Thermal effect of climate change on groundwater-fed ecosystems
Abstract
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 »
- Authors:
-
- USGS Oregon Water Science Center, Portland, OR (United States)
- China Univ. of Geosciences, Wuhan (China)
- Texas A & M Univ., College Station, TX (United States)
- Univ. of California, Berkeley, CA (United States)
- USGS Geology, Minerals, Energy, and Geophysics Science Center, Menlo Park, CA (United States)
- USGS National Research Program, Menlo Park, CA (United States)
- USGS Forest and Rangeland Ecosystem Science Center, Corvallis, OR (United States)
- Publication Date:
- Research Org.:
- United States Geological Survey, Reston, VA (United States); Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)
- Sponsoring Org.:
- USDOE Office of Energy Efficiency and Renewable Energy (EERE), Renewable Power Office. Geothermal Technologies Office; USDOE Office of Science (SC)
- OSTI Identifier:
- 1425401
- Alternate Identifier(s):
- OSTI ID: 1479308
- Grant/Contract Number:
- EE0007169; AC02-05CH11231
- Resource 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)
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 54 ENVIRONMENTAL SCIENCES
Citation Formats
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., 2017.
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. https://doi.org/10.1002/2016WR020007
Burns, Erick R., Zhu, Yonghui, Zhan, Hongbin, Manga, Michael, Williams, Colin F., Ingebritsen, Steven E., and Dunham, Jason B. Mon .
"Thermal effect of climate change on groundwater-fed ecosystems". United States. https://doi.org/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 = {Mon Apr 24 00:00:00 EDT 2017},
month = {Mon Apr 24 00:00:00 EDT 2017}
}
Web of Science
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