JP4.4
Satellite-Derived Poleward Moisture Transport Over the Southern Oceans
Cheng-Zhi Zou, NOAA/NESDIS, Camp Springs, MD; and M. L. Van Woert
ABSTRACT Meridional moisture transport across the Southern Ocean in 1988 is reinvestigated by applying conservation of mass to the wind derivation approach of Slonaker and Van Woert. The moisture field is derived from the TIROS Operational Vertical Sounder (TOVS). The wind field is derived by using thermal wind assumption and a combination of TOVS temperature data and Special Sensor Microwave/Imager (SSM/I) satellite surface wind data. A variational method is developed to apply the mass balance correction to the thermal wind. The resulting annual mean winds compare favorably to the Macquarie Island radiosonde observations, and ECMWF (European Center for Medium-Range Weather Forecasts) and CDAS (Climate Data Assimilation System of NCEP/NCAR) reanalyses.
The mass balance correction reduces the moisture transport estimation dramatically compared to the previous Slonaker and Van Woert results using the same dataset. In Slonaker and Van Woert's study, the zonally-averaged, vertically-integrated moisture flux across 50S is -31.8 kg m-1 s-1; while the value of this study is only -14.1 kg m-1 s-1. The net precipitation estimation also substantially differs between the two studies. Between the 50S-60S latitude belt, the zonally averaged net precipitation from Slonaker and Van Woert is 636 mm yr-1, while in this study the estimation is 233 mm yr-1.
The reason for the difference is that the wind derivation approach without conservation of mass used by Slonaker and Van Woert leads to unrealistically strong annual mean wind speeds in the lower troposphere. Their strong mean wind estimates resulted in exaggerated mean moisture transport compared to other studies. The conservation of mass corrects the problem and produces mean moisture flux consisted with historical estimates.
The eddy moisture flux of the satellite derived in both Slonaker and Van Woert's study and the current study is underestimated by about 45% compared to radiosonde and analyses studies. This underestimation is most likely due to the lower spatial and temporal resolutions of the satellite observations.
The detailed characteristics of moisture flux across different sectors of the Southern Oceans and comparisons with analyses and radiosonde data will also be discussed.
Topic Area: Climatology and long-term satellite data studies
Joint Poster Session 4, Climatology and Long-Term Satellite Data Studies: Part IV (Joint 1th Symposium on Global Change Studies)
Thursday, 13 January 2000, 3:00 PM-5:00 PM
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