Philip Marsh

TL;DR: In this paper, the authors studied the effect of climate change on the water balance in the arctic and subarctic regions of North America and found that precipitation changes will play an important role in precipitation changes associated with climate warming.

TL;DR: In this paper, the authors showed that when the wetting front reached premelt stratigraphic horizons, water ponded at the interface and then flow fingers developed and penetrated the lower stratum.

TL;DR: In this paper, the authors used a Landsat-derived vegetation classification and a digital elevation model to divide the basin into snow sources and sinks, and then relocates snow from sources to sinks and calculates intransit sublimation loss.

TL;DR: In this paper, the authors show that over the past several decades, geomorphic processes in the Arctic have been changing or intensifying due to global warming and that lakes, ponds, and wetlands appear to be more dynamic, growing in some areas, shrinking in others, and changing distribution across lowland regions.

TL;DR: The first direct measurements of evaporation from a large high-latitude lake, Great Slave Lake, Northwest Territories, Canada, were made using eddy covariance between July 24 and September 10, 1997, and June 22 and September 26, 1998 as mentioned in this paper.