Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Kyung-Kuk Kang"'
Publikováno v:
IEEE Transactions on Geoscience and Remote Sensing. 55:5956-5965
Observations of ice thickness are limited in high latitude regions, at a time when they are increasingly being requested by operational ice centers. This study aims to improve the retrieval of lake ice thickness using data from the Moderate Resolutio
Autor:
Kevin Kyung-Kuk Kang, M. Foroutan, Marie Hoekstra, Kiana Zolfaghari, Amir M. Chegoonian, Claude R. Duguay
Publikováno v:
IGARSS
This work describes a pilot study in southern Ontario, Canada evaluating the use of the ‘Headwall Nano-Hyperspec’ hyperspectral imager onboard a Remotely Piloted Aircraft System (RPAS). Hyperspectral imagers are extremely useful for monitoring ve
Publikováno v:
The Cryosphere, Vol 10, Iss 2, Pp 569-584 (2016)
The aim of this study was to develop an approach for estimating ice break-up dates on the Mackenzie River (MR) using more than a decade of MODIS Level 3 500 m snow products (MOD/MYD10A1), complemented with 250 m Level 1B radiance products (MOD/MYD02Q
Publikováno v:
Remote Sensing of Environment. 150:1-19
An ice thickness retrieval algorithm utilizing data from the Advanced Microwave Scanning Radiometer-Earth Observing System (AMSR-E) was developed and applied to Great Bear Lake (GBL) and Great Slave Lake (GSL), Northwest Territories, Canada, for the
Publikováno v:
The Cryosphere, Vol 6, Iss 2, Pp 235-254 (2012)
Time series of brightness temperatures (TB) from the Advanced Microwave Scanning Radiometer–Earth Observing System (AMSR-E) are examined to determine ice phenology variables on the two largest lakes of northern Canada: Great Bear Lake (GBL) and Gre
Publikováno v:
IEEE Geoscience and Remote Sensing Letters. 7:751-755
The sensitivity of brightness temperature (TB) at 6.9, 10.7, and 18.7 GHz from Advanced Microwave Scanning Radiometer-Earth Observing System (AMSR-E) observations is investigated over five winter seasons (2002-2007) on Great Bear Lake and Great Slave
Publikováno v:
Remote Sensing of Environment. 113:816-834
The temporal evolution of the backscatter coefficient, sigma-nought (σ°) from QuikSCAT was evaluated for monitoring ice phenology on Great Bear Lake (66°N, 121°W) and Great Slave Lake (61°40′N, 114°W), Northwest Territories, Canada. Results i