2024
Rempe, D; McCormick, EL; Hahm, WJ; Persad, GG; Cummins, C
Resilience of woody ecosystems to precipitation variability Journal Article
In: EarthArXiv, 2024.
Links | BibTeX | Tags: climate change, Drought, ERCZO, precipitation, woody plants
@article{Rempe2022,
title = {Resilience of woody ecosystems to precipitation variability},
author = {D Rempe and EL McCormick and WJ Hahm and GG Persad and C Cummins},
doi = {https://doi.org/10.31223/X5XW7D},
year = {2024},
date = {2024-12-31},
urldate = {2024-12-31},
journal = {EarthArXiv},
keywords = {climate change, Drought, ERCZO, precipitation, woody plants},
pubstate = {published},
tppubtype = {article}
}
2021
McCormick, E.; Dralle, D. N.; Hahm, W. J.; Tune, A. K.; Schmidt, L. M.; Chadwick, K. D.; Rempe, D. M.
Evidence for widespread woody plant use of water stored in bedrock Journal Article
In: Nature, 2021.
Abstract | Links | BibTeX | Tags: bedrock water, ERCZO, root zone, transpiration, woody plants
@article{McCormick2021,
title = {Evidence for widespread woody plant use of water stored in bedrock},
author = {E. McCormick and D. N. Dralle and W. J. Hahm and A. K. Tune and L. M. Schmidt and K. D. Chadwick and D. M. Rempe},
doi = {https://doi.org/10.1038/s41586-021-03761-3},
year = {2021},
date = {2021-09-08},
urldate = {2021-01-14},
journal = {Nature},
abstract = {Woody plant transpiration is a major control on Earth’s climate system, streamflow, and human water supply. Soils are widely considered to be the primary reservoir of water for woody plants, however, plants also access water stored in the fractures and pores of bedrock, either as rock moisture (water stored in the unsaturated zone) (Schwinning, 2010) or bedrock groundwater (below the water table) (Miller et al., 2010). Bedrock as a water source for plants has not been evaluated over large scales, and consequently, its importance to terrestrial water and carbon cycling is poorly known (Fan et al., 2019). Here, we show that woody plants routinely access significant quantities of water stored in bedrock —commonly as rock moisture —for transpiration across diverse climates and biomes. For example, in California, the volume of bedrock water transpired by woody vegetation annually exceeds that stored in man-made reservoirs, and woody vegetation that withdraws bedrock water accounts for over 50% of the aboveground carbon stocks in the state. Our findings show that bedrock water storage dynamics are a critical element of terrestrial water cycling and therefore necessary to capture the effect of shifting climate on woody ecosystems, above- and belowground carbon storage, and water resources.},
keywords = {bedrock water, ERCZO, root zone, transpiration, woody plants},
pubstate = {published},
tppubtype = {article}
}
Woody plant transpiration is a major control on Earth’s climate system, streamflow, and human water supply. Soils are widely considered to be the primary reservoir of water for woody plants, however, plants also access water stored in the fractures and pores of bedrock, either as rock moisture (water stored in the unsaturated zone) (Schwinning, 2010) or bedrock groundwater (below the water table) (Miller et al., 2010). Bedrock as a water source for plants has not been evaluated over large scales, and consequently, its importance to terrestrial water and carbon cycling is poorly known (Fan et al., 2019). Here, we show that woody plants routinely access significant quantities of water stored in bedrock —commonly as rock moisture —for transpiration across diverse climates and biomes. For example, in California, the volume of bedrock water transpired by woody vegetation annually exceeds that stored in man-made reservoirs, and woody vegetation that withdraws bedrock water accounts for over 50% of the aboveground carbon stocks in the state. Our findings show that bedrock water storage dynamics are a critical element of terrestrial water cycling and therefore necessary to capture the effect of shifting climate on woody ecosystems, above- and belowground carbon storage, and water resources.