Evapotranspiration and water yield of a pine-broadleaf forest are not altered by long-term atmospheric [CO2] enrichment under native or enhanced soil fertility
Abstract
Abstract Changes in evapotranspiration ( ET ) from terrestrial ecosystems affect their water yield ( WY ), with considerable ecological and economic consequences. Increases in surface runoff observed over the past century have been attributed to increasing atmospheric CO 2 concentrations resulting in reduced ET by terrestrial ecosystems. Here, we evaluate the water balance of a Pinus taeda (L.) forest with a broadleaf component that was exposed to atmospheric [CO 2 ] enrichment (ECO 2 ; +200 ppm) for over 17 years and fertilization for 6 years, monitored with hundreds of environmental and sap flux sensors on a half‐hourly basis. These measurements were synthesized using a one‐dimensional Richard's equation model to evaluate treatment differences in transpiration ( T ), evaporation ( E ), ET , and WY . We found that ECO 2 did not create significant differences in stand T, ET , or WY under either native or enhanced soil fertility, despite a 20% and 13% increase in leaf area index, respectively. While T , ET , and WY responded to fertilization, this response was weak (<3% of mean annual precipitation). Likewise, while E responded to ECO 2 in the first 7 years of the study, this effect was of negligible magnitude (<1%more »
- Authors:
-
[1];
[4];
[8];
- Duke Univ., Durham, NC (United States); Oak Ridge National Lab. (ORNL), Oak Ridge, TN (United States)
- Duke Univ., Durham, NC (United States); Univ. of Helsinki, Helsinki (Finland)
- Duke Univ., Durham, NC (United States); Seoul National Univ., Seoul (Korea); National Center for Agro‐Meteorology, Seoul (Korea)
- Duke Univ., Durham, NC (United States); Univ. of Notre Dame, Notre Dame, IN (United States)
- Duke Univ., Durham, NC (United States); Chulalongkorn Univ., Bangkok (Thailand)
- Univ. of Wyoming, Laramie, WY (United States)
- Univ. of Oklahoma, Norman, OK (United States)
- Duke Univ., Durham, NC (United States); USDA Forest Service, Otto, NC (United States)
- Univ. of Utah, Salt Lake City, UT (United States)
- Duke Univ., Durham, NC (United States)
- Boston Univ., Boston, MA (United States)
- Rutgers Univ., Newark, NJ (United States)
- Publication Date:
- Research Org.:
- Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States)
- Sponsoring Org.:
- USDOE Office of Science (SC), Biological and Environmental Research (BER)
- OSTI Identifier:
- 1560506
- Alternate Identifier(s):
- OSTI ID: 1462779
- Grant/Contract Number:
- AC05-00OR22725
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Global Change Biology
- Additional Journal Information:
- Journal Volume: 24; Journal Issue: 10; Journal ID: ISSN 1354-1013
- Publisher:
- Wiley
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 59 BASIC BIOLOGICAL SCIENCES
Citation Formats
Ward, Eric J., Oren, Ram, Seok Kim, Hyun, Kim, Dohyoung, Tor-ngern, Pantana, Ewers, Brent E., McCarthy, Heather R., Oishi, Andrew Christopher, Pataki, Diane E., Palmroth, Sari, Phillips, Nathan G., and Schäfer, Karina V. R. Evapotranspiration and water yield of a pine-broadleaf forest are not altered by long-term atmospheric [CO2] enrichment under native or enhanced soil fertility. United States: N. p., 2018.
Web. doi:10.1111/gcb.14363.
Ward, Eric J., Oren, Ram, Seok Kim, Hyun, Kim, Dohyoung, Tor-ngern, Pantana, Ewers, Brent E., McCarthy, Heather R., Oishi, Andrew Christopher, Pataki, Diane E., Palmroth, Sari, Phillips, Nathan G., & Schäfer, Karina V. R. Evapotranspiration and water yield of a pine-broadleaf forest are not altered by long-term atmospheric [CO2] enrichment under native or enhanced soil fertility. United States. https://doi.org/10.1111/gcb.14363
Ward, Eric J., Oren, Ram, Seok Kim, Hyun, Kim, Dohyoung, Tor-ngern, Pantana, Ewers, Brent E., McCarthy, Heather R., Oishi, Andrew Christopher, Pataki, Diane E., Palmroth, Sari, Phillips, Nathan G., and Schäfer, Karina V. R. Wed .
"Evapotranspiration and water yield of a pine-broadleaf forest are not altered by long-term atmospheric [CO2] enrichment under native or enhanced soil fertility". United States. https://doi.org/10.1111/gcb.14363. https://www.osti.gov/servlets/purl/1560506.
@article{osti_1560506,
title = {Evapotranspiration and water yield of a pine-broadleaf forest are not altered by long-term atmospheric [CO2] enrichment under native or enhanced soil fertility},
author = {Ward, Eric J. and Oren, Ram and Seok Kim, Hyun and Kim, Dohyoung and Tor-ngern, Pantana and Ewers, Brent E. and McCarthy, Heather R. and Oishi, Andrew Christopher and Pataki, Diane E. and Palmroth, Sari and Phillips, Nathan G. and Schäfer, Karina V. R.},
abstractNote = {Abstract Changes in evapotranspiration ( ET ) from terrestrial ecosystems affect their water yield ( WY ), with considerable ecological and economic consequences. Increases in surface runoff observed over the past century have been attributed to increasing atmospheric CO 2 concentrations resulting in reduced ET by terrestrial ecosystems. Here, we evaluate the water balance of a Pinus taeda (L.) forest with a broadleaf component that was exposed to atmospheric [CO 2 ] enrichment (ECO 2 ; +200 ppm) for over 17 years and fertilization for 6 years, monitored with hundreds of environmental and sap flux sensors on a half‐hourly basis. These measurements were synthesized using a one‐dimensional Richard's equation model to evaluate treatment differences in transpiration ( T ), evaporation ( E ), ET , and WY . We found that ECO 2 did not create significant differences in stand T, ET , or WY under either native or enhanced soil fertility, despite a 20% and 13% increase in leaf area index, respectively. While T , ET , and WY responded to fertilization, this response was weak (<3% of mean annual precipitation). Likewise, while E responded to ECO 2 in the first 7 years of the study, this effect was of negligible magnitude (<1% mean annual precipitation). Given the global range of conifers similar to P. taeda , our results imply that recent observations of increased global streamflow cannot be attributed to decreases in ET across all ecosystems, demonstrating a great need for model–data synthesis activities to incorporate our current understanding of terrestrial vegetation in global water cycle models.},
doi = {10.1111/gcb.14363},
journal = {Global Change Biology},
number = 10,
volume = 24,
place = {United States},
year = {Wed Jun 27 00:00:00 EDT 2018},
month = {Wed Jun 27 00:00:00 EDT 2018}
}
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