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首页> 外文期刊>Remote Sensing of Environment: An Interdisciplinary Journal >Evaluation of the Interactive Multisensor Snow and Ice Mapping System (IMS) for monitoring sea ice phenology
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Evaluation of the Interactive Multisensor Snow and Ice Mapping System (IMS) for monitoring sea ice phenology

机译:用于监测海冰物候的交互式多传感器冰雪测绘系统(IMS)的评估

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We present an evaluation of the Interactive Multisensor Snow and Ice Mapping System (IMS) for monitoring northern hemisphere sea ice phenology. Analysts utilize a variety of datasets tomanually derive the daily extent of snow, ice, water and land, available at both 24 and 4 km. The 4 km IMS product was assessed for 2004–2008 against several previously established melt/freeze algorithms using Scatterometer Image Reconstruction (SIR) SeaWinds/QuikSCAT (QuikSCAT) backscatter (σ~°), Advanced Microwave Scanning Radiometer for the Earth Observing System (AMSR-E) brightness temperature (T_B) measurements, data from the Special Sensor Microwave/Image data (SSM/I) and sea ice concentrations derived from DMSP Special Sensor Microwave/Imager–Special Sensor Microwave Imager Sounder (SSMI–SSMIS) data (NASATeam dataset). The resolution possible with the 4 km IMS product allows for better spatial representation of sea ice along the coastlines, the ice edges and in the narrow channels of the Canadian Arctic Archipelago as compared to themicrowave products. IMSdetects openwater earlier and freeze onset later than the automatedmicrowave products, and also allows for the detection of opening, and the subsequent closing, of leads that the other datasets are unable to detect. Using RADARSAT-1 imagery for evaluation, IMS is shown to outperformthe other datasets for the timing and extent of the first openwater detection. IMS identified between 17 and 53% greater openwater coverage than the other datasets in the narrowchannels of theNorthwest Passage (Barrow Strait). In order to further the use of IMS for sea ice applications, we derived two new spatial datasets using the full record of IMS data (4 km: 2004–present, 24 km: 1997–present):melt duration to openwater (duration frommelt onset detectedwith SSM/I passive microwave until openwater detected by IMS) and first year ice cover duration (duration from freeze onset until open water, both detected by IMS).
机译:我们目前对用于监视北半球海冰物候的交互式多传感器冰雪测绘系统(IMS)进行评估。分析人员利用各种数据集来手动得出每天24、4公里处有雪,冰,水和土地的日范围。使用散射仪图像重建(SIR)SeaWinds / QuikSCAT(QuikSCAT)背向散射(σ〜°),用于地球观测系统(AMSR)的先进微波扫描辐射仪,针对2004-2008年4 km IMS产品进行了评估,采用了先前建立的几种融解/冻结算法-E)亮度温度(T_B)测量,来自特殊传感器微波/图像数据(SSM / I)的数据以及源自DMSP的海冰浓度特殊传感器微波/成像器–特殊传感器微波成像仪发声器(SSMI–SSMIS)数据(NASATeam数据集)。与微波产品相比,使用4 km IMS产品可能实现的分辨率可以更好地在加拿大北极群岛的海岸线,冰缘和狭窄通道中显示海冰的空间。 IMS可以比自动化微波产品更早地检测到开水,而冻害的发生要晚于自动化的微波产品,并且还允许检测其他数据集无法检测到的引线的打开和随后的闭合。使用RADARSAT-1影像进行评估,显示IMS在首次开放水域探测的时间和范围方面优于其他数据集。 IMS确定的西北水域(巴罗海峡)狭窄通道的开放水域覆盖率比其他数据集高17%至53%。为了将IMS进一步用于海冰应用,我们使用IMS数据的完整记录(4 km:2004年至今,24 km:1997年至今)得出了两个新的空间数据集:融化到开阔水的持续时间(融化开始的持续时间)使用SSM / I被动微波检测到直到被IMS检测到是开水为止,以及第一年的冰盖持续时间(从冻结开始到开水的持续时间,都被IMS检测到)。

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