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A SIMULATION STUDY OF RESPONSES OF THE NORTHEAST CHINA TRANSECT TO ELEVATED CO 2 AND CLIMATE CHANGE
Author(s) -
Gao Qiong,
Zhang Xinshi
Publication year - 1997
Publication title -
ecological applications
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.864
H-Index - 213
eISSN - 1939-5582
pISSN - 1051-0761
DOI - 10.1890/1051-0761(1997)007[0470:assoro]2.0.co;2
Subject(s) - environmental science , biomass (ecology) , evapotranspiration , normalized difference vegetation index , precipitation , transect , atmospheric sciences , vegetation (pathology) , primary production , relative humidity , climate change , ecosystem , hydrology (agriculture) , ecology , meteorology , geography , geology , medicine , geotechnical engineering , pathology , biology
The spatiotemporal variations of vegetation biomass of the ecological transect in northeast China were simulated. State variables of the model included green biomass and nongreen biomass of 12 vegetation categories and water contents of three soil layers. The simulated monthly green biomass was converted into NDVI, or Normalized Differential Vegetation Index of AVHRR (Advanced Very High Resolution Radiometry). A comparison between the modeled and the observed NDVI was made at 10′ spatial resolution. Atmospheric CO 2 concentration and monthly precipitation were used as two driving variables for global change simulation. Effects of precipitation increments on percentage sunshine, relative humidity, radiation, evapotranspiration, and eventually soil water and plant growth, were considered. Two levels of CO 2 concentration (present, doubled) and seven levels of precipitation increments (0, 0.05, 0.1, 0.15, 0.2, 0.25, and 0.30) were prescribed for a total of 14 simulation runs. A steady‐state solution was obtained for each simulation run. The results of simulation showed that with the present climate conditions, doubling atmospheric CO 2 concentration led approximately to a 20.3% increase in green biomass, 11.0% increase in nongreen biomass, 19.0% increase in green NPP, 12.8% increase in nongreen NPP, and 14.9% increase in overall average NPP at steady state. These increases go, respectively, to 32.9, 13.9, 30.0, 20.1, and 23.4% when a 30% precipitation increase was superimposed on the doubled CO 2 concentration.