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Radiation budget changes with dry forest clearing in temperate Argentina.

机译:辐射预算随着温带阿根廷的干燥森林砍伐而变化。

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Land cover changes may affect climate and the energy balance of the Earth through their influence on the greenhouse gas composition of the atmosphere (biogeochemical effects) but also through shifts in the physical properties of the land surface (biophysical effects). We explored how the radiation budget changes following the replacement of temperate dry forests by crops in central semiarid Argentina and quantified the biophysical radiative forcing of this transformation. For this purpose, we computed the albedo and surface temperature for a 7-year period (2003-2009) from MODIS imagery at 70 paired sites occupied by native forests and crops and calculated the radiation budget at the tropopause and surface levels using a columnar radiation model parameterized with satellite data. Mean annual black-sky albedo and diurnal surface temperature were 50% and 2.5 degrees C higher in croplands than in dry forests. These contrasts increased the outgoing shortwave energy flux at the top of the atmosphere in croplands by a quarter (58.4 vs. 45.9 W m-2) which, together with a slight increase in the outgoing longwave flux, yielded a net cooling of -14 W m-2. This biophysical cooling effect would be equivalent to a reduction in atmospheric CO2 of 22 Mg C ha-1, which involves approximately a quarter to a half of the typical carbon emissions that accompany deforestation in these ecosystems. We showed that the replacement of dry forests by crops in central Argentina has strong biophysical effects on the energy budget which could counterbalance the biogeochemical effects of deforestation. Underestimating or ignoring these biophysical consequences of land-use changes on climate will certainly curtail the effectiveness of many warming mitigation actions, particularly in semiarid regions where high radiation load and smaller active carbon pools would increase the relative importance of biophysical forcing.Digital Object Identifier http://dx.doi.org/10.1111/gcb.12121
机译:土地覆盖变化可能通过影响大气中的温室气体组成(生物地球化学效应),也可能通过改变土地表面的物理特性(生物物理效应)来影响气候和地球的能量平衡。我们探索了阿根廷中部半干旱地区的农作物取代温带干燥森林后的辐射预算变化,并量化了这种转变的生物物理辐射强迫。为此,我们根据MODIS影像计算了原始森林和农作物所占的70个配对地点在7年期间(2003-2009年)的反照率和地表温度,并使用柱状辐射计算了对流层顶和地表水平的辐射预算用卫星数据参数化的模型。耕地的年平均黑天空反射率和日表面温度分别比干旱森林高50%和2.5摄氏度。这些对比使农田中大气层顶部的短波能量通量增加了四分之一(58.4 vs. 45.9 W m -2 ),同时长波通量略有增加,产生了净冷却为-14 W m -2 。这种生物物理降温效果相当于将大气中CO 2 减少22 Mg C ha -1 ,这大约占典型碳排放量的四分之一到一半。伴随着这些生态系统中的森林砍伐。我们表明,阿根廷中部地区的农作物替代干旱的森林对能源预算具有很强的生物物理影响,可以抵消森林砍伐的生物地球化学影响。低估或忽略土地利用变化对气候的这些生物物理后果肯定会限制许多减缓气候变化行动的有效性,特别是在半干旱地区,那里的高辐射负荷和较小的活性炭池会增加生物物理强迫的相对重要性。 ://dx.doi.org/10.1111/gcb.12121

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