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Title: The coastal streamflow flux in the Regional Arctic System Model

Abstract

The coastal streamflow flux from the Arctic drainage basin is an important driver of dynamics in the coupled ice-ocean system. Comprising more than one third of the total freshwater flux into the Arctic Ocean, streamflow is a key component of the regional and global freshwater cycle. To better represent the coupling of the streamflow flux to the ocean, we have developed and applied the RVIC streamflow routing model within the Regional Arctic System Model (RASM). The RASM is a high-resolution regional Earth System Model whose domain includes all of the Arctic drainage basin. Here in this paper, we introduce the RVIC streamflow routing model, detailing its application within RASM and its advancements in terms of representing high-resolution streamflow processes. We evaluate model simulated streamflow relative to in situ observations and demonstrate a method for improving model performance using a simple optimization procedure. We also present a new, spatially and temporally consistent, high-resolution data set of coastal freshwater fluxes for the Arctic drainage basin and surrounding areas that is based on a fully coupled RASM simulation and intended for use in Arctic Ocean modeling applications. This data set is evaluated relative to other coastal streamflow data sets commonly used by themore » ocean modeling community. We demonstrate that the RASM-simulated streamflow flux better represents the annual cycle than existing data sets, especially in ungauged areas. Finally, we assess the impact that streamflow has on the coupled ice-ocean system, finding that the presence of streamflow leads to reduced sea surface salinity, increased sea surface temperatures, and decreased sea ice thickness.« less

Authors:
ORCiD logo [1]; ORCiD logo [2]; ORCiD logo [3];  [3]; ORCiD logo [3]; ORCiD logo [4]
  1. Univ. of Washington, Seattle, WA (United States). Dept. of Civil and Environmental Engineering; National Center for Atmospheric Research, Boulder, CO (United States)
  2. Univ. of Washington, Seattle, WA (United States). Dept. of Civil and Environmental Engineering
  3. Naval Postgraduate School, Monterey, CA (United States). Dept. of Oceanography
  4. Polish Inst. of Oceanology, Sopot (Poland)
Publication Date:
Research Org.:
Univ. of Washington, Seattle, WA (United States); Naval Postgraduate School, Monterey, CA (United States)
Sponsoring Org.:
USDOE Office of Science (SC)
OSTI Identifier:
1466299
Alternate Identifier(s):
OSTI ID: 1374924
Grant/Contract Number:  
FG02-07ER64460; SC0006856; SC0005783; SC0005522
Resource Type:
Accepted Manuscript
Journal Name:
Journal of Geophysical Research. Oceans
Additional Journal Information:
Journal Volume: 122; Journal Issue: 3; Journal ID: ISSN 2169-9275
Publisher:
American Geophysical Union
Country of Publication:
United States
Language:
English
Subject:
54 ENVIRONMENTAL SCIENCES; Arctic; climate; hydrology; streamflow; runoff; streamflow routing

Citation Formats

Hamman, Joseph, Nijssen, Bart, Roberts, Andrew, Craig, Anthony, Maslowski, Wieslaw, and Osinski, Robert. The coastal streamflow flux in the Regional Arctic System Model. United States: N. p., 2017. Web. doi:10.1002/2016JC012323.
Hamman, Joseph, Nijssen, Bart, Roberts, Andrew, Craig, Anthony, Maslowski, Wieslaw, & Osinski, Robert. The coastal streamflow flux in the Regional Arctic System Model. United States. https://doi.org/10.1002/2016JC012323
Hamman, Joseph, Nijssen, Bart, Roberts, Andrew, Craig, Anthony, Maslowski, Wieslaw, and Osinski, Robert. Fri . "The coastal streamflow flux in the Regional Arctic System Model". United States. https://doi.org/10.1002/2016JC012323. https://www.osti.gov/servlets/purl/1466299.
@article{osti_1466299,
title = {The coastal streamflow flux in the Regional Arctic System Model},
author = {Hamman, Joseph and Nijssen, Bart and Roberts, Andrew and Craig, Anthony and Maslowski, Wieslaw and Osinski, Robert},
abstractNote = {The coastal streamflow flux from the Arctic drainage basin is an important driver of dynamics in the coupled ice-ocean system. Comprising more than one third of the total freshwater flux into the Arctic Ocean, streamflow is a key component of the regional and global freshwater cycle. To better represent the coupling of the streamflow flux to the ocean, we have developed and applied the RVIC streamflow routing model within the Regional Arctic System Model (RASM). The RASM is a high-resolution regional Earth System Model whose domain includes all of the Arctic drainage basin. Here in this paper, we introduce the RVIC streamflow routing model, detailing its application within RASM and its advancements in terms of representing high-resolution streamflow processes. We evaluate model simulated streamflow relative to in situ observations and demonstrate a method for improving model performance using a simple optimization procedure. We also present a new, spatially and temporally consistent, high-resolution data set of coastal freshwater fluxes for the Arctic drainage basin and surrounding areas that is based on a fully coupled RASM simulation and intended for use in Arctic Ocean modeling applications. This data set is evaluated relative to other coastal streamflow data sets commonly used by the ocean modeling community. We demonstrate that the RASM-simulated streamflow flux better represents the annual cycle than existing data sets, especially in ungauged areas. Finally, we assess the impact that streamflow has on the coupled ice-ocean system, finding that the presence of streamflow leads to reduced sea surface salinity, increased sea surface temperatures, and decreased sea ice thickness.},
doi = {10.1002/2016JC012323},
journal = {Journal of Geophysical Research. Oceans},
number = 3,
volume = 122,
place = {United States},
year = {Fri Feb 03 00:00:00 EST 2017},
month = {Fri Feb 03 00:00:00 EST 2017}
}

Journal Article:
Free Publicly Available Full Text
Publisher's Version of Record

Citation Metrics:
Cited by: 23 works
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Figures / Tables:

Figure 1 Figure 1: Coupling schematic for the Regional Arctic System Model. Circles represent model components (e.g., RVIC) and arrows between circles represent flux and state variables shared between components (e.g., streamflow). The colors of the arrows reflect the source of the fluxes and state variables.

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