/vahmani-etal_2021_et

Will anthropogenic warming increase Evapotranspiration? Examining Irrigation Water Demand Implications of Climate Change in California

Primary LanguageMATLABBSD 2-Clause "Simplified" LicenseBSD-2-Clause

DOI

vahmani-etal_2021_et

Will anthropogenic warming increase Evapotranspiration? Examining Irrigation Water Demand Implications of Climate Change in California

P. Vahmani*1, A. D. Jones1, and D. Li2

1 Lawrence Berkeley National Laboratory, One Cyclotron Road, Berkeley, CA 94720, USA.

2 Department of Earth and Environment, Boston University, Boston, MA, USA.

* corresponding author: pvahmani@lbl.gov

Abstract

Climate modeling studies and observations do not fully agree on the implications of anthropogenic warming for evapotranspiration (ET), a major component of the water cycle and driver of irrigation water demand. Here we use California as a testbed to assess the ET impacts of changing atmospheric conditions induced by climate change on irrigated systems. Our analysis of irrigated agricultural and urban regions shows that warmer atmospheric temperatures have minimal implications for ET rates and irrigation water demands--about one percent change per degree Celsius warming (~1%°C-1). By explicitly modeling irrigation, we control for the confounding effect of climate-driven soil moisture changes and directly estimate water demand implications. Our attribution analysis of the drivers of ET response to global anthropogenic warming shows that as the atmospheric temperature and vapor pressure deficit depart from the ideal conditions for transpiration, regulation of stomata resistance by stressed vegetation almost completely offsets the expected increase in ET rates that would otherwise result from abiotic processes alone. We further show that anthropogenic warming of the atmosphere has minimal implications for mean relative humidity (<1.7%°C-1) and the surface available energy (<0.2%°C-1), which are critical drivers of ET. This study corroborates the growing evidence that plant physiological changes moderate the degree to which changes in potential ET are realized as actual ET.

Journal reference

P. Vahmani P., A. D. Jones, and D. Li, 2021, Will anthropogenic warming increase Evapotranspiration? Examining Irrigation Water Demand Implications of Climate Change in California, Earth's Future.

Data reference

Input data

National Centers for Environmental Prediction/National Weather Service/NOAA/U.S. Department of Commerce (2005), NCEP North American Regional Reanalysis (NARR), https://rda.ucar.edu/datasets/ds608.0/, Research Data Archive at the National Center for Atmospheric Research, Computational and Information Systems Laboratory, Boulder, Colo.

Output data

WRF-UCM output data at 1.5 km resolution and supporting files can be accessed via Globus endpoint.

Contributing modeling software

Model Version Repository Link DOI
WRF 3.6.1 https://github.com/hanschen/WRFV3 NA

Reproduce my experiment

  1. Follow the instruction at https://www2.mmm.ucar.edu/wrf/OnLineTutorial/ to Download and compile WRFv3.6.1
  2. Run WRF-UCM over CA for 15 years (2001-2015):
  3. Repeat step 2 for three different scenarios as described in the manuscript. The WRF folders (one for each scenario) with the inputs, parameter tables, and namelists are available via Globus endpoint:
    • S31_base_ens01_WRFRun_2001.tar
    • S31_cnrm_ens01_WRFRun_2001.tar
    • S31_hadg_ens01_WRFRun_2001.tar
  4. The attribution analysis (Figure 3) can be reproduced using the spreadsheet:

Reproduce my figures

Use the scripts from the folder 4.Figures to reproduce the figures used in this publication:

Script Name Description How to Run
M01_Variable_Extraction_for_hpc_V2.m Script to convert NetCDF files to MATLAB files matlab -nodisplay -nosplash -nodesktop -r "run('M01_Variable_Extraction_for_hpc_V2.m');exit;"
aM01_wrfout_plot_spatial_v4.m Script to create spatial maps in Figures 2, 4, S1, S2, S4 matlab -nodisplay -nosplash -nodesktop -r "run(‘aM01_wrfout_plot_spatial_v4.m');exit;"
aM0_wrfout_attribution_of_changes_in_ET_v11.m Script to create intermediate data on partial differentials presented in the attribution analysis matlab -nodisplay -nosplash -nodesktop -r "run('aM0_wrfout_attribution_of_changes_in_ET_v11.m');exit;"
aM1_change_spatial.m


aM2_change_bar.m


aM3_attribution_bar.m
Scripts to use intermediate data from above to create Figures 3 and S3 matlab -nodisplay -nosplash -nodesktop -r "run(aM1_change_spatial.m');exit;"

matlab -nodisplay -nosplash -nodesktop -r "run(aM1_change_bar.m');exit;"

matlab -nodisplay -nosplash -nodesktop -r "run(aM1_attricution_bar.m');exit;"