The Advanced Technology Microwave Sounders (ATMS), carried on the Suomi National Polar-orbiting Partnership (S-NPP) satellite, was launched on October 28, 2011. The ATMS is a follow-on instrument to Advanced Microwave Sounding Unit (AMSU), currently flying on National Oceanic and Atmospheric Administration (NOAA) satellites. The primary new ATMS features are a reduced hardware package and improved gap coverage. One thing in common about cross-track sounders is a scan perpendicular to the motion of the satellite, allowing a broad swath of measurements to be taken. But an undesirable feature is that the measurements vary with scan angle because of changes in the optical pathlength through the earth's atmosphere between the earth and the satellite. One approach to this problem is to limb adjust the measurements to a fixed view angle. The limb correction algorithm applied to ATMS is based on the heritage methodology originally applied to MSU and later to AMSU. The limb correction method is applied to each of the 96 ATMS field-of-view (FOV) per scan line, adjusting the off-nadir FOV to the nadir view with fitting error generally within the instrumental noise. The limb adjusted brightness temperature were used in the original, legacy TOVS and ATOVS NOAA sounding product algorithms and more recently to derive the total precipitation water (TPW) retrieval over ocean, with a bias of 0.046 mm and a standard deviation of 3.43 mm, when compared with ECMWF TPW data. The limb corrected brightness temperature can be used to detect the atmospheric weather features, such as the warm cores for tropical cyclones, and the imagery presents snapshots for quick weather signal diagnosis.
[1]
M. Goldberg,et al.
Joint Polar Satellite System: The United States next generation civilian polar‐orbiting environmental satellite system
,
2013
.
[2]
Fuzhong Weng,et al.
Uses of NOAA-16 and -18 Satellite Measurements for Verifying the Limb-Correction Algorithm
,
2007
.
[3]
Antonia Gambacorta,et al.
A review of sources of systematic errors and uncertainties in observations and simulations at 183 GHz
,
2016
.
[4]
Hu Yang,et al.
Validation of ATMS Calibration Accuracy Using Suomi NPP Pitch Maneuver Observations
,
2016,
Remote. Sens..
[5]
Christopher D. Barnet,et al.
Microwave radiative transfer model validation
,
2006
.
[6]
Lihang Zhou,et al.
An Overview of the Joint Polar Satellite System (JPSS) Science Data Product Calibration and Validation
,
2016,
Remote. Sens..
[7]
Quanhua Liu,et al.
Community Radiative Transfer Model (CRTM) applications in supporting the Suomi National Polar-orbiting Partnership (SNPP) mission validation and verification
,
2014
.
[8]
Fuzhong Weng,et al.
Advanced microwave sounding unit cloud and precipitation algorithms
,
2003
.
[9]
D. Wark.
Adjustment of TIROS operational vertical sounder data to a vertical view
,
1993
.
[10]
Fuzhong Weng,et al.
Determination of precipitable water and cloud liquid water over oceans from the NOAA 15 advanced microwave sounding unit
,
2001
.
[11]
Mitchell D. Goldberg,et al.
The Limb Adjustment of AMSU-A Observations: Methodology and Validation
,
2001
.