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Assessment of tundra-taiga boundary changes using MODIS LAI data

机译:使用MODIS LAI数据评估TUNDRA-TAIGA边界变化

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Surface of the earth temperature of the earth caused phenomenon that rise and is global warming as greenhouse gas concentration into waiting by continuous discharge of greenhouse gas increases since passing industrial revolution. While gravity about climate fluctuation is risen worldwide, place that can diminish successively biggest surface of the earth change by global warming is high latitude area of polar regions. This study observed distribution of vegetation to confirm change of tundra-taiga boundary. Tundra-taiga boundary is used to observe the transfer of vegetation pattern because it is very sensitive to human activity, natural disturbances and climate change. The circumpolar tundra-taiga boundary could observe reaction about some change. Reaction and confirmation about climate change were definite than other place. This study used Leaf Area Index(LAI) 8-Day data in August from 2000 to 2009 that acquire from Terra satellite MODerate resolution Imaging Spectroradiometer(MODIS) sensor and used Koppen Climate Map, Global Land Cover 2000 for reference data. This study conducted analysis of spatial distribution in low density vegetated areas and inter-annual / zonal analysis for using the long period data of LAI. Change of LAI was confirmed by analysis based on boundary value of LAI in study area. Development of vegetation could be confirmed by area of grown vegetation(730,325km~(2)) than area of reduced vegetation(22,372km~(2)) in tundra climate. Also, area was increased with the latitude 64 deg N approx 66 deg N as the center and around the latitude 62 deg N through area analysis by latitude. Vegetation of tundra-taiga boundary was general increase from 2000 to 2009. While area of reduced vegetation was a little, area of vegetation growth and development was increased significantly.
机译:地球温度的表面引起了现象,由于经过工业革命以来,通过连续排放温室气体的温室气体浓度等待着的全球变暖。虽然关于气候波动的严重性在全球范围内上升,但通过全球变暖可以递减地球变化的最大表面的地方是极地地区的高纬度区域。本研究观察了植被的分布,以确认苔原 - Taiga边界的变化。苔原 - Taiga边界用于观察植被模式的转移,因为它对人类活动,自然扰动和气候变化非常敏感。 Circumpolar Tundra-Taiga边界可以观察到一些变化的反应。关于气候变化的反应和确认是明确的。本研究使用叶面积指数(Lai)8月8日数据从2000年到2009年,从Terra卫星中间分辨率成像分光镜(MODIS)传感器和使用的Koppen气候图,全球陆地覆盖2000用于参考数据。该研究对使用Lai长期数据的低密度植被区域和年间/区间分析进行了分析。基于研究区赖边值的分析证实了LAI的变化。植被的发展可以通过生长的植被面积(730,325km〜(2))确认,苔原气候减少植被(22,372km〜(2))。此外,通过纬度地通过纬度地通过面积分析随着纬度66°D,纬度64°Deg n和纬度地分析。苔原 - Taiga边界的植被从2000年到2009年普遍增加。虽然植被降低的面积有点,植被增长和发展面积显着增加。

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