...
首页> 外文期刊>SOLA: Scientific Online Letters on the Atmosphere >Direct Validation of TRMM/PR Near Surface Rain over the Northeastern Indian Subcontinent Using a Tipping Bucket Raingauge Network
【24h】

Direct Validation of TRMM/PR Near Surface Rain over the Northeastern Indian Subcontinent Using a Tipping Bucket Raingauge Network

机译:使用翻斗式雨量计网络直接验证印度东北亚次大陆的TRMM / PR近地表雨

获取原文
           

摘要

The near surface rain (NSR) dataset of the Tropical Rainfall Measurement Mission (TRMM) Precipitation Radar (PR) 2A25 V7 was validated using 36 tipping bucket raingauges installed over the northeastern Indian subcontinent, which correspond with the rain center of the Asian summer monsoon. This raingauge network covers the Brahmaputra flood plains and mountainous areas, including the Meghalaya Plateau, which is one of the wettest places in the world. We analyzed data from 2004 to 2013, and obtained 28,207 TRMM/PR-raingauge matchups with 2,170 TRMM/PR rainy field of views. Using them, we detected a reasonable time lag of around 300 seconds between the estimates from the TRMM/PR NSR and raingauges. Significant and large underestimations of TRMM/PR NSR were detected during the monsoon season (June–September) over the large areas of Meghalaya, Sylhet, and Barak. The bias ratios were ?51.3% and ?35.2% for the Meghalaya and Sylhet-Barak areas, respectively. In the Meghalaya subregion, major contribution to underestimation came from moderate TRMM/PR NSR from stratiform systems, and missed detection error was secondary contributor. In Sylhet-Barak subregion, moderate TRMM/PR NSR from convective systems largely contributed. Underestimation was not detected in premonsoon season (March–May).
机译:热带印度降水量测量任务(TRMM)降水雷达(PR)2A25 V7的近地表降雨(NSR)数据集使用安装在印度东北亚次大陆上的36个翻斗式雨量计进行了验证,该雨量计与亚洲夏季风的降雨中心相对应。该雨量计网络覆盖了雅鲁藏布江泛滥平原和山区,包括梅加拉亚高原,梅加拉亚高原是世界上最潮湿的地方之一。我们分析了2004年至2013年的数据,获得了28,207个TRMM / PR-雨量计搭配以及2,170个TRMM / PR雨天视野。使用它们,我们在TRMM / PR NSR和雨量计的估计值之间发现了大约300秒的合理时滞。在季风季节(6月至9月)的梅加拉亚邦,锡尔赫特和巴拉克大片地区,TRMM / PR NSR明显低估。梅加拉亚邦和锡尔赫特-巴拉克地区的偏倚率分别约为51.3%和35.2%。在梅加拉亚邦次区域,低估的主要贡献来自于层状系统的适度TRMM / PR NSR,而漏检探测误差是次要原因。在锡尔赫特-巴拉克(Sylhet-Barak)次区域,对流系统产生的中等TRMM / PR NSR贡献很大。在季风季节(3月至5月)未发现低估。

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号