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Climatic driving forces in inter-annual variation of global FPAR

机译:在全球FPA的年间变异中的气候驱动力

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Fraction of Absorbed Photosynthetically Active Radiation (FPAR) characterizes vegetation canopy functioning and its energy absorption capacity. In this paper, we focus on climatic driving forces in inter-annual variation of global FPAR from 1982 to 2006 by Global Historical Climatology Network (GHCN-Monthly) data. Using FPAR-Simple Ratio Vegetation Index (SR) relationship, Advanced Very High Resolution Radiometer (AVHRR) Global Inventory Modeling and Mapping Studies (GIMMS) Normalized Difference Vegetation Index (NDVI) was used to estimate FPAR at the global scale. The correlation between inter-annual variation of FPAR and temperature, precipitation derived from GHCN-Monthly was examined, during the periods of March-May (MAM), June-August (JJA), September-November (SON), and December-February (DJF) over from 1982 to 2006. The analysis of climatic influence on global FPAR revealed the significant correlation with temperature and precipitation in some meteorological stations area, and a more significant correlation with precipitation was found than which with temperature. Some stations in the regions between 30° N and 60° N and around 30° S in South America, where the annual FPAR variation showed a significant positive correlation with temperature (P < 0.01 or P < 0.05) during MAM, SON, and DJF, as well as in Europe during MAM and SON period. A negative correlation for more stations was observed during JJA. For precipitation, there were many stations showed a significant positive correlation with inter-annual variation of global FPAR (P < 0.01 or P < 0.05), especially for the tropical rainfall forest of Africa and Amazon during the dry season of JJA and SON.
机译:吸收的光合作用辐射(FPAR)的分数表征植被冠层功能及其能量吸收能力。在本文中,我们通过全球历史气候网络(GHCN-月刊)数据从1982年到2006年全球FPAR间全球FPAR间变异的气候驱动力。使用FPAS-简单的比率植被指数(SR)关系,使用先进的非常高分辨率辐射计(AVHRR)全球库存建模和映射研究(GIMMS)归一化差异植被指数(NDVI)以全球规模估算FPAR。在3月至5月(JJA),9月至11月(儿子)和12月 - 2月期间,研究了FPAR和温度的年度常数,从GHCN-HOREN的降水,从GHCN-HOREN的降水进行了相关性,审查了GHCN-月刊的降水(DJF)于1982年至2006年。对全球FPAR的气候影响分析揭示了一些气象站区域中与温度和沉淀的显着相关性,并且发现了与温度的沉淀更明显的相关性。在南美洲的30°N和60°N和大约30°S之间的区域中的一些站点,每年的FPAR变化与MAM,儿子和DJF的温度(P <0.01或P <0.05)显示出显着的正相关以及在妈妈和儿子时期的欧洲。在JJA期间观察到更多站的负相关性。对于沉淀,有许多站点表现出与全球FPA的年间变异的显着正相关(P <0.01或P <0.05),特别是在JJA和儿子的干燥季节期间非洲和亚马逊的热带降雨林。

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