RESTRICTED only accessable in ZMAW network or via CliSAP login What does that mean?
Objectives and applications:
Coverage, spatial and temporal resolution
Period and temporal resolution:
Coverage and spatial resolution:
Note: We are offering 3-day composites, mainly because the resulting fields cover the complete ocean (rain flag excluded).
Upon request we also offer data of the single satellite overpasses. These have data gaps however. The advantage of this data is that the overpass time is available for each overpass, allowing to compare this data with, e.g., buoy data.
Note: Wind direction 0° (180°) is a wind blowing TOWARDS north (TOWARDS south) - according to the oceanographic convention; u- and v-component however are as usual POSITIVE pointing towards east and north, respectively.
The data set offered here does not include any explicit uncertainty estimations.
The following things have be taken into account when using this data set.
1) Radar backscatter intensities of the water surface as measured by QuikSCAT are as accurate as 0.2 dB.
2) Wind speed retrieval is carried out using a model function which translates between wind-induced water surface roughness and the measured radar backscatter intensity. This translation is straight forward and retrieved wind speeds compare to buoy observations with about 0 m/s difference and an RMS below 1 m/s. The retrieval of the wind direction is more difficult because of signal ambiguities. These are mitigated by including NCEP/NCAR model derived wind directions into the retrieval.
3) The offered 3-day composites comprise wind vector estimates of a maximum of 6 (minimum of 2) QuikSCAT overpasses (both ascending and descending). In areas of highly varying wind speeds and directions the obtained mean values might not reflect the real strength and direction of the wind.
4) Precipitation influences the measured radar backscatter intensity either directly by scattering of the microwave radiation by the precipitation particles or indirectly by adding to the water surface roughness due to precipitation particles impinging on the water surface. These areas are flagged invalid in these data. The data flag either relies directly on the QuikSCAT data and the model function or it may rely in addition on precipitation rates retrieved from near-coincident satellite passive microwave observations.
CliSAP / KlimaCampus
email: stefan.kern@ zmaw.de
CliSAP / KlimaCampus
email: annika.jahnke-bornemann@ zmaw.de
When using these 3-day composites please include the following note:
SeaWinds data are produced by Remote Sensing Systems and sponsored by the NASA Ocean Vector Winds Science Team. Data are available at www.remss.com, distributed in netCDF format by the Integrated Climate Data Center (ICDC, http://icdc.zmaw.de) University of Hamburg, Hamburg, Germany.