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Modeling the interannual variability and trends in gross and net primary productivity of tropical forests from 1982 to 1999

机译:对1982年至1999年热带森林的总初级生产力和净初级生产力的年际变化和趋势进行建模

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The role of tropical ecosystems in global carbon cycling is uncertain, at least partially due to an incomplete understanding of climatic forcings of carbon fluxes. To reduce this uncertainty, we simulated and analyzed 1982-1999 Amazonian, African, and Asian carbon fluxes using the Biome-BGC prognostic carbon cycle model driven by National Centers for Environmental Prediction reanalysis daily climate data. We first characterized the individual contribution of temperature, precipitation, radiation, and vapor pressure deficit to interannual variations in carbon fluxes and then calculated trends in gross primary productivity (GPP) and net primary productivity (NPP). In tropical ecosystems, variations in solar radiation and, to a lesser extent, temperature and precipitation, explained most interannual variation in GPP. On the other hand, temperature followed by solar radiation primarily determined variation in NPP. Tropical GPP gradually increased in response to increasing atmospheric CO_2. Confirming earlier studies, changes in solar radiation played a dominant role in CO_2 uptake over the Amazon relative to other tropical regions. Model results showed negligible impacts from variations and trends in precipitation or vapor pressure deficits on CO_2 uptake.
机译:热带生态系统在全球碳循环中的作用尚不确定,至少部分原因是对碳通量的气候强迫没有完全理解。为了减少这种不确定性,我们使用由国家环境预测中心重新分析每日气候数据驱动的Biome-BGC预后性碳循环模型对1982-1999年亚马逊,非洲和亚洲的碳通量进行了模拟和分析。我们首先描述了温度,降水,辐射和蒸气压赤字对碳通量年际变化的个体贡献,然后计算了总初级生产力(GPP)和净初级生产力(NPP)的趋势。在热带生态系统中,太阳辐射的变化以及较小程度的温度和降水是GPP中大多数年际变化的原因。另一方面,温度随后是太阳辐射主要决定了NPP的变化。热带GPP随着大气CO_2的增加而逐渐增加。证实了较早的研究,相对于其他热带地区,太阳辐射的变化在亚马逊地区吸收CO_2中起主要作用。模型结果表明,降水变化或趋势或蒸气压不足对CO_2吸收的影响可忽略不计。

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