Winter season backscatter (?°) evolution of snow covered lake ice was observed by ground-based University of Waterloo X-(9.6 GHz) and Ku-band (17.2 GHz) scatterometers (UW-SCAT) during the winter of 2010-11. The UW-SCAT post-processing procedure allowed for the observation of ?° at the surface (snow/ice interface, ice types) and the ice volume. Observations indicated that: (1) ?° associated with the development of tubular bubbles within the ice volume causes double-bounce of the signal and high returns at X- and Ku-bands; (2) ice types at the surface (grey ice) composed of high density spherical micro-bubbles result in ?° increases at both X- and Ku-bands; and (3) the removal of snow overlying ice results in a drop in Ku-band ?° up to 5.5 dB, exhibiting sensitivity to snow water equivalent.
Ground-based scatterometer observations of snow-covered freshwater lake ice using UW-SCAT (9.6/17.2 GHz)
Macelloni Giovanni;Brogioni Marco
2014
Abstract
Winter season backscatter (?°) evolution of snow covered lake ice was observed by ground-based University of Waterloo X-(9.6 GHz) and Ku-band (17.2 GHz) scatterometers (UW-SCAT) during the winter of 2010-11. The UW-SCAT post-processing procedure allowed for the observation of ?° at the surface (snow/ice interface, ice types) and the ice volume. Observations indicated that: (1) ?° associated with the development of tubular bubbles within the ice volume causes double-bounce of the signal and high returns at X- and Ku-bands; (2) ice types at the surface (grey ice) composed of high density spherical micro-bubbles result in ?° increases at both X- and Ku-bands; and (3) the removal of snow overlying ice results in a drop in Ku-band ?° up to 5.5 dB, exhibiting sensitivity to snow water equivalent.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
