�H m˙ 1n�1 z �
where t m is the model age of ice at a depth d � (H – z). 22. If the melt rate exceeds the surface accumulation rate, the thickness of an annual layer actually increases with age and depth in the ice (which is equivalent to saying that there is net convergence of flow in the horizontal plane or a sl...
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.180.2679 http://geodesy.unr.edu/publications/Blewitt_et_al_seasonalsignal_2001.pdf |
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.180.2679 2023-05-15T16:28:05+02:00 �H m˙ 1n�1 z � Ε Nye D. Dahl-jensen S. J. Johnsen C. U. Hammer The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.180.2679 http://geodesy.unr.edu/publications/Blewitt_et_al_seasonalsignal_2001.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.180.2679 http://geodesy.unr.edu/publications/Blewitt_et_al_seasonalsignal_2001.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://geodesy.unr.edu/publications/Blewitt_et_al_seasonalsignal_2001.pdf text ftciteseerx 2016-01-07T16:26:24Z where t m is the model age of ice at a depth d � (H – z). 22. If the melt rate exceeds the surface accumulation rate, the thickness of an annual layer actually increases with age and depth in the ice (which is equivalent to saying that there is net convergence of flow in the horizontal plane or a slow-down along flow in a flow-line model). This situation occurs in several areas in northeast Greenland. The thinning rate can be expressed with a thinning rate factor ƒ � ε ˙ D–J ε ˙ Nye, h � 0;ƒ � ε ˙ melt Text Greenland Unknown Greenland |
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Open Polar |
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ftciteseerx |
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English |
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where t m is the model age of ice at a depth d � (H – z). 22. If the melt rate exceeds the surface accumulation rate, the thickness of an annual layer actually increases with age and depth in the ice (which is equivalent to saying that there is net convergence of flow in the horizontal plane or a slow-down along flow in a flow-line model). This situation occurs in several areas in northeast Greenland. The thinning rate can be expressed with a thinning rate factor ƒ � ε ˙ D–J ε ˙ Nye, h � 0;ƒ � ε ˙ melt |
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The Pennsylvania State University CiteSeerX Archives |
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Text |
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Ε Nye D. Dahl-jensen S. J. Johnsen C. U. Hammer |
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Ε Nye D. Dahl-jensen S. J. Johnsen C. U. Hammer �H m˙ 1n�1 z � |
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Ε Nye D. Dahl-jensen S. J. Johnsen C. U. Hammer |
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Ε Nye |
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�H m˙ 1n�1 z � |
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�H m˙ 1n�1 z � |
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�H m˙ 1n�1 z � |
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�H m˙ 1n�1 z � |
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�H m˙ 1n�1 z � |
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�h m˙ 1n�1 z � |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.180.2679 http://geodesy.unr.edu/publications/Blewitt_et_al_seasonalsignal_2001.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.180.2679 http://geodesy.unr.edu/publications/Blewitt_et_al_seasonalsignal_2001.pdf |
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