Projects per year
measurements made by Sentinel-2 (S-2) and MODIS. S-2 observations provide a highly conservative estimate of algal bloom presence because algal blooms occur in patches much smaller than the ground resolution of S-2 data. Nevertheless, the bare ice albedo distribution at the scale of 20×20 m S-2 pixels is generally unimodal and unskewed. Conversely, bare ice surfaces have a left-skewed albedo distribution at MODIS MOD10A1 scales. Thus, when MOD10A1 observations are used as input to energy balance modelling then meltwater production can be under-estimated by ∼2%. Our study highlights that (1) the impact of weathering crust state is of similar importance to the direct darkening role of light-absorbing impurities upon ice albedo and (2) there is a spatial scale dependency in albedo measurement which reduces detection of real changes at coarser resolutions.
FingerprintDive into the research topics of 'Algal growth and weathering crust state drive variability in western Greenland Ice Sheet ice albedo'. Together they form a unique fingerprint.
- 2 Active
Bates, P. D., Bingham, R. J., Chuter, S. J., Hofer, S., Llovell, W., Martin Espanol, A., Rougier, J. C., Schumacher, M., Sha, Z., Westaway, R. M., Royston, S. J., Vishwakarma, B. D., Bamber, J. L., Brady, A., Ziegler, Y., Abele, A. K. & Lehmann, F.
1/08/16 → 31/07/22
1/07/15 → 30/09/21