Zobrazeno 1 - 7
of 7
pro vyhledávání: '"M. E. Shokr"'
Publikováno v:
The Cryosphere, Vol 14, Pp 3611-3627 (2020)
The Robeson Channel is a narrow sea water passage between Greenland and Ellesmere Island in the Arctic. It is a pathway of sea ice from the central Arctic and out to Baffin Bay. In this study, we used a set of daily synthetic aperture radar (SAR) ima
Externí odkaz:
https://doaj.org/article/e389b828aafc4251bed6b8b3d76ccdd9
Publikováno v:
Canadian Journal of Remote Sensing. 25:70-79
Un algorithme interactif a ete developpe dans le contexte de l'analyse operationnelle des images satellite ROS pour le suivi des glaces. L'intrant a l'algorithme est une estimation subjective des types de glace dans une zone donnee de l'image et le p
Autor:
M. E. Shokr, Robert Moucha
Publikováno v:
International Journal of Remote Sensing. 19:855-869
Quantitative integration of remote sensing data requires accurate co-location of pixels between data from different sensors. A technique has been developed, based on a simple spherical Earth model, to map ground resolution cells pertaining to pixel/g
Publikováno v:
International Journal of Remote Sensing. 17:667-682
ERS-1 SAR images have been used to monitor sea ice in the Canadian east coast and the Gulf of St. Lawrence since December 1992. Operational ice parameters were obtained, in near real-time, through visual image analysis. The information was incorporat
Publikováno v:
International Journal of Remote Sensing. 16:3343-3363
In this work we examine the seasonal co-evolution of: the microwave scattering coefficient (σ°) as observed with ERS-l; the radiative components of the surface energy balance; and the physical and electrical properties of the snow/ sea-ice system.
Autor:
Moucha, M. E. Shokr R.
Publikováno v:
International Journal of Remote Sensing; 3/20/98, Vol. 19 Issue 5, p855-869, 15p
Publikováno v:
Boundary-Layer Meteorology. 40:1-29
Wind-tunnel simulations of neutrally-stable atmospheric boundary-layer flow over an isolated, low hill (Askervein) have been carried out at three different length scales in two wind-tunnel facilities. The objectives of these simulations were to asses