Abstract
The melt extent, duration and melt season on the Greenland ice sheet were estimated using an edge detection technique on passive microwave data from the SSM/I and SMMR instruments (18/19V GHz channel) for the period 1979 to 1997. The annual brightness temperature (Tb) time series at a pixel location that experiences summer melt has a steep rise and drop in Tb with the onset and end of melt, respectively. A derivative‐of‐Gaussian edge detector is used to detect edges corresponding to the onset and end of melt. The time lapsed between the first upward and last downward edge on the annual Tb time series gives an estimate of the melt season and the time lapsed between successive upward and downward edges gives the duration of melt. While the maximum melt extent increased by 18%, the total duration of melt increased by 3.7% and the total melt season decreased by 3.8% during the period 1979–1997.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
