首页> 外文期刊>Journal of Geophysical Research, C. Oceans: JGR >Ganga-Brahmaputra river discharge from Jason-2 radar altimetry: An update to the long-term satellite-derived estimates of continental freshwater forcing flux into the Bay of Bengal
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Ganga-Brahmaputra river discharge from Jason-2 radar altimetry: An update to the long-term satellite-derived estimates of continental freshwater forcing flux into the Bay of Bengal

机译:Jason-2雷达测高仪的恒河-布拉马普特拉河排放量:对长期卫星估算的大陆淡水强迫流入孟加拉湾的最新动态

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This paper discusses the use of Jason-2 radar altimeter measurements to estimate the Ganga-Brahmaputra surface freshwater flux into the Bay of Bengal for the period mid-2008 to December 2011. A previous estimate was generated for 1993-2008 using TOPEX-Poseidon, ERS-2 and ENVISAT, and is now extended using Jason-2. To take full advantages of the new availability of in situ rating curves, the processing scheme is adapted and the adjustments of the methodology are discussed here. First, using a large sample of in situ river height measurements, we estimate the standard error of Jason-2-derived water levels over the Ganga and the Brahmaputra to be respectively of 0.28 m and 0.19 m, or less than ~4% of the annual peak-to-peak variations of these two rivers. Using the in situ rating curves between water levels and river discharges, we show that Jason-2 accurately infers Ganga and Brahmaputra instantaneous discharges for 2008-2011 with mean errors ranging from ~2180 m ~3/s (6.5%) over the Brahmaputra to ~1458 m ~3/s (13%) over the Ganga. The combined Ganga-Brahmaputra monthly discharges meet the requirements of acceptable accuracy (15-20%) with a mean error of ~16% for 2009-2011 and ~17% for 1993-2011. The Ganga-Brahmaputra monthly discharge at the river mouths is then presented, showing a marked interannual variability with a standard deviation of ~12500 m ~3/s, much larger than the data set uncertainty. Finally, using in situ sea surface salinity observations, we illustrate the possible impact of extreme continental freshwater discharge event on the northern Bay of Bengal as observed in 2008.
机译:本文讨论了使用Jason-2雷达高度计测量来估计2008年中至2011年12月期间恒河-布拉马普特拉地表的淡水通入孟加拉湾的情况。先前使用TOPEX-Poseidon对1993-2008年进行了估算, ERS-2和ENVISAT,现在使用Jason-2进行了扩展。为了充分利用原位额定曲线的新优势,将对处理方案进行调整,并在此讨论方法的调整。首先,使用大量的原位河高测量样本,我们估计恒河和雅鲁藏布江上Jason-2派生水位的标准误差分别为0.28 m和0.19 m,或小于水位的〜4%。这两条河的年峰峰值变化。利用水位和河流排放之间的原位定额曲线,我们发现Jason-2可以准确推断2008-2011年的Ganga和Brahmaputra瞬时流量,在Brahmaputra上平均误差范围为〜2180 m〜3 / s(6.5%)。恒河上方〜1458 m〜3 / s(13%)。 Ganga-Brahmaputra合并排放量满足可接受的精度要求(15-20%),2009-2011年的平均误差为〜16%,1993-2011年的平均误差为〜17%。然后给出了河口的Ganga-Brahmaputra月度流量,显示出明显的年际变化,标准偏差为〜12500 m〜3 / s,远大于数据集的不确定性。最后,使用原位海表盐度观测,我们举例说明了2008年观测到的极端大陆淡水排放事件对孟加拉北部湾的可能影响。

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