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Remote sensing analysis of forest vegetation changes due to climate and anthropogenic impacts

机译:森林植被因气候和人为影响因森林植被变化的遥感分析

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Forest vegetation interaction with climate and anthropogenic stressors is done through a series of complex feedbacks, which are not very well understood. The patterns of forest vegetation are highly determined by temperature, precipitation, solar irradiance, soil conditions and CO_2 concentration. Vegetation impacts climate directly through moisture, energy, and momentum exchanges with the atmosphere and indirectly through biogeochemical processes that alter atmospheric CO_2 concentration. Changes inforest vegetation land use/cover alter the surface albedo and radiation fluxes, leading to a local temperature change and eventually a vegetation response. This albedo (energy) feedback is particularly important when forests mask snow cover. Forest vegetation-climate feedback regimes are designated based on the temporal correlations between the vegetation and and the surface temperature and precipitation. The different feedback regimes are linked to the relative importance of vegetation and soil moisture in determining land-atmosphere interactions. The spatio-temporal dynamics are assessed in terms of the NDVI-surface temperature correlations. Observed vegetation feedbacks on temperature and precipitation are assessed based on Landsat TM, ETM, MODIS and IKONOS satellite data across some forested areas placed in North/Eastern part of Bucharest town as well as in Prahova Valley, Romania for 1989 -2007 period.
机译:森林植被与气候和人为压力源的相互作用是通过一系列复杂的反馈进行的,这不是很好地理解。森林植被的图案是通过温度,降水,太阳辐照度,土壤条件和CO_2浓度的高度决定的。植被直接通过与大气的水分,能量和势头交换的气候产生影响,并通过改变大气CO_2浓度的生物地球化学过程间接化学过程。改变史型植被土地使用/覆盖改变表面反照和辐射助焊剂,导致局部温度变化,最终是植被反应。当森林面罩雪覆盖时,这款反馈(能源)反馈尤为重要。森林植被 - 气候反馈制度基于植被和表面温度和降水之间的时间相关性指定。不同的反馈制度与植被和土壤水分在确定土地气氛中相互作用的相对重要性有关。在NDVI表面温度相关性方面评估时空动态。根据Landsat TM,ETM,MODIS和IKONOS卫星在布加勒斯特镇(Buchova Valley)的一些森林区域以及罗马尼亚的普拉莫瓦谷的一些森林地区,评估了对温度和降水的温度和降水的植被反馈,并于1989 -2007期间。

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