1 to 10 of 10 Results
Jul 6, 1998
Joughin, I.; Fahnestock, M.; Thomas, B.; Kwok, R., 1998, "Ice Flow in Northeast Greenland Derived Using Balance Velocities as Control", https://hdl.handle.net/2014/19255, ['IGARSS', 'Seattle, Washington, USA'], JPL Open Repository
Satellite radar interferometry provides an important new means for measuring ice motion. |
Jan 1, 1998
Joughin, I.; Fahnestock, M.; Kwok, R.; Gogineni, P.; Allen, C., 1998, "Ice Flow in the Humboldt, Petermann, and Ryder Glaciers, North Greenland", https://hdl.handle.net/2014/18934, ['Journal of Glaciology', 'USA'], JPL Open Repository
Radar Interferometry, ice-penetrating radar profiles, and an elevation model are used to determine the catchment area, rates of ice discharge, and approximate states of balance for three large outlet glaciers in northeast Greenland. |
Mar 17, 1997
Joughin, I.; Kwok, R.; Fahnestock, M.; Winebrenner, D.; Tulaczyk, S.; Gogenini, P., 1997, "Interferometric Estimation of Ice Sheet Motion and Topography", https://hdl.handle.net/2014/21907, Florence, Italy, JPL Open Repository
With ERS-1/2 satellite radar interferometry, it is now possible to make measurements of glacier motion with high accuracy and fine spatial resolution. |
Dec 15, 1996
Joughin, I.; Tulaczyk, Slawek; Fahnestock, M.; Kwok, R., 1996, "(abstract) A Mini-Surge on the Ryder Glacier, Greenland", https://hdl.handle.net/2014/26514, SAn Francisco, CA, JPL Open Repository
We have detected a dramatic short-term speedup of the Ryder Glacier, Greenland, using satellite radar interferometry. The accelerated flow represents a substantial, though short-lived, change in the ice discharge from the basin. We use the term |
Dec 15, 1996
Joughin, I.; Kwok, R.; Fahnestock, M., 1996, "(abstract) Three Dimensional Ice-Flow Velocity Estimation Using Satellite Radar Interferometry", https://hdl.handle.net/2014/26513, San Francisco, CA, JPL Open Repository
An understanding of the flow dynamics of an ice sheet's outlet glaciers and ice streams requires knowledge of their flow velocity and strain rates (i.e., velocity gradients). Prior to the recent advent of satellite radar interferometry, it was not possible to measure detailed ice... |
Jan 1, 1996
Joughin, I.; Tulaczyk, S.; Fahnestock, M.; Kwok, R., 1996, "A Mini-Surge on theRyder Glacier, Greenland Observed via Satelite Radar Interferometry", https://hdl.handle.net/2014/26051, UNKNOWN, JPL Open Repository
A dramatic short term speed up of the Ryder glacier has been detected using satellite radar interferometry. The accelerated flow represents a substantial, though short-lived, change in the ice discharge from this basin. We believe that meltwater was involved in this event, either... |
Jan 1, 1996
Joughin, I.; Kwok, R.; Fahnestock, M., 1996, "Interferometric Estimation of theThree-Dimensional Ice-Flow Velocity Vector Using Ascending and Descending Passes", https://hdl.handle.net/2014/27656, UNKNOWN, JPL Open Repository
Satellite radar interferometry provides an importatn new tool for determining ice-flow velocity. Interferometric measurements made from a single track direction are sensitive only to a single component of the three-dimensional velocity vector. Observations from along thre differe... |
Jul 10, 1995
Kwok, R.; Fahnestock, M., 1995, "ERS-1 Radar Interferometry Over an Ice Stream in Northeast Greenland", https://hdl.handle.net/2014/33390, Florence, Italy, JPL Open Repository
No abstract provided |
Dec 5, 1994
Kwok, R.; Fahnestock, M., 1994, "Determination of Ice Sheet Motion and Topography Using Radar Interferometry", https://hdl.handle.net/2014/33277, San Francisco, California, USA, JPL Open Repository
No abstract provided |
Sep 22, 1994
Kwok, R.; Fahnestock, M.; Chan, C., 1994, "Ice Sheet Motion and Topography from Radar Interferometry", https://hdl.handle.net/2014/33538, IEEE Trans on Geoscience and Remote Sensing, JPL Open Repository
Both topography and motion information are present in repeat pass ERS-1 interferograms over ice sheets. |