Estimation of Wind Induced Ocean Microwave Emission at C- and X-band Frequencies from the AMSR2 Measurements over the Arctic Waters

E. Zabolotskikh, B. Chapron
{"title":"Estimation of Wind Induced Ocean Microwave Emission at C- and X-band Frequencies from the AMSR2 Measurements over the Arctic Waters","authors":"E. Zabolotskikh, B. Chapron","doi":"10.1109/piers55526.2022.9792892","DOIUrl":null,"url":null,"abstract":"Passive microwave ocean response to sea surface wind speed at C- and X-bands is estimated using numerical modeling of the atmosphere — ocean system brightness temperatures (BTs) and the measurements of the Advanced Microwave Scanning Radiometer 2 (AMSR2) over cold waters. A large dataset of the AMSR2 measurements over the Arctic open water seas for a whole year is collected to match up measurements and modeling results. ERA-Interim reanalysis data are explored to calculate the AMSR2 BTs. The sea surface wind speeds (SWS) are retrieved from the AMSR2 6.9 and 10.65 GHz measurements at both vertical and horizontal polarization with an algorithm developed earlier using an old version of the geophysical model function (GMF) for the BT dependency on SWS. Only SWS less than 20 m/s are used to derive the new GMFs to minimize the effect of foam. The new GMFs are compared to old ones and found to be very close for both vertically and horizontally polarized microwave signal at 6.9 GHz and a little bit different for the signal at 10.65 GHz — more for vertically and less for horizontally polarized signal. The new experimental models of the ocean response to SWS may be used for verification and elaboration of theoretical GMFs for cold Arctic waters for low to moderate sea surface winds.","PeriodicalId":422383,"journal":{"name":"2022 Photonics & Electromagnetics Research Symposium (PIERS)","volume":"47 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2022-04-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"2022 Photonics & Electromagnetics Research Symposium (PIERS)","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1109/piers55526.2022.9792892","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0

Abstract

Passive microwave ocean response to sea surface wind speed at C- and X-bands is estimated using numerical modeling of the atmosphere — ocean system brightness temperatures (BTs) and the measurements of the Advanced Microwave Scanning Radiometer 2 (AMSR2) over cold waters. A large dataset of the AMSR2 measurements over the Arctic open water seas for a whole year is collected to match up measurements and modeling results. ERA-Interim reanalysis data are explored to calculate the AMSR2 BTs. The sea surface wind speeds (SWS) are retrieved from the AMSR2 6.9 and 10.65 GHz measurements at both vertical and horizontal polarization with an algorithm developed earlier using an old version of the geophysical model function (GMF) for the BT dependency on SWS. Only SWS less than 20 m/s are used to derive the new GMFs to minimize the effect of foam. The new GMFs are compared to old ones and found to be very close for both vertically and horizontally polarized microwave signal at 6.9 GHz and a little bit different for the signal at 10.65 GHz — more for vertically and less for horizontally polarized signal. The new experimental models of the ocean response to SWS may be used for verification and elaboration of theoretical GMFs for cold Arctic waters for low to moderate sea surface winds.
查看原文
分享 分享
微信好友 朋友圈 QQ好友 复制链接
本刊更多论文
北极海域AMSR2测量的C波段和x波段风致海洋微波辐射估算
利用大气-海洋系统亮度温度(BTs)的数值模拟和先进微波扫描辐射计2 (AMSR2)在冷水上的测量结果,估计了被动微波海洋对海面风速在C和x波段的响应。收集了一整年北极开放水域AMSR2测量数据的大型数据集,以匹配测量结果和建模结果。利用ERA-Interim再分析数据计算AMSR2 bt。海面风速(SWS)由AMSR2的6.9 GHz和10.65 GHz垂直和水平极化测量数据反演,采用较早开发的算法,利用旧版本的地球物理模型函数(GMF)来处理BT对SWS的依赖。仅使用小于20 m/s的SWS来推导新的GMFs,以尽量减少泡沫的影响。将新的GMFs与旧的GMFs进行比较,发现在6.9 GHz垂直和水平极化的微波信号中,新GMFs非常接近,而在10.65 GHz的信号中则略有不同——垂直极化信号更大,水平极化信号更小。海洋对SWS响应的新实验模型可用于验证和阐述北极冷水域低至中等海面风的理论gmf。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 去求助
来源期刊
自引率
0.00%
发文量
0
期刊最新文献
Artificial Doppler and Micro-Doppler Effect Induced by Time-modulated Metasurface A Physics-based Compact Model for Set Process of Resistive Random Access Memory (RRAM) with Graphene Electrode An Overview of Metamaterial Absorbers and Their Applications on Antennas Spatio-Temporal Data Prediction of Braking System Based on Residual Error Homogenization Based Fast Computation of Electromagnetic Scattering by Inhomogeneous Objects with Honeycomb Structures
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
已复制链接
已复制链接
快去分享给好友吧!
我知道了
×
扫码分享
扫码分享
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1