O'Neal, Michael A.This thesis evaluates spatial errors, inherent to image-based analysis, that affect our ability to detect areal changes in glaciers. Analysis of areal differences of 742 North Cascade glaciers, observed in A.D. 1958 and A.D. 2006 inventories, suggests change detection is limited by linear errors of 5 m, 7 m, and 184 m caused by the imagery, digitization operators, and snowpack variability, respectively. Using the cumulative error of 196 m as a threshold for detecting areal change over the 48-year period, only 250 glaciers were detectable outside of the error threshold. Of those detectable changes, 240 glaciers were decreasing in area and 10 were increasing in area. Coupling the A.D. 2006 inventory with a contemporary 15 m ...
The Randolph Glacier Inventory (RGI) is a globally complete collection of digital outlines of glacie...
Abstract To chronicle the change of alpine glaciers analysis of historical data and comparison with ...
ABSTRACT. An analysis of the local topographic setting of very small (<0.4 km 2) glaciers within ...
Since the mid-19th century, most glaciers have been losing area and volume. This loss of area has no...
The spatial characteristics for all glaciers in the North Cascades National Park Complex, USA, were ...
ABSTRACT. Benchmark glaciers were established in many alpine areas during the 1960s as part of the I...
ABSTRACT. Net changes in glacier area in the region 50–518N, 116–1258W, which includes the Columbia ...
Most glaciers and ice caps (GIC) are out of balance with the current climate. To return to equilibri...
ABSTRACT. Net changes in glacier area in the region 50–518N, 116–1258W, which includes the Columbia ...
Glacier inventories provide the baseline data to perform climate-change impact assessment on a regio...
This paper aims to evaluate sources of uncertainty and variability associated with rock glacier inve...
Benchmark glaciers were established in many alpine areas during the 1960s as part of the Internation...
1998 the glacier area had decreased to 109.11.1 km2, a reduction of 8.20.1 km2 (7%). Estimated volum...
© 2017 Swedish Society for Anthropology and Geography. To estimate hydrological storage and better u...
The paper compares the results of two alternative methods for studying glacier variations in Mt. Nai...
The Randolph Glacier Inventory (RGI) is a globally complete collection of digital outlines of glacie...
Abstract To chronicle the change of alpine glaciers analysis of historical data and comparison with ...
ABSTRACT. An analysis of the local topographic setting of very small (<0.4 km 2) glaciers within ...
Since the mid-19th century, most glaciers have been losing area and volume. This loss of area has no...
The spatial characteristics for all glaciers in the North Cascades National Park Complex, USA, were ...
ABSTRACT. Benchmark glaciers were established in many alpine areas during the 1960s as part of the I...
ABSTRACT. Net changes in glacier area in the region 50–518N, 116–1258W, which includes the Columbia ...
Most glaciers and ice caps (GIC) are out of balance with the current climate. To return to equilibri...
ABSTRACT. Net changes in glacier area in the region 50–518N, 116–1258W, which includes the Columbia ...
Glacier inventories provide the baseline data to perform climate-change impact assessment on a regio...
This paper aims to evaluate sources of uncertainty and variability associated with rock glacier inve...
Benchmark glaciers were established in many alpine areas during the 1960s as part of the Internation...
1998 the glacier area had decreased to 109.11.1 km2, a reduction of 8.20.1 km2 (7%). Estimated volum...
© 2017 Swedish Society for Anthropology and Geography. To estimate hydrological storage and better u...
The paper compares the results of two alternative methods for studying glacier variations in Mt. Nai...
The Randolph Glacier Inventory (RGI) is a globally complete collection of digital outlines of glacie...
Abstract To chronicle the change of alpine glaciers analysis of historical data and comparison with ...
ABSTRACT. An analysis of the local topographic setting of very small (<0.4 km 2) glaciers within ...