Details:

Journal Title:
Hydrology and Earth System Sciences
Personal Author:
Lawston-Parker, Patricia ; Santanello Jr., Joseph A. ; Chaney, Nathaniel W.
Lawston-Parker, Patricia ; Santanello Jr., Joseph A. ; Chaney, Nathaniel W. Less -
NOAA Program & Office:
OAR (Oceanic and Atmospheric Research)
Description:
The transport of water, heat, and momentum from the surface to the atmosphere is dependent, in part, on the characteristics of the land surface. Along with the model physics, parameterization schemes, and parameters employed, land datasets determine the spatial variability in land surface states (i.e., soil moisture and temperature) and fluxes. Despite the importance of these datasets, they are often chosen out of convenience or owing to regional limitations, without due assessment of their impacts on model results. Irrigation is an anthropogenic form of land heterogeneity that has been shown to alter the land surface energy balance, ambient weather, and local circulations. As such, irrigation schemes are becoming more prevalent in weather and climate models, with rapid developments in dataset availability and parameterization scheme complexity. Thus, to address pragmatic issues related to modeling irrigation, this study uses a high-resolution, regional coupled modeling system to investigate the impacts of irrigation dataset selection on land–atmosphere (L–A) coupling using a case study from the Great Plains Irrigation Experiment (GRAINEX) field campaign. The simulations are assessed in the context of irrigated vs. nonirrigated regions, subregions across the irrigation gradient, and sub-grid-scale process representation in coarser-scale models. The results show that L–A coupling is sensitive to the choice of irrigation dataset and resolution and that the irrigation impact on surface fluxes and near-surface meteorology can be dominant, conditioned on the details of the irrigation map (e.g., boundaries and heterogeneity), or minimal. A consistent finding across several analyses was that even a low percentage of irrigation fraction (i.e., 4 %–16 %) can have significant local and downstream atmospheric impacts (e.g., lower planetary boundary layer, PBL, height), suggesting that the representation of boundaries and heterogeneous areas within irrigated regions is particularly important for the modeling of irrigation impacts on the atmosphere in this model. When viewing the simulations presented here as a proxy for “ideal” tiling in an Earth-system-model-scale grid box, the results show that some “tiles” will reach critical nonlinear moisture and PBL thresholds that could be important for clouds and convection, implying that heterogeneity resulting from irrigation should be taken into consideration in new sub-grid L–A exchange parameterizations.
Keywords:
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General Earth And Planetary Sciences General Engineering General Environmental Science
Source:
Hydrology and Earth System Sciences, 27(14), 2787-2805
DOI:
https://doi.org/10.5194/hess-27-2787-2023
ISSN:
1607-7938
Format:
PDF
Publisher:
Copernicus GmbH
Document Type:
Journal Article
Funding:
Grant no. NOAA-OAR-CPO-2019-2005530 ; Grant no. OAR-CPO-2019-2005530
Grant no. NOAA-OAR-CPO-2019-2005530 ; Grant no. OAR-CPO-2019-2005530 Less -
License:
https://creativecommons.org/licenses/by/4.0/
Rights Information:
CC BY
Compliance:
Library
Main Document Checksum:
[+]
urn:sha256:de5fac5be3a8cdb2143365efe45b7fb3786c41b65c9b0839460d4da02616778d
Download URL:
https://repository.library.noaa.gov/view/noaa/58224/noaa_58224_DS1.pdf
File Type:

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