Stochastic generation of meteorological variables and effects on global models of water and carbon cycles in vegetation and soils

Citation
B. Hubert et al., Stochastic generation of meteorological variables and effects on global models of water and carbon cycles in vegetation and soils, J HYDROL, 213(1-4), 1998, pp. 318-334
Citations number
31
Categorie Soggetti
Environment/Ecology,"Civil Engineering
Journal title
JOURNAL OF HYDROLOGY
ISSN journal
00221694 → ACNP
Volume
213
Issue
1-4
Year of publication
1998
Pages
318 - 334
Database
ISI
SICI code
0022-1694(199812)213:1-4<318:SGOMVA>2.0.ZU;2-C
Abstract
Global models of water and carbon cycles in continental vegetation and soil s are usually forced with monthly mean climatic data-sets and thus neglect day to day variations of the weather. This treatment may be justified for e mpirical models based on parametrizations validated at a monthly timescale. Mechanistic models handling hydrological and biological processes at much shorter timescales might, however, be largely affected by such an approxima tion, since the various processes described are highly nonlinear. A random generator of daily precipitations and temperatures applicable at the global scale has thus been developed from worldwide meteorological data covering 6 years of observations. The probability of a wet day is correlated to the weather encountered the previous day. The amount of precipitation, the dail y mean temperature and the diurnal. range of temperature are described from the statistical point of view by the cumulative distribution functions (CD F) of three random variables. The CDF's a relative to temperatures are diff erent for rainy and dry days. This stochastically generated weather field i s used as input to IBM (Improved Bucket Model) and CARAIB (CARbon Assimilat ion In the Biosphere), two global models of respectively soil hydrology and vegetation productivity. Large differences in both the geographical distri bution and the global value of soil water, vegetation productivity and carb on stocks are obtained between the model runs using monthly uniform weather on one side and randomly generated weather on the other. The main contribu tion to this difference at the global scale arises from the precipitation g eneration occurring as a result of high degree of nonlinearity of the inter ception scheme used in IBM. (C) 1998 Elsevier Science B.V. All rights reser ved.