Temporal and Spatial Trends in Soil Moisture in Arctic Alaska 1992-2010

Details

Meeting2014 Fall Meeting
SectionBiogeosciences
SessionRemote Sensing of Northern High-Latitude Terrestrial and Aquatic Ecosystems II
IdentifierB54F-08
Authors Jenkins, L K*, School of Natural Resources and Environment, University of Michigan Ann Arbor, Ann Arbor, MI, United States, Michigan Tech Research Institute, Michigan Technological University, Ann Arbor, MI, United States
Bourgeau-Chavez, L L, Michigan Tech Research Institute, Michigan Technological University, Ann Arbor, MI, United States
French, N H F, Michigan Tech Research Institute, Michigan Technological University, Houghton, MI, United States
Chavez, M C, Michigan Tech Research Institute, Michigan Technological University, Ann Arbor, MI, United States
Index Terms Carbon cycling [0428]
Permafrost, cryosphere, and high-latitude processes [0475]
Remote sensing [0480]
Modeling [0798]

Abstract

Previous research in the Arctic has demonstrated changes associated with a warming climate including shrub expansion northward, drying of lakes, increasing active layer depths, and decreasing ice and snow cover. With a warming climate, potential for permafrost thaw, increased evapotranspiration from shrubs, and drying lakes, there have likely been widespread changes in patterns of surface soil moisture across the Arctic landscape over the past 20 to 30 years. We investigated trends in soil moisture in Arctic Alaska using the two-decade long data record of ERS-1 and -2 synthetic aperture radar (SAR) satellite data and ground based measurements of precipitation and soil moisture. SAR data have long been known to be highly sensitive to changes in soil moisture condition, and the C-band SAR (~5.6 cm wavelength) of ERS-1 and 2 are particularly useful for monitoring moisture in the low biomass, open ecosystems of the tundra. Eight sites in Alaska, spanning low to high Arctic and coastal to interior tundra, have been used to develop methodologies and relationships between SAR backscatter and soil moisture in tundra ecosystems. Given the dearth of long-term, in-situ soil moisture data, methods have been investigated using surrogate soil moisture information derived from weather station data and the use of the Fire Weather Index (FWI) subsystem of the Canadian Forest Fire Danger Rating System. Previous SAR work in boreal regions has demonstrated high correlations between SAR backscatter at C-band and the drought code (DC) component of the FWI subsystem. DC is a measure of moisture in the deep organic soil layers of 10-20 cm. This paper will present temporal and spatial trends in soil moisture over the two-decade long observation period among the eight study sites. Differences in soil moisture mapping using SAR data between Arctic and boreal systems will be discussed. Recommendations for the use of ERS-1 and -2 data in longitudinal studies will also be highlighted given calibration and data processing issues encountered in this study.

Cite as: Author(s) (2014), Title, Abstract B54F-08 presented at 2014 Fall Meeting, AGU, San Francisco, Calif., 15-19 Dec.