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Detailed Reference Information |
Goetz, S.J., Prince, S.D., Small, J. and Gleason, A.C.R. (2000). Interannual variability of global terrestrial primary production: Results of a model driven with satellite observations. Journal of Geophysical Research 105: doi: 10.1029/2000JD900274. issn: 0148-0227. |
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Interannual variation in terrestrial net primary production (NPP) was modeled using the global production efficiency model (GLO-PEM), a semimechanistic plant photosynthesis and respiration model driven entirely with satellite advanced very high resolution radiometer (AVHRR) observations. The model also estimated a wide range of biophysical variables at 10-day intervals for the period 1982--1989, including air temperature, vapor pressure deficit, soil moisture, biomass, autotrophic respiration, canopy-absorbed photosynthetically active radiation, gross primary production, and light use efficiency. The accuracy of the simulated variables has previously been shown to be within 10--30% of field measurements, depending on the specific variable. We analyze here interannual changes in NPP, which showed large spatial variability (0--1500 gC m-2 yr-1) and trends that differed regionally over the 8-year period. Annually integrated global NPP was found to vary as much as 12% between years and was very sensitive to air temperature. The coefficient of variation in NPP of sparsely vegetated areas (mostly semiarid) on an interannual basis was as much as 80%, whereas densely vegetated areas (broadleaf evergreen and seasonally deciduous forests) varied comparatively little (0--10%). Mean annual NPP of the latter decreased 36 gC m-2 yr-1 over the time series examined. There was extreme seasonal and moderate interannual variation (10--60%) in NPP of middle- to high-latitude regions (temperate and boreal forests) with evidence for a slight trend toward increased values through time (+3 to 12 gC m-2 yr-1). The results indicate significant interannual and regional differences in responses to climate variability, with boreal regions increasing 39 gC m-2 yr-1 compared to a decrease of 116 gC m-2 yr-1 in tropical regions for each 1 ¿C rise in air temperature. We explore a few of the possible reasons for these observations and discuss some of the issues and limitations to the use of the current global AVHRR observational record. ¿ 2000 American Geophysical Union |
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Abstract |
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Keywords
Atmospheric Composition and Structure, Biosphere/atmosphere interactions, Global Change, Biogeochemical processes, Global Change, Remote sensing, Meteorology and Atmospheric Dynamics, Land/atmosphere interactions |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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