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Global Distribution of Surface Water Vapour Density Using in Situ and Reanalysis Data

机译:使用原位和再分析数据的地表水蒸气密度的全局分布

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Global spatial and annual distribution of surface water vapour density were estimated using 2005 -2016 monthly air temperature and relative humidity at 1 1 resolution obtained from Era interim and NCEP/NCAR database products. Obtained results from reanalysis were statistically tested using in situ data from Tropospheric Data Acquisition Network (TRODAN) of The Center for Atmospheric Research (CAR). Four seasonal variations of surface water vapour density (winter (DJF), spring (MAM), summer (JJA) and autumn (SON)) was examined. Observed result from the two reanalysis follow similar trends with value from Era interim leading. High values ranges between 50 g/m~2 and 68 g/m~2 were observed in tropical regions and humid sub-tropical regions. Low values ranges between 8 g/m~2 and 38 g/m~2 were observed in Ice cap, Tundra and arid regions. High warming may be experienced in tropical and sub-tropical regions, similarly, climate change with alarming rate may be experienced in locations with low values. The annual cycle of surface water vapor density is clearly established from two reanalysis across world classified into twelve regions. The statistical test for the reanalysis present good result with a mean bias error, MBE, root mean square error, RMSE and R square of 20.56, 18.29, 0.87 and 5.87, 0.98, 0.93 for Era interim and NCEP/NCAR respectively.
机译:使用2005 -2016每月空气温度和相对湿度估计从ERA临时和NCEP / NCAR数据库产品获得的分辨率的全局空间和年度分布的表面水蒸气密度。通过来自大气研究中心的对流层数据采集网络(Trodan)的原位数据,在统计上测试Reanalysics的结果。检查了表面水蒸气密度的四个季节变化(冬季(DJF),春季(MAM),夏季(JJA)和秋季(儿子))。观察到两次再分析的结果遵循类似ERA临时领先的相似趋势。在热带地区和潮湿的亚热带地区观察到50g / m〜2和68g / m〜2之间的高值。在冰盖,苔原和干旱地区观察到8g / m〜2和38g / m〜2之间的低值范围。热带和亚热带地区可能在高温中经历高温,同样,在具有低值的位置可能在地点内经历动力变化的气候变化。表面水蒸气密度的年度周期明显从分类为十二个地区的世界两次再分析。再分析的统计测试存在良好的结果,其中平均误差,MBE,均方误差,RMSE和R平方分别为2.56,18.29,0.87和5.87,0.98,0.98,0.98,0.93,用于ERA临时和NCEP / NCAR。

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