Watershed slope as a predictor of fluvial dissolved organic matter and nitrate concentrations across geographical space and catchment size in the Arctic
Watershed slope as a predictor of fluvial dissolved organic matter and nitrate concentrations across geographical space and catchment size in the Arctic
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DOI:
10.1088/1748-9326/aae35d
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发表时间:
2018-10
影响因子:
6.7
通讯作者:
C. Connolly;M. Khosh;G. Burkart;T. Douglas;R. Holmes;A. Jacobson;S. Tank;J. McClelland
中科院分区:
文献类型:
--
作者:
C. Connolly;M. Khosh;G. Burkart;T. Douglas;R. Holmes;A. Jacobson;S. Tank;J. McClelland
Understanding linkages between river chemistry and biological production in arctic coastal waters requires improved estimates of riverine nutrient export. Here we present the results of a synthesis effort focusing on relationships between watershed slope and seasonal concentrations of river-borne dissolved organic carbon (DOC), dissolved organic nitrogen (DON), and nitrate ( NO 3 − ) around the pan-Arctic. Strong negative relationships exist between watershed slope and concentrations of DOC and DON in arctic rivers. Spring and summer concentration-slope relationships for DOC and DON are qualitatively similar, although spring concentrations are higher. Relationships for NO 3 − are more variable, but a significant positive relationship exists between summer NO 3 − concentrations and watershed slopes. These results suggest that watershed slope can serve as a master variable for estimating spring and summer DOC and DON concentrations, and to a lesser degree NO 3 − , from drainage areas where field data are lacking, thus improving our ability to develop pan-arctic estimates of watershed nutrient export.