首页> 外文期刊>Hydrology and Earth System Sciences >A global water cycle reanalysis (2003-2012) merging satellite gravimetry and altimetry observations with a hydrological multi-model ensemble
【24h】

A global water cycle reanalysis (2003-2012) merging satellite gravimetry and altimetry observations with a hydrological multi-model ensemble

机译:全球水循环再分析(2003-2012年),结合了卫星重力测量法和高程观测与水文多模型合奏

获取原文
获取原文并翻译 | 示例
           

摘要

We present a global water cycle reanalysis that merges water balance estimates derived from the Gravity Recovery And Climate Experiment (GRACE) satellite mission, satellite water level altimetry and off-line estimates from several hydrological models. Error estimates for the sequential data assimilation scheme were derived from available uncertainty information and the triple collocation technique. Errors in four GRACE storage products were estimated to be 11-12mm over land areas, while errors in monthly storage changes derived from five global hydrological models were estimated to be 17-28 mm. Prior and posterior water storage estimates were evaluated against independent observations of river water level and discharge, snow water storage and glacier mass loss. Data assimilation improved or maintained agreement overall, although results varied regionally. Uncertainties were greatest in regions where glacier mass loss and subsurface storage decline are both plausible but poorly constrained. We calculated a global water budget for 2003- 2012. The main changes were a net loss of polar ice caps (-342 Gt yr~(-1)) and mountain glaciers (-230 Gt yr~(-1)), with an additional decrease in seasonal snowpack (-18 Gt yr~(-1)). Storage increased due to new impoundments (+16 Gt yr~(-1)), but this was compensated by decreases in other surface water bodies (-10 Gt yr~(-1)). If the effect of groundwater depletion (-92 Gt yr~(-1)) is considered separately, subsurface water storage increased by +202 Gt yr~(-1) due particularly to increased wetness in northern temperate regions and in the seasonally wet tropics of South America and southern Africa. The reanalysis results are publicly available via www.wenfo.org/wald/.
机译:我们提出了一项全球水循环再分析,将重力恢复和气候实验(GRACE)卫星任务,卫星水位测高法和几种水文模型的离线估算得出的水平衡估算值合并在一起。顺序数据同化方案的误差估计是从可用的不确定性信息和三重配置技术得出的。四种GRACE储藏产品在陆地上的误差估计为11-12mm,而来自五个全球水文模型的月度储藏变化误差估计为17-28mm。根据对河水水位和流量,雪水储量和冰川质量损失的独立观察,评估了之前和之后的储水量估计。数据同化总体上改善或保持了一致,尽管结果因地区而异。在冰川质量损失和地下储藏量下降均是合理的但受制于约束的地区,不确定性最大。我们计算了2003-2012年的全球水资源预算。主要变化是极地冰盖(-342 Gt yr〜(-1))和高山冰川(-230 Gt yr〜(-1))的净损失,季节性积雪进一步减少(-18 Gt yr〜(-1))。由于新的蓄水量(+16 Gt yr〜(-1)),存储量增加了,但是这被其他地表水体的减少(-10 Gt yr〜(-1))所补偿。如果单独考虑地下水枯竭的影响(-92 Gt yr〜(-1)),则地下水的储量增加了+202 Gt yr〜(-1),这主要是由于北部温带地区和季节性湿热带地区的湿度增加南美和南部非洲。重新分析的结果可通过www.wenfo.org/wald/公开获得。

著录项

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