ EOS Trans. A G U 29, 187–196.CrossRefGoogle Scholar
- Cubasch, U., Waszkewitz, J., Hegerl, G., and Periwitz, J.: 1995, ‘Regional climate changes as simulated in time-slice experiments.’ Clim. Change 31, 273–304.CrossRefGoogle Scholar
- Fankhauser, J. C.: 1988, ‘Estimates of thunderstorm precipitation efficiency from field measurements in CCOPE.’ Mon. Wea. Rev. 116, 663–684.CrossRefGoogle Scholar
- Ferrier, B. S., Simpson J., and Tao, W-K.: 1996, ‘Factors responsible for precipitation efficiencies in midlatitude and tropical squall simulations.’ Mon. Wea. Rev. 124, 2100–2125.CrossRefGoogle Scholar
- Gaffen, D. J., Barnett, T. P., and Elliott, W. P.: 1991, ‘Space and time scales of global tropospheric moisture.’ J. Clim. 4, 989–1008.CrossRefGoogle Scholar
- Held, I. M.: 1993, ‘Large-scale dynamics and global warming.’ Bull. Am. Meteorol. Soc. 74, 228–241.CrossRefGoogle Scholar
- Hennessy, K. J., Gregory, J. M., and Mitchell, J. F. B.: 1997, ‘Changes in daily precipitation under enhanced greenhouse conditions.’ Clim. Dyn. 13, 667–680.CrossRefGoogle Scholar
- Hense, A., Krahe P., and Flohn, H.: 1988, ‘Recent fluctuations of tropospheric temperature and water vapour content in the tropics.’ Meteorol. Atmos. Phys., 38, 215–227CrossRefGoogle Scholar
- IPCC (Intergovernmental Panel of Climate Change): 1996, Climate Change 1995: The Science of Climate Change. Eds. J. T. Houghton, F. G. Meira Filho, B. A. Callander, N. Harris, A. Kattenberg, and K. Maskell, Cambridge Univ. Press, Cambridge, U.K., 572pp.Google Scholar
- Iwashima, T., and Yamamoto, R.: 1993, ‘A statistical analysis of the extreme events: Longterm trend of heavy daily precipitation.’ J. Met. Soc. Japan 71, 637–640.Google Scholar
- Jones, R. G., Murphy, J. M., Noguer, M., and Keen, A. B.: 1997, ‘Simulation of climate change over Europe using a nested regional-climate model II: Comparison of driving and regional model responses to a doubling of carbon dioxide.’ Quart. J. Roy. Met. Soc. 123, 265–292.Google Scholar
- Kalnay E., Kanamitsu, M., Kistler, R., Collins, W., Deaven, D., Gandin, L., Iredell, M., Saha, S., White, G., Woollen, J., Zhu, Y., Cheffiah, M., Ebisuzaki, W., Higgins, W., Janowiak, J., Mo, K-C., Ropelewski, C., Leetmaa, A., Reynolds, R., and Jenne, R. 1996, ‘The NCEP/NCAR Reanalysis Project.’ Bull. Am. Meteorol. Soc. 77, 437–471CrossRefGoogle Scholar
- Karl, T. R., and Knight R. W.: 1998, ‘Secular trends of precipitation amount, frequency and intensity in the USA.’ Bull. Am. Meteorol. Soc. 79, 231–242.CrossRefGoogle Scholar
- Karl, T. R., Knight, R. W., Easterling, D. R. and Quayle, R.G.: 1996; ‘Indices of climate change for the United States. Bull. Am. Meteorol. Soc. 77, 279–292.CrossRefGoogle Scholar
- Karl, T. R., Knight, R. W. and Plummer, N.: 1995, Trends in high frequency climate variability in the twentieth century.’ Nature 377, 217–220.CrossRefGoogle Scholar
- Mearns, L. O., Giorgi, F., McDaniel, L., and Shields, C.: 1995, ‘Analysis of daily variability of precipitation in a nested regional climate model: comparison with observations and doubled CO2 results.’ Global Planetary Change 10, 55–78.CrossRefGoogle Scholar
- Mitchell, J. F. B., Wilson C. A., and Cunnington, W. M.: 1987, ‘On CO2 climate sensitivity and model dependence of results.’ Quart. J. Roy. Met. Soc. 113, 293–322.CrossRefGoogle Scholar
- Osborn, T. J., and Hulme, M.: 1997, ‘Development of a relationship between station and grid-box rainday frequencies for climate model evaluation.’ J. Clim. 10, 1885–1908.CrossRefGoogle Scholar
- Roads, J. O., Marshall, S., Oglesby R., and Chen, S-C.: 1996, ‘Sensitivity of the CCM1 hydrological cycle to CO2.’ J. Geophys. Res. 101, 7321–7339.CrossRefGoogle Scholar
- Ross, R. J., and Elliot, W. P. 1996, ‘Tropospheric water vapor climatology and trends over North America: 1973–93.’ J. Clim. 9, 3561–3574.CrossRefGoogle Scholar
- Schroeder, S. R., and McGuirk, J. P.: 1998, ‘Widespread tropical atmsopheric drying from 1979 to 1995.’ Geophys. Res. Lett. 25, 1301–1304.CrossRefGoogle Scholar
- Suppiah, R., and Hennessy, K. J.: 1998, ‘Trends in the intensity and frequency of heavy rainfall in troipcal Australia and links with the Southern Oscillation.’ Aust. Meteorol. Mag., 45, 1–17.Google Scholar
- Trenberth, K. E.: 1998, ‘Atmospheric moisture residence times and cycling: Implications for rainfall rates with climate change.’ Clim. Change, 36, (in press).Google Scholar
- Trenberth, K. E., and Guillemot, C. J.: 1996, ‘Physical processes involved in the 1988 drought and 1993 floods in North America.’ J. Clim. 9, 1288–1298.CrossRefGoogle Scholar
- Trenberth, K. E., and Hoar, T. J.: 1996, ‘The 1990–1995 El Niño-Southern Oscillation event: Longest on record.’ Geophys. Res. Lett. 23, 57–60.CrossRefGoogle Scholar
- Xie, P, and Arkin, P. A.: 1997, ‘Global precipitation: A 17-year monthly analysis based on gauge observations, satellite estimates and numerical model outputs.’ Bull. Am. Meteorol. Soc. 78, 2539–2558.CrossRefGoogle Scholar
- Zhai, P., and Eskridge, R. E.: 1997, ‘Atmospheric water vapor over China.’ J. Clim. 10, 2643–2652.CrossRefGoogle Scholar