Three different methods for deriving elevation changes from the ICESat altimetry dataset are used. This multi-method approach provides a method to assess the complexity of deriving elevation changes from this dataset. The altimetry alone can not provide an estimate of the mass balance of the Greenland ice sheet. Firn dynamics and surface densities are important factors that contribute to the mass change derived from remote-sensing altimetry. The volume change derived from ICESat data is corrected for changes in firn compaction over the observation period, vertical bedrock movement and an intercampaign elevation bias in the ICESat data. Subsequently, the corrected volume change is converted into mass change by the application of a simple...
The Greenland ice sheet is sensitive to climate change. Global heating is expected to result in ice ...
We estimate ice volume change rates in the northwest Greenland drainage basin during 2003–2009 using...
Estimating the contribution of ice sheets to sea level change is a major goal of glaciologists and o...
Three different methods for deriving elevation changes from the ICESat altimetry dataset are used. T...
Three different methods for deriving elevation changes from the ICESat altimetry dataset are used. T...
Three different methods for deriving elevation changes from the ICESat altimetry dataset are used. T...
Three different methods for deriving elevation changes from the ICESat altimetry dataset are used. T...
Three different methods for deriving elevation changes from the ICESat altimetry dataset are used. T...
Three different methods for deriving elevation changes from the ICESat altimetry dataset are used. T...
Observed changes in the surface elevation of the Greenland Ice Sheet are caused by ice dynamics, bas...
Mass changes of the Greenland Ice Sheet may be estimated by the input-output method (IOM), satellite...
Mass changes of the Greenland Ice Sheet may be estimated by the input-output method (IOM), satellite...
The focus of this paper is on the quantification of ongoing mass and volume changes over the Greenla...
Observed changes in the surface elevation of the Greenland Ice Sheet are caused by ice dynamics, bas...
Mass changes of the Greenland ice sheet may be estimated by the Input Output Method (IOM), satellite...
The Greenland ice sheet is sensitive to climate change. Global heating is expected to result in ice ...
We estimate ice volume change rates in the northwest Greenland drainage basin during 2003–2009 using...
Estimating the contribution of ice sheets to sea level change is a major goal of glaciologists and o...
Three different methods for deriving elevation changes from the ICESat altimetry dataset are used. T...
Three different methods for deriving elevation changes from the ICESat altimetry dataset are used. T...
Three different methods for deriving elevation changes from the ICESat altimetry dataset are used. T...
Three different methods for deriving elevation changes from the ICESat altimetry dataset are used. T...
Three different methods for deriving elevation changes from the ICESat altimetry dataset are used. T...
Three different methods for deriving elevation changes from the ICESat altimetry dataset are used. T...
Observed changes in the surface elevation of the Greenland Ice Sheet are caused by ice dynamics, bas...
Mass changes of the Greenland Ice Sheet may be estimated by the input-output method (IOM), satellite...
Mass changes of the Greenland Ice Sheet may be estimated by the input-output method (IOM), satellite...
The focus of this paper is on the quantification of ongoing mass and volume changes over the Greenla...
Observed changes in the surface elevation of the Greenland Ice Sheet are caused by ice dynamics, bas...
Mass changes of the Greenland ice sheet may be estimated by the Input Output Method (IOM), satellite...
The Greenland ice sheet is sensitive to climate change. Global heating is expected to result in ice ...
We estimate ice volume change rates in the northwest Greenland drainage basin during 2003–2009 using...
Estimating the contribution of ice sheets to sea level change is a major goal of glaciologists and o...