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Title: Thermal effect of climate change on groundwater-fed ecosystems

Groundwater temperature changes will lag surface temperature changes from a changing climate. Steady state solutions of the heat-transport equations are used to identify key processes that control the long-term thermal response of springs and other groundwater discharge to climate change, in particular changes in (1) groundwater recharge rate and temperature and (2) land-surface temperature transmitted through the vadose zone. Transient solutions are developed to estimate the time required for new thermal signals to arrive at ecosystems. The solution is applied to the volcanic Medicine Lake highlands, California, USA, and associated springs complexes that host groundwater-dependent ecosystems. In this system, upper basin groundwater temperatures are strongly affected only by recharge conditions. However, as the vadose zone thins away from the highlands, changes in the average annual land-surface temperature also influence groundwater temperatures. Transient response to temperature change depends on both the conductive time scale and the rate at which recharge delivers heat. Most of the thermal response of groundwater at high elevations will occur within 20 years of a shift in recharge temperatures, but the large lower elevation springs will respond more slowly, with about half of the conductive response occurring within the first 20 years and about half of themore » advective response to higher recharge temperatures occurring in approximately 60 years.« less
Authors:
ORCiD logo [1] ; ORCiD logo [2] ; ORCiD logo [3] ; ORCiD logo [4] ; ORCiD logo [5] ; ORCiD logo [6] ; ORCiD logo [7]
  1. USGS Oregon Water Science Center, Portland, OR (United States)
  2. China Univ. of Geosciences, Wuhan (China)
  3. Texas A & M Univ., College Station, TX (United States)
  4. Univ. of California, Berkeley, CA (United States)
  5. USGS Geology, Minerals, Energy, and Geophysics Science Center, Menlo Park, CA (United States)
  6. USGS National Research Program, Menlo Park, CA (United States)
  7. USGS Forest and Rangeland Ecosystem Science Center, Corvallis, OR (United States)
Publication Date:
Grant/Contract Number:
EE0007169; AC02-05CH11231
Type:
Accepted Manuscript
Journal Name:
Water Resources Research
Additional Journal Information:
Journal Volume: 53; Journal Issue: 4; Journal ID: ISSN 0043-1397
Publisher:
American Geophysical Union (AGU)
Research Org:
United States Geological Survey, Reston, VA (United States); Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States)
Sponsoring Org:
USDOE Office of Energy Efficiency and Renewable Energy (EERE), Geothermal Technologies Office (EE-4G); USDOE Office of Science (SC)
Country of Publication:
United States
Language:
English
Subject:
54 ENVIRONMENTAL SCIENCES
OSTI Identifier:
1425401
Alternate Identifier(s):
OSTI ID: 1479308

Burns, Erick R., Zhu, Yonghui, Zhan, Hongbin, Manga, Michael, Williams, Colin F., Ingebritsen, Steven E., and Dunham, Jason B.. Thermal effect of climate change on groundwater-fed ecosystems. United States: N. p., Web. doi:10.1002/2016WR020007.
Burns, Erick R., Zhu, Yonghui, Zhan, Hongbin, Manga, Michael, Williams, Colin F., Ingebritsen, Steven E., & Dunham, Jason B.. Thermal effect of climate change on groundwater-fed ecosystems. United States. doi:10.1002/2016WR020007.
Burns, Erick R., Zhu, Yonghui, Zhan, Hongbin, Manga, Michael, Williams, Colin F., Ingebritsen, Steven E., and Dunham, Jason B.. 2017. "Thermal effect of climate change on groundwater-fed ecosystems". United States. doi:10.1002/2016WR020007. https://www.osti.gov/servlets/purl/1425401.
@article{osti_1425401,
title = {Thermal effect of climate change on groundwater-fed ecosystems},
author = {Burns, Erick R. and Zhu, Yonghui and Zhan, Hongbin and Manga, Michael and Williams, Colin F. and Ingebritsen, Steven E. and Dunham, Jason B.},
abstractNote = {Groundwater temperature changes will lag surface temperature changes from a changing climate. Steady state solutions of the heat-transport equations are used to identify key processes that control the long-term thermal response of springs and other groundwater discharge to climate change, in particular changes in (1) groundwater recharge rate and temperature and (2) land-surface temperature transmitted through the vadose zone. Transient solutions are developed to estimate the time required for new thermal signals to arrive at ecosystems. The solution is applied to the volcanic Medicine Lake highlands, California, USA, and associated springs complexes that host groundwater-dependent ecosystems. In this system, upper basin groundwater temperatures are strongly affected only by recharge conditions. However, as the vadose zone thins away from the highlands, changes in the average annual land-surface temperature also influence groundwater temperatures. Transient response to temperature change depends on both the conductive time scale and the rate at which recharge delivers heat. Most of the thermal response of groundwater at high elevations will occur within 20 years of a shift in recharge temperatures, but the large lower elevation springs will respond more slowly, with about half of the conductive response occurring within the first 20 years and about half of the advective response to higher recharge temperatures occurring in approximately 60 years.},
doi = {10.1002/2016WR020007},
journal = {Water Resources Research},
number = 4,
volume = 53,
place = {United States},
year = {2017},
month = {4}
}