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Validation of Tropical Cyclone Heat Potential (TCHP) derived from satellite products over the North Indian Ocean

机译:验证北印度洋卫星产品产生的热带气旋热势(TCHP)

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The North Indian Ocean (NIO) is home to severe depressions and frequent Tropical Cyclones (TCs). TCs are largely influenced by TC Heat potential (TCHP), a major ocean parameter responsible for genesis, intensification changes, as well as their propagation tracks. Hence, accurate estimation of TCHP is highly essential for better prediction of TC track and intensity changes. Conventionally, TCHP is estimated from in situ ocean temperature and salinity profiles. However, owing to the spatio-temporal limitations of in situ measurements, estimation of TCHP from satellite observations of ocean parameters namely, Sea Surface Temperature (SST) and Sea Surface Height Anomaly (SSHA) have attained significance in recent times. In order to examine the reliability of satellite based TCHP estimates and a view to fine-tune retrieval algorithms if necessary, satellite based delayed-time (DT) TCHP data from National Oceanic and Atmospheric Administration (NOAA) are inter-compared with in situ TCHP computed from temperature and salinity observations from Argo autonomous profiling floats. DT-TCHP products are generated using SST measurements and delayed-time AVISO SSHA gridded fields that merge all available satellite observations using an optimal interpolation technique and are available at 0.25° × 0.25° spatial resolution. The inter-comparison exercise in the NIO ranges for a 15 year period, spanning the years 2005 to 2015. The satellite based DT-TCHP products from NOAA are found to have a good match with TCHP from temperature profiles measured using Argo floats with correlation higher than 0.5. It is further found that DT-TCHP from NOAA are slightly overestimated compared to TCHP from Argo profiles. This difference may be interpreted as satellite's inability to capture accurately the daily ocean subsurface variability which are quite prominent in the TCHP computed from autonomous Argo temperature and salinity profiles in the study region.
机译:北印度洋(NIO)是严重的低气压和频繁的热带气旋(TC)的所在地。 TC受TC热潜势(TCHP)的影响很大,而TCH热潜势是导致成因,强度变化及其传播轨迹的主要海洋参数。因此,对TCHP的准确估计对于更好地预测TC轨迹和强度变化非常重要。通常,TCHP是根据原位海洋温度和盐度剖面估算的。然而,由于原位测量的时空局限性,近来从卫星对海洋参数即海面温度(SST)和海面高度异常(SSHA)的观测中估计TCHP变得有意义。为了检查基于卫星的TCHP估计值的可靠性,并在必要时微调检索算法,将美国国家海洋与大气管理局(NOAA)的基于卫星的延迟时间(DT)TCHP数据与原位TCHP进行了相互比较。根据Argo自主轮廓浮标的温度和盐度观测值计算得出。 DT-TCHP产品使用SST测量值和AVISO SSHA延迟时间网格化字段生成,这些字段使用最佳插值技术合并了所有可用的卫星观测结果,并且空间分辨率为0.25°×0.25°。在NIO范围内进行的比对活动范围为2005年至2015年,为期15年。使用Argo浮子测得的温度曲线具有较高的相关性,发现NOAA的基于卫星的DT-TCHP产品与TCHP有很好的匹配性大于0.5。进一步发现,与来自Argo配置文件的TCHP相比,来自NOAA的DT-TCHP稍有高估。这种差异可以解释为卫星无法准确捕获每日海洋表层下的变化,这在根据研究区域的自主Argo温度和盐度剖面计算出的TCHP中非常突出。

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