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Journal ArticleDOI

Effects of Antenna Cross-Polarization Coupling on the Brightness Temperature Retrieval at L-Band

TLDR
The formal proof of the insensitivity is presented: when the Faraday rotation correction is performed by the square sum of the two retrieved Stokes, the retrieved TB below the ionosphere and at the top of the atmosphere after thefaraday correction becomes insensitive to the additional rotation.
Abstract
Retrieval of the brightness temperature (TB) at the L-band is studied in the context of the remote sensing of ocean surface salinity. The measurement of antenna temperature and the retrieval of TB are simulated with a radiative transfer model and an observing system model of an orbiting spacecraft. Two sets of antenna gain patterns are used: 1) theoretical analysis and 2) measurements of a 1/10th-size scale model. The latter set notably shows the large cross-polarization coupling from the first Stokes transmit into the third Stokes receive. The large cross-polarization coupling causes an error of up to 4° in the estimate of the Faraday rotation angle (the size of the angle itself is mostly less than 15° in the severe ionospheric condition). By this amount of the error, an additional rotation is introduced to the retrieval of the second and third Stokes TBs in front of the feed horn before the Faraday rotation correction. The additional rotation also degrades the performance of the antenna pattern correction (APC). However, when the Faraday rotation correction is performed by the square sum of the two retrieved Stokes, the retrieved TB below the ionosphere and at the top of the atmosphere after the Faraday correction becomes insensitive to the additional rotation (i.e., being insensitive to the error in the Faraday angle estimate and the rotational error in the APC). The formal proof of the insensitivity is presented. The first and second Stokes TBs at the top of the atmosphere observed at 5.6-s intervals from space may be retrieved with an error smaller than 0.1-K rms without the accurate ancillary information of the gain pattern and the Faraday rotation angle, assuming correct calibration, 0.08 K NEΔT for the radiometer noise, and accurate correction or flagging of the solar and galaxy radiation.

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Citations
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Journal ArticleDOI

Aquarius L-band Radiometers Calibration Using Cold Sky Observations

TL;DR: The cold sky calibration for Aquarius is described and how it is used as part of the absolute calibration of the Aquarius radiometers.
Journal ArticleDOI

Weekly gridded Aquarius L-band radiometer/scatterometer observations and salinity retrievals over the polar regions – Part 1: Product description

TL;DR: In this paper, the authors presented three weekly polar-gridded products of Aquarius data to improve our understanding of L-band observations of ice sheets, sea ice, permafrost, and the polar oceans.

Sea surface salinity variability in the East China Sea observed by the Aquarius instrument

TL;DR: In this paper, the authors demonstrate that the spaceborne Aquarius instrument is able to monitor the sea surface salinity (SSS) variations in the East China Sea (ECS) with the spatial resolution of about 150 km at 7 day interval, where routine observations are difficult.
Journal ArticleDOI

Sea surface salinity variability in the East China Sea observed by the Aquarius instrument

TL;DR: In this article, the authors demonstrate that the spaceborne Aquarius instrument is able to monitor the sea surface salinity (SSS) variations in the East China Sea (ECS) with the spatial resolution of about 150 km at 7 day interval, where routine observations are difficult.
References
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Book

Microwave Remote Sensing, Active and Passive

TL;DR: In this article, the authors present a model of a MICROWAVE REMOTE SENSING FUNDAMENTALS and RADIOMETRY, which is based on the idea of surface scattering.
Journal ArticleDOI

The SMOS Mission: New Tool for Monitoring Key Elements ofthe Global Water Cycle

TL;DR: The SMOS satellite was launched successfully on November 2, 2009, and will achieve an unprecedented maximum spatial resolution of 50 km at L-band over land (43 km on average over the field of view), providing multiangular dual polarized (or fully polarized) brightness temperatures over the globe.
Journal ArticleDOI

A well‐calibrated ocean algorithm for special sensor microwave / imager

TL;DR: In this article, the authors describe an algorithm for retrieving geophysical parameters over the ocean from special sensor microwave/imager (SSM/I) observations, based on a model for the brightness temperature T(sub B) of the ocean and intervening atmosphere.
Journal ArticleDOI

The complex dielectric constant of pure and sea water from microwave satellite observations

TL;DR: A new fit for the microwave complex dielectric constant of water in the salinity range between 0-40 ppt using two Debye relaxation wavelengths is provided and a validation using an extensive analysis of brightness temperatures from the Special Sensor Microwave Imager is provided.
Journal ArticleDOI

The Aquarius/SAC-D mission: Designed to meet the salinity remote-sensing challenge

TL;DR: The Aquarius/SAC-D mission as discussed by the authors was designed to provide monthly global salinity measurements at a similar, scientifically useful accuracy and spatio-temporal resolution, and it came at a time of growing scientific awareness of the need for the data.
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