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Sea ice remote sensing from space
Remote Sensing I Lecture 10 Summer 2006
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Sea ice remote sensing from space
Optical (e.g. MODIS) High resolution (about 100 meters) Can‘t „see“ through clouds; difficult to distinguish clouds and sea ice Passive Microwave Can differentiate between open water, first year and multiyear ice Can „see“ through clouds Low spatial resolution (several km) Radar Can look through clouds High spatial resolution (< 1km) Images difficult to interprete
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MODIS - Antarctica 21 March 2005
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Radar Image ENVISAT ASAR 15 April 2005
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Sea ice concentration from AMSR-E 89 GHz
09 July 2006 courtesy of Lars Kaleschke
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Sea ice concentration from AMSR-E 89 GHz
23 April 2006 courtesy of Lars Kaleschke
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1. RADAR
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Real Aperture Radar Viewing angle θ h S Opening angle β Xa Xr
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Antenna beamwidth The opening angle β (beamwidth) of an antenna with aperture D at a wavelength of λ is given by: The azimuth resolution for a real aperture radar is then
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Azimuth resolution fro real aperture radar
Example: h=800km, λ=23cm, D=12m then Xa=16km This is a coarse resolution!
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Synthetic aperture radar: Schematic
L Radar flight direction Ground L
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Synthetic aperture radar
Ground „footprint“ L given by: Individual measurements can be combined, corresponding to a Measurement with a virtual or synthetic aperture of size L. The resolution for such a synthetica aperture radar (SAR) is then given by:
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2. Passive Microwave Sensors
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Passive microwave remote sensing
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Emissivity of Sea Ice vs. Frequency
Summer First year Ice Multiyear Ice Emissivity Water Frequency [GHz]
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Polarization Ratio (PR) and Spectral Gradient (GR)
Clouds
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Sea ice concentration The sea ice surface concentration C can then be calculated from the contributions of the three base points for open water, first year ice, and multi year ice. The sum of the three concentrations must sum to unit:
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MODIS 645, 555, 469 nm AMSR-E 89 GHz courtesy of Lars Kaleschke
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Optical tick clouds are still transparent at 89 GHz
courtesy of Lars Kaleschke
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courtesy of Lars Kaleschke
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