全球日雨量计测量值的偏差校正

M. Ungersböck , F. Rubel , T. Fuchs , B. Rudolf
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引用次数: 34

摘要

到目前为止,基于雨量计的全球降水气候学仅使用月校正因子对系统测量误差进行了校正。我们提出了一个日常测量的统计修正模型的结果。它是在BALTEX的框架内开发的,并为全球降水气候学中心(GPCC)进行了调整,以校正通过GTS常规传输的全球每日雨量计数据。我们专注于GEWEX大陆规模实验区域BALTEX(欧洲),GAME(亚洲),LBA(南美)和GCIP(北美)。将修正模型应用于1996年、1997年2年的资料,并与广泛使用的Legates(1987)降水气候学的修正因子进行比较。在BALTEX地区,我们的平均每日修正系数大约等于Legates在夏季给出的月修正系数,而Legates估计雪的修正系数更高(高达50%)。在GAME和LBA区域,Legates给出的更正通常也比我们的更正高(50 - 100%)。这与GCIP雨量计计算的修正相反,两者没有显著差异。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Bias correction of global daily rain gauge measurements

Up to the present global precipitation climatologies based on rain gauges have been corrected for systematic measurement errors using monthly correction factors only. We present results from a statistical correction model for daily measurements. It was developed in the framework of BALTEX and adapted for the Global Precipitation Climatology Centre (GPCC) to correct global daily rain gauge data routinely transmitted via GTS. We focus on regions of the GEWEX continental scale experiments BALTEX (Europe), GAME (Asia), LBA (South-America) and GCIP (North- America). The correction model was applied to 2 years of data (1996, 1997) and compared with the correction factors of the widely used precipitation climatology of Legates (1987). In the BALTEX region our averaged daily correction factor is about equal to the monthly correction given by Legates during the summer months, while Legates estimated higher corrections for snow (up to 50 %). In the regions of GAME and LBA the corrections given by Legates are also generally higher (50 – 100 %) than our corrections. This is opposite to the corrections calculated for GCIP rain gauges, which are not significantly different.

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