2016
DOI: 10.1109/tgrs.2016.2600239
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SMAP L-Band Passive Microwave Observations of Ocean Surface Wind During Severe Storms

Abstract: Please note that this is an author-produced PDF of an article accepted for publication following peer review. The definitive publisher-authenticated version is available on the publisher Web site.

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Cited by 63 publications
(38 citation statements)
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References 18 publications
(42 reference statements)
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“…The impact of the different spatial resolutions is presented in Figure b. This comparison shows the benefit of high‐resolution compared to medium‐resolution missions such as L‐band radiometers (about 40 km for Soil Moisture Active Passive (SMAP); Meissner et al, ; Yueh et al, ; or Soil Moisture and Ocean Salinity (SMOS); Reul et al, ) or scatterometers (about 25 km for nominal resolution with the next European SCA on MeTop SG; Stoffelen et al, ). In this case, larger averaging areas blur the interpretation of the data, clearly showing that both the central wind minimum and peakedness of the wind maxima are severely impacted at spatial resolutions exceeding 12 km.…”
Section: Discussionmentioning
confidence: 99%
“…The impact of the different spatial resolutions is presented in Figure b. This comparison shows the benefit of high‐resolution compared to medium‐resolution missions such as L‐band radiometers (about 40 km for Soil Moisture Active Passive (SMAP); Meissner et al, ; Yueh et al, ; or Soil Moisture and Ocean Salinity (SMOS); Reul et al, ) or scatterometers (about 25 km for nominal resolution with the next European SCA on MeTop SG; Stoffelen et al, ). In this case, larger averaging areas blur the interpretation of the data, clearly showing that both the central wind minimum and peakedness of the wind maxima are severely impacted at spatial resolutions exceeding 12 km.…”
Section: Discussionmentioning
confidence: 99%
“…The algorithm to retrieve SSS from SMAP radiometer data has been developed at 59 the Jet Propulsion Laboratory (JPL) [Fore et al, 2016]. Analyzing available SMAP and 60 matchup ancillary data, it is found that SMAP T B well corroborates the Aquarius GMFs 61 for wind speed up to at least 40 m s -1 [Yueh et al, 2016]. Therefore, the roughness 62 correction which removes excess surface emissivity from SMAP-measured T B is 63 currently based on the Aquarius radiometer GMF.…”
Section: Introduction 36 37mentioning
confidence: 99%
“…The revisit time of SMAP is 8 days. The root-mean-square difference (RMSD) with WindSat or Special Sensor Microwave Imager/Sounder is 1.7 m s 21 for wind speeds lower than 20 m s 21 (Yueh et al 2016). The SMAP measurements also have a good agreement with the airborne Stepped Frequency Microwave Radiometer (SFMR) wind speeds with an RMSD of 4.6 m s 21 for wind speeds between 20 and 40 m s 21 (Yueh et al 2016).…”
Section: B Wind Referencesmentioning
confidence: 82%