On detection of the thermophysical state of landfast first-year sea ice using in-situ microwave emission during spring melt

被引:6
|
作者
Hwang, Byong Jun [1 ]
Langlols, Alexandre [1 ]
Barber, David G. [1 ]
Papakyriakou, Timothy N. [1 ]
机构
[1] Univ Manitoba, Ctr Earth Observ Sci, Clayton H Riddell Fac Earth Environm & Resources, Dept Environm & Geog, Winnipeg, MB R3T 2N2, Canada
基金
加拿大自然科学与工程研究理事会;
关键词
spring melt; sea ice; snow; thermophysical; melt onset; SSM/I; microwave emission;
D O I
10.1016/j.rse.2007.02.033
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
In this study we examine the critical linkages between thermophysical properties and microwave emissions of landfast snow-covered first-year sea ice during spring melt. For this we analyzed the temporal evolution of radiation fluxes, electro-thermophysical properties and microwave emissions, and perform model simulations to evaluate the observations. The results show five major microwave signature events: brine-rich, blowing snow, melt onset, the onset of funicular regime, and freezing. A brine-rich snow basal layer can considerably increase the snow wetness in the upper and mid layers, resulting in a significant increase in complex permittivity that in turn increases in polarization difference (delta p) at 19 and 37 GHz. A dense (similar to 0.40 g cm(-3)) wind-packed snow surface layer, during a blowing snow event, was found to increase the permittivity (i.e., surface reflectivity) that in turn increases delta p in microwave emissions. Melt onset caused by sustained warming (above -5 degrees C) corresponded to increased delta p of similar to 9 K at 19 GHz. The most dramatic increase in delta p (up to 17 K at 19 GHz) coincided with the occurrence of a rainstorm. During a freezing, melt-freeze events enlarged snow grains and led to formation of ice lenses and layers within the snow, thereby significantly decreasing microwave emissions. We found that these five factors state above were critical to the melt indicators (i.e., Delta T-B(H) (T-B(19H)-T-B(37H)) and XPGR ([T-B(19H)-T-B(37V)]/[T-B(19H)+T-B(37V)])) commonly used in the satellite melt detection algorithms. The results suggests that the absolute value of TB(19H) (brightness temperature of horizontal polarization at 19 GHz) would be a good indicator along with Delta T-B(H) (or XPGR) to delineate the melt onset from ambiguous factors (i.e., a brine-rich slush layer or wind-packed layer), and that the funicular stage of snow melt on sea ice could be unambiguously detected by either Delta T-B(H) or XPGR. (c) 2007 Elsevier Inc. All rights reserved.
引用
收藏
页码:148 / 159
页数:12
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