contributor author | Sikora, T. D. | |
contributor author | Young, G. S. | |
contributor author | Beal, R. C. | |
contributor author | Edson, J. B. | |
date accessioned | 2017-06-09T16:10:37Z | |
date available | 2017-06-09T16:10:37Z | |
date copyright | 1995/12/01 | |
date issued | 1995 | |
identifier issn | 0027-0644 | |
identifier other | ams-62653.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4203569 | |
description abstract | Two distinct backscatter regimes are seen on a European remote sensing satellite ERS-1 C-band (5.6 cm) synthetic aperture radar (SAR) image of the sea surface during a time of fair synoptic-scale weather conditions. One backscatter regime is mottled. In contrast to that, the second backscatter regime is marbled. The authors hypothesize that the mottled backscatter pattern is a characteristic SAR backscatter pattern linked to the presence of the convective (i.e., statically unstable/convective-eddy containing) marine atmospheric boundary layer (CMABL) and can be used to help determine CMABL structure [convective-eddy type (cellular convection versus longitudinal rolls), eddy wavelength, and CMABL depth (via mixed-layer similarity theory for aspect ratio)]. The hypothesis linking the presence and structure of the CMABL to the mottled backscatter pattern on SAR imagery is validated by analyzing data from a number of sources gathered in the vicinity of the boundary between the mottled and marbled regimes on the SAR image. | |
publisher | American Meteorological Society | |
title | Use of Spaceborne Synthetic Aperture Radar Imagery of the Sea Surface in Detecting the Presence and Structure of the Convective Marine Atmospheric Boundary Layer | |
type | Journal Paper | |
journal volume | 123 | |
journal issue | 12 | |
journal title | Monthly Weather Review | |
identifier doi | 10.1175/1520-0493(1995)123<3623:UOSSAR>2.0.CO;2 | |
journal fristpage | 3623 | |
journal lastpage | 3632 | |
tree | Monthly Weather Review:;1995:;volume( 123 ):;issue: 012 | |
contenttype | Fulltext | |