New research is finding that satellite-based radar remote sensing techniques are particularly well-suited for quantifying the transition of remote boreal regions from a frozen to a thawed condition. The implications for studying global warming are far reaching. If the timing or areal extent of this freeze/thaw transition were to change significantly, measurable changes in boreal climate, hydrology, and biogeochemistry would result. Abrupt transition from frozen to thawed conditions occurs each year over roughly 50 million km2of the Earth\u27s remote terrestrial surface at latitudes above 40°N. Radar remote sensing works well to capture this transition because of the way electromagnetic radiation at radar wavelengths interacts with polar wat...
The seasonal transition of the land surface between frozen and nonfrozen conditions affects a number...
Large fractions (15-40%) of the arctic and subarctic land surface are covered by lakes and rivers, e...
The seasonal transition of the land surface between frozen and nonfrozen conditions affects a number...
New research is finding that satellite-based radar remote sensing techniques are particularly well-s...
Monitoring freeze-thaw cycles of high latitude terrestrial ecosystems is useful for estimating the l...
The seasonal transition of the boreal forest between frozen and non-frozen conditions affects a numb...
The transition of the landscape between predominantly frozen and nonfrozen conditions in seasonally ...
We hypothesize that the strong sensitivity of radar backscatter to surface dielectric properties, an...
Spatial and temporal variability in landscape freeze- thaw (FT) status at higher latitudes and eleva...
In the terrestrial cryosphere, freeze/thaw (FT) state transitions play an important and measurable r...
The annual freeze/thaw (FT) cycle determines the potential growing season in boreal landscapes and i...
Springtime snowmelt is a major hydrological event across the pan-Arctic. Melt is typically simulated...
This study investigates the use of remote sensing for monitoring ice phenology and ice characteristi...
We evaluated whether satellite radar remote sensing of landscape seasonal freeze–thaw cycles provide...
The seasonal transition of the land surface between fro- spring were also generally consistent with ...
The seasonal transition of the land surface between frozen and nonfrozen conditions affects a number...
Large fractions (15-40%) of the arctic and subarctic land surface are covered by lakes and rivers, e...
The seasonal transition of the land surface between frozen and nonfrozen conditions affects a number...
New research is finding that satellite-based radar remote sensing techniques are particularly well-s...
Monitoring freeze-thaw cycles of high latitude terrestrial ecosystems is useful for estimating the l...
The seasonal transition of the boreal forest between frozen and non-frozen conditions affects a numb...
The transition of the landscape between predominantly frozen and nonfrozen conditions in seasonally ...
We hypothesize that the strong sensitivity of radar backscatter to surface dielectric properties, an...
Spatial and temporal variability in landscape freeze- thaw (FT) status at higher latitudes and eleva...
In the terrestrial cryosphere, freeze/thaw (FT) state transitions play an important and measurable r...
The annual freeze/thaw (FT) cycle determines the potential growing season in boreal landscapes and i...
Springtime snowmelt is a major hydrological event across the pan-Arctic. Melt is typically simulated...
This study investigates the use of remote sensing for monitoring ice phenology and ice characteristi...
We evaluated whether satellite radar remote sensing of landscape seasonal freeze–thaw cycles provide...
The seasonal transition of the land surface between fro- spring were also generally consistent with ...
The seasonal transition of the land surface between frozen and nonfrozen conditions affects a number...
Large fractions (15-40%) of the arctic and subarctic land surface are covered by lakes and rivers, e...
The seasonal transition of the land surface between frozen and nonfrozen conditions affects a number...