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Open AccessArticle

Characterizing Post-Drainage Succession in Thermokarst Lake Basins on the Seward Peninsula, Alaska with TerraSAR-X Backscatter and Landsat-based NDVI Data

1
Geophysical Institute, University of Alaska Fairbanks, Fairbanks, AK 99775, USA
2
Eastern Geology and Paleoclimate Center, US Geological Survey, Reston, VA 20192, USA
3
Water and Environmental Research Center, University of Alaska, Fairbanks, AK 99775, USA
4
Alaska Science Center, US Geological Survey, Anchorage, AK 99508, USA
*
Author to whom correspondence should be addressed.
Remote Sens. 2012, 4(12), 3741-3765; https://doi.org/10.3390/rs4123741
Received: 15 September 2012 / Revised: 10 November 2012 / Accepted: 16 November 2012 / Published: 27 November 2012
Drained thermokarst lake basins accumulate significant amounts of soil organic carbon in the form of peat, which is of interest to understanding carbon cycling and climate change feedbacks associated with thermokarst in the Arctic. Remote sensing is a tool useful for understanding temporal and spatial dynamics of drained basins. In this study, we tested the application of high-resolution X-band Synthetic Aperture Radar (SAR) data of the German TerraSAR-X satellite from the 2009 growing season (July–September) for characterizing drained thermokarst lake basins of various age in the ice-rich permafrost region of the northern Seward Peninsula, Alaska. To enhance interpretation of patterns identified in X-band SAR for these basins, we also analyzed the Normalized Difference Vegetation Index (NDVI) calculated from a Landsat-5 Thematic Mapper image acquired on July 2009 and compared both X-band SAR and NDVI data with observations of basin age. We found significant logarithmic relationships between (a) TerraSAR-X backscatter and basin age from 0 to 10,000 years, (b) Landat-5 TM NDVI and basin age from 0 to 10,000 years, and (c) TerraSAR-X backscatter and basin age from 50 to 10,000 years. NDVI was a better indicator of basin age over a period of 0–10,000 years. However, TerraSAR-X data performed much better for discriminating radiocarbon-dated basins (50–10,000 years old). No clear relationships were found for either backscatter or NDVI and basin age from 0 to 50 years. We attribute the decreasing trend of backscatter and NDVI with increasing basin age to post-drainage changes in the basin surface. Such changes include succession in vegetation, soils, hydrology, and renewed permafrost aggradation, ground ice accumulation and localized frost heave. Results of this study show the potential application of X-band SAR data in combination with NDVI data to map long-term succession dynamics of drained thermokarst lake basins. View Full-Text
Keywords: thermokarst lake; drained thermokarst lake basin; X-band SAR; arctic peatland succession; permafrost; land surface age determination thermokarst lake; drained thermokarst lake basin; X-band SAR; arctic peatland succession; permafrost; land surface age determination
MDPI and ACS Style

Regmi, P.; Grosse, G.; Jones, M.C.; Jones, B.M.; Anthony, K.W. Characterizing Post-Drainage Succession in Thermokarst Lake Basins on the Seward Peninsula, Alaska with TerraSAR-X Backscatter and Landsat-based NDVI Data. Remote Sens. 2012, 4, 3741-3765.

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