Isotopic signals ( 18 O, 2 H, 3 H) of six major rivers draining the pan-Arctic watershed
À6 g/km 2 per year) are found to be positively correlated with permafrost coverage within the studied drainage basins. Isotope-discharge relationships demonstrate both linear and nonlinear response patterns, which highlights the complexity of hydrological processes in large Arctic river basins. Thes...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.1048.4027 2023-05-15T14:35:27+02:00 Isotopic signals ( 18 O, 2 H, 3 H) of six major rivers draining the pan-Arctic watershed Y Yi J J Gibson L W Cooper J.-F Hélie S J Birks J W Mcclelland R M Holmes B J Peterson The Pennsylvania State University CiteSeerX Archives 2012 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1048.4027 http://www.science.uwaterloo.ca/%7Ejjgibson/mypdfs/gbc1850.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1048.4027 http://www.science.uwaterloo.ca/%7Ejjgibson/mypdfs/gbc1850.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.science.uwaterloo.ca/%7Ejjgibson/mypdfs/gbc1850.pdf text 2012 ftciteseerx 2020-04-05T00:22:58Z À6 g/km 2 per year) are found to be positively correlated with permafrost coverage within the studied drainage basins. Isotope-discharge relationships demonstrate both linear and nonlinear response patterns, which highlights the complexity of hydrological processes in large Arctic river basins. These isotope observations and their relationship to discharge and landscape features indicate that basin-specific characteristics significantly influence hydrological processes in the pan-Arctic watershed. Text Arctic permafrost Unknown Arctic |
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Open Polar |
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Unknown |
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ftciteseerx |
language |
English |
description |
À6 g/km 2 per year) are found to be positively correlated with permafrost coverage within the studied drainage basins. Isotope-discharge relationships demonstrate both linear and nonlinear response patterns, which highlights the complexity of hydrological processes in large Arctic river basins. These isotope observations and their relationship to discharge and landscape features indicate that basin-specific characteristics significantly influence hydrological processes in the pan-Arctic watershed. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Y Yi J J Gibson L W Cooper J.-F Hélie S J Birks J W Mcclelland R M Holmes B J Peterson |
spellingShingle |
Y Yi J J Gibson L W Cooper J.-F Hélie S J Birks J W Mcclelland R M Holmes B J Peterson Isotopic signals ( 18 O, 2 H, 3 H) of six major rivers draining the pan-Arctic watershed |
author_facet |
Y Yi J J Gibson L W Cooper J.-F Hélie S J Birks J W Mcclelland R M Holmes B J Peterson |
author_sort |
Y Yi |
title |
Isotopic signals ( 18 O, 2 H, 3 H) of six major rivers draining the pan-Arctic watershed |
title_short |
Isotopic signals ( 18 O, 2 H, 3 H) of six major rivers draining the pan-Arctic watershed |
title_full |
Isotopic signals ( 18 O, 2 H, 3 H) of six major rivers draining the pan-Arctic watershed |
title_fullStr |
Isotopic signals ( 18 O, 2 H, 3 H) of six major rivers draining the pan-Arctic watershed |
title_full_unstemmed |
Isotopic signals ( 18 O, 2 H, 3 H) of six major rivers draining the pan-Arctic watershed |
title_sort |
isotopic signals ( 18 o, 2 h, 3 h) of six major rivers draining the pan-arctic watershed |
publishDate |
2012 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1048.4027 http://www.science.uwaterloo.ca/%7Ejjgibson/mypdfs/gbc1850.pdf |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic permafrost |
genre_facet |
Arctic permafrost |
op_source |
http://www.science.uwaterloo.ca/%7Ejjgibson/mypdfs/gbc1850.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1048.4027 http://www.science.uwaterloo.ca/%7Ejjgibson/mypdfs/gbc1850.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766308274723880960 |