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Published byPaulina Dickerson Modified over 9 years ago
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Landsat – A key climate sensor Compton Tucker NASA/Goddard Space Flight Center Greenbelt, Maryland and Climate Change Science Program Washington DC
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Houston, We Have a Problem… We are altering our planet’s climate
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Atmospheric CO 2 since 1740 Different CO 2 slopes time reflect techno-economic conditions 385 ppm now
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What? Me worry?
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What do we need to be rescued from?
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Landsat – A key climate sensor Absolutely crucial land climate sensors: Landsat 1972 – now AVHRR-MODIS-VIIRS continuum 1981 -- now Lidar for the 3 rd Dimension (DESDnyI) Why? Land use, land cover change Carbon cycle land Cryosphere, etc.
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Landsat – A key climate sensor Why? 1.30 m spatial resolution close-to-perfect match to surface variability (Townshend and Justice 1988) 2.Spectral bands are well situated 3.Repeat cycle OK 4.Excellent data system
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Tropical Glaciers of Peru & Bolivia: Landsat data from 1972 to 2008 90% of world’s tropical glaciers are in Peru (70%) and Bolivia (20%) 5500-6500+ m elevations, summer growth/winter recession Compton Tucker, Tim Killeen, and Dan Slayback NASA/GSFC Code 610 & Conservation International NASA/GSFC Code 610 & Conservation International
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Study Area and Landsat Scenes Used (WRS-2)
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Cordillera Blanca Peru 2006
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Cordillera Blanca 22-Jul-2006 / TM5 / 543
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Landsat-4/5 TM Data Used
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Tropical Glaciers of Peru & Bolivia: 1982-1986: 2,854 km 2 2006-2007: 2,150 km 2 90% of world’s tropical glaciers are in Peru (70%) and Bolivia (20%) 5500-6500+ m elevations, summer growth/winter recession
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How to enhance Landsat Landsat exploits the spatial & spectral domains – 30 m spatial resolution excellent – Excellent spectral band selection Exploit the time domain (e.g. AVHRR, MODIS, Seawifs, etc.) but at 30 m spatial resolution with TM/ETM spectral bands Wider field of view, 4-5 day repeat cycle Build multiple instruments (e.g. Landsat-5’s TM) = Continuity!!
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Tropical Air Temperature
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Cloud cover variations 1978 to 2004
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