Open AccessA method for including mesoscale and synoptic‐scale information in scatterometer wind retrievals
Author(s) -
Patoux Jérôme,
Foster Ralph C.,
Brown Robert A.
Publication year - 2010
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2009jd013193
Subject(s) - scatterometer , mesoscale meteorology , environmental science , meteorology , remote sensing , buoy , planetary boundary layer , wind speed , scale (ratio) , synoptic scale meteorology , geology , geography , oceanography , cartography , turbulence
A method for improving scatterometer wind retrievals based on the mesoscale and synoptic‐scale structure of the flow field is presented and evaluated. The large‐scale structure of the flow is inferred from the sea‐level pressure (SLP) field derived from the scatterometer winds using a planetary boundary layer model. The wind vectors derived from this SLP field can be used to either (1) inform the ambiguity selection, (2) correct the direction of the scatterometer wind vectors, in all cases or above a certain threshold, or (3) replace the scatterometer winds. The methodology is demonstrated with QuikSCAT (QS) scatterometer wind vectors. The new wind vector set is evaluated statistically by comparison with buoy measurements, with numerical weather prediction model analyses, and by spectral analysis. It is found that the new wind vectors are particularly valuable at nadir and in rain‐contaminated areas, and that their spectral behavior is closer to a power law than are the uncorrected QS winds.