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), wind and relative humidity profiles from airborne lidar ( Weissmann et al. 2005 ), or dropwindsondes and remotely sensed observations mounted aboard high-altitude, long-endurance unmanned aircraft systems ( MacDonald 2005 ). In contrast to campaigns such as Winter Storm Reconnaissance (WSR; Szunyogh et al. 2002 ) in which limited targeted data are collected at one synoptic time, one may consider temporally continuous data from satellites or unmanned platforms over the ocean. For instance, in
), wind and relative humidity profiles from airborne lidar ( Weissmann et al. 2005 ), or dropwindsondes and remotely sensed observations mounted aboard high-altitude, long-endurance unmanned aircraft systems ( MacDonald 2005 ). In contrast to campaigns such as Winter Storm Reconnaissance (WSR; Szunyogh et al. 2002 ) in which limited targeted data are collected at one synoptic time, one may consider temporally continuous data from satellites or unmanned platforms over the ocean. For instance, in
