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Intra-seasonal variability in Oceansat-2 scatterometer sea-surface winds over the Indian summer monsoon region

机译:印度夏季风地区Oceansat-2散射仪海面风的季节内变化

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摘要

In September 2009, the Indian Space Research Organisation launched a Ku-band microwave scatterometer (OSCAT) onboard the polar orbiting satellite 'Oceansat-2'. In this article, the capabilities of the newly available OSCAT sea-surface winds are demonstrated by studying the monsoon intra-seasonal variabilities during the 2010 summer monsoon season. A preliminary validation of OSCAT surface winds with European Centre for Medium Range Weather Forecasting (ECMWF) analysis surface winds carried out during June to August 2010 suggests that the quality of the OSCAT winds are able to meet the mission specifications. The observed mean monthly features of the Indian summer monsoon in July and August 2010 from OSCAT match well with those of ECMWF reanalysis winds. The OSCAT winds capture the known characteristics of the Indian summer monsoon, such as the northward propagation of a low level jet, and its preferred locations during active and break monsoon conditions, reasonably well. The Morlet wavelet transform is used for time series analysis. The OSCAT measured sea-surface winds were found to possess two dominant modes of variability during the 2010 monsoon season: one with a periodicity between 32 and 64 days, and another with a periodicity between 8 and 16 days. Rainfall activity over the Indian summer monsoon region is closely associated with the phases of the two above-mentioned dominant intra-seasonal variabilities. This study demonstrates that the OSCAT winds can be used very well and with confidence for meteorological studies.
机译:2009年9月,印度航天研究组织在极地轨道卫星“ Oceansat-2”上发射了Ku波段微波散射仪(OSCAT)。在本文中,通过研究2010年夏季季风季节的季风季节内变化,证明了新近可用的OSCAT海面风的能力。欧洲中程天气预报中心(ECMWF)分析地面风在2010年6月至8月进行了OSCAT地面风的初步验证,这表明OSCAT风的质量能够满足任务规范。 OSCAT观测到的印度夏季风在2010年7月和2010年8月的平均月度特征与ECMWF再分析风的特征相吻合。 OSCAT风捕捉到了印度夏季风的已知特征,例如低空急流向北传播,以及在活跃季风和断裂季风条件下的最佳位置。 Morlet小波变换用于时间序列分析。发现OSCAT测量的海面风在2010年季风季节具有两种主要的变化模式:一种周期为32至64天,另一种周期为8至16天。印度夏季风区域的降雨活动与上述两个主要的季节内主要变化的阶段密切相关。这项研究表明OSCAT风能很好地用于气象学研究,并且充满信心。

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