Download Earth System Monitoring: Selected Entries from the by John Orcutt PDF

By John Orcutt

Modern Earth method tracking represents a basic swap within the manner scientists research the Earth System.  In Oceanography, for the prior centuries, ships have supplied the systems for observing.  Expeditions at the continents and Earth’s poles are land-based analogues. primary figuring out of present structures, weather, average dangers, and ecosystems has been drastically complicated. whereas those techniques were remarkably winning, the necessity to determine measurements over the years can in simple terms be made utilizing Earth observations and observatories with exacting criteria and non-stop data.  the nineteen peer-reviewed contributions during this quantity supply early insights into this emerging view of Earth in either house and time within which switch is a severe part of our growing understanding.

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IEEE Trans Geosc Remote Sens 44(10): 2991–2995 61. Joughin I, Gray L, Bindschadler R, Price S, Morse D, Hulba C, Mattar K, Werner C (1999) Tributaries of West Antarctic ice streams revealed by RADARSAT interferometer. Science 286:283–286 62. Stearns L, Jezek K, Van der Veen CJ (2005) Decadal scale variations in ice flow along Whillans ice stream and its tributaries, West Antarctica. J Glaciol 51(172): 147–157 63. Beem L, Jezek K, van der Veen CJ (2010) Basal melt rates beneath the Whillans ice stream, West Antarctica.

J Glaciol 54(185):203–212 84. Rignot E, Velicogna I, van den Broeke MR, Monaghan A, Lenaerts J (2011) Acceleration of the contribution of the Greenland and Antarctic ice sheets to sea level rise. Geophys Res Lett 38:L05503. 1029/2011GL046583 85. Hall D, Riggs G, Salomonson V, DiGirolamo N, Bayr K (2002) MODIS snow-cover products. Remote Sens Environ 83:181–194 86. Dery S, Brown R (2007) Recent northern hemisphere snow cover extent trends and implications for the snow-albedo feedback. Geophys Res Lett 34:L22504.

C. Jezek 2 Airborne and Space-borne Remote Sensing of Cryosphere 27 US, Canada, Russia, China, Japan, and the European Space Agency (ESA), which in itself represents 19 nations. The STG determined how best to satisfy GIIPSY science requirements in a fashion that distributed the acquisition burden across the space agencies and recognized the operational mandates that guide the activities of each agency. The STG adopted four primary data acquisition objectives for its contribution to the IPY. These are: • Pole to coast multi-frequency InSAR measurements of ice-sheet surface velocity • Repeat fine-resolution SAR mapping of the entire Southern Ocean sea ice cover for sea ice motion • One complete high resolution visible and thermal IR (Vis/IR) snapshot of circumpolar permafrost • Pan-Arctic high and moderate resolution Vis/IR snapshots of freshwater (lake and river) freeze-up and breakup The STG achieved most of these objectives including: acquiring Japanese, ALOS L-band, ESA Envisat and Canadian Radarsat C-band, and German TerraSAR-X (Fig.

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