the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Representing Farmer Irrigated Crop Area Adaptation in a Large-Scale Hydrological Model
Nathalie Voisin
Christian Klassert
Travis Thurber
Wenwei Xu
Abstract. Large-scale hydrological models (LHMs) are commonly used for regional and global assessment of future water shortage outcomes under climate and socioeconomic scenarios. The irrigation of croplands, which accounts for the lion’s share of human water consumption, is critical in understanding these water shortage trajectories. Despite irrigation’s defining role, LHM frameworks typically impose trajectories of land use that underlie irrigation demand, neglecting potential dynamic feedbacks in the form of human instigation of and subsequent adaptation to water shortage via irrigated crop area changes. We extend an LHM, MOSART-WM, with adaptive farmer agents, applying the model to the Continental United States to explore water shortage outcomes that emerge from the interplay between hydrologic-driven surface water availability, reservoir management, and farmer irrigated crop area adaptation. The extended modeling framework is used to conduct hypothetical computational experiment comparing differences between a model run with and without the incorporation of adaptive farmer agents. These comparative simulations reveal that accounting for farmer adaptation via irrigated crop area changes substantially alters modeled water shortage outcomes, with U.S.-wide annual water shortage reduced by as much as 42 percent when comparing adaptive and non-adaptive versions of the model forced with U.S. climatology from 1950–2009.
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Jim Yoon et al.
Status: final response (author comments only)
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RC1: 'Comment on egusphere-2023-1604', Yi-Chen Ethan Yang, 10 Aug 2023
The paper “Representing Farmer Irrigated Crop Area Adaptation in a Large-Scale Hydrological Model” developed an agent-based module for a large-scale hydrologic model to incorporate the adaptive crop-related decisions of farmers. I believe this is an urgent topic in the field of water resources systems analysis, the research is scientifically sound, the paper is well organized, and the results are very interesting. Nevertheless, I have the following comments for the authors to consider and potentially improve the quality of their manuscript.
First, I would suggest adding more references to the “two-way” coupling studies to smooth the logic flow. While I think this paper might be one of the first to conduct a two-way coupling of an agent-based model with a hydrologic model at the US scale, the concept itself is not brand new. There are several previous studies have already done this at the basin scale (some of the basins are fairly large such as the Mekong, Niger, and Colorado Basins). Citing these previous studies will provide readers with a better understanding of how this two-way coupling concept was developed.
Second, I do think more technical details should be provided in the methodology section. While the development and the connection of the two sub-models are quite clear, several technical details are only mentioned briefly. For example, the setting of groundwater supply, the real-world meaning of the two PMP coefficients, and the calculation of the adjusted perceived cost of production. To me, it is totally ok to make some assumptions to make the model development feasible, but these details should be provided and the readers can judge themselves. Two related comments regarding methodology. 1) I think the authors should provide the ODD+D document in the supplementary material which becomes a standard in any ABM study. This will allow other ABMers to quickly understand the ABM setting. 2) I think a summary table to show the necessary data (sources, years, resolution, etc.) can help readers better understand the scope and scale of this model.
Third, I understand that this manuscript is testing a hypothetical experiment and I think it is fine for model development purposes. But I think the authors should still provide the calibration results and partially demonstrate that the model they developed (at least more or less) captures the overall trend and pattern of historical data (e.g., crop area and/or streamflow). Otherwise, it is very difficult to convince readers that the model is suitable for hypothetical experiments. One of the major criticisms of ABM is that these models are “toy models” that do not reflect reality. Since the authors use historical data to calibrate their PMP parameters, they should show the results as evidence that this is not just a toy model. Again, several two-way coupled ABM studies in recent years have already shown the calibration results to demonstrate the model's credibility. This is the most critical comment I have.
I have some minor comments below to help the authors to improve the readability.
Line 85: Does this mean groundwater is an "infinite underground reservoir?" It is ok for this assumption but need to make it clear to the readers.
Line 97: This is interesting. Is there a reason why this 50 km threshold? How sensitive is this threshold?
Line 103: I assume the hydrological proxy during the calibration period is like a long-term average?
Line 173: I assume “Data Sources and Processing” mean Section 2.3? Because there is no sub-section with this title.
Line 188: Is there a specific reason why this period: 2010-2013 is used?
Line 233: I assume farm-level optimization is agent level in Section 2.2?
Line 246: I think the calculation is Water Demand = crop area * irrigation requirement. In the ABM, when you adjust water demand, did you change both crop area and irrigation requirement? Or do you only change the crop area?
Line 252 and 265: Are these assumed to be the same throughout the simulation period? It is fine if that is the case, but should be clarified.
Line 256: Do you mean Table S1?
Line 286: Is this a typo for PerceivedCost?
Line 292: Can you provide an equation?
Line 312: I think you might need to mention what is VIC first. Also, is irrigation water availability = streamflow in each grid?
Line 322 (Section 2.4): Don't really think you need one page of these backgrounds since these are already published. So maybe merge this section with 2.3.6 to smooth the logic flow? Otherwise, a sudden mention of simulated irrigation water availability is a bit logical jump.
Line 371: I think an equation to show how you calculate water shortage is still necessary.
Line 393: I think some text in the caption of Fig 2 should be moved (or copied) to the main text like how you calculate the blue and orange bars and dots.
Line 394: Is it a typo for Fig2b?
Line 426 and 444: I think you need to at least show the Eastern US results in the supplementary material because you do emphasize in your abstract and introduction that this is a CONUS study. But currently, there are no results showing this scale.
Line 435: It is a bit unclear how you calculate Fig 3e-h? Is it a long-term average? Counting every model year?
Line 470: I don't see the results of agricultural profits. Are you showing any figures or tables?
Line 545: I think there is another limitation worth mentioning which is social norm effects. Farmers' behaviors are heavily affected by their social networks (neighbors, friends, etc.). There are ABM out there showing this already and can be considered in the future.
Citation: https://doi.org/10.5194/egusphere-2023-1604-RC1 -
RC2: 'Comment on egusphere-2023-1604', Anonymous Referee #2, 07 Sep 2023
The study introduces an agent-based module into a hydrological model to integrate the dynamic decision-making processes of farmers regarding crop-related choices. The research demonstrates strong scientific rigor, the paper maintains a well-structured organization, and the findings are notably captivating. I would like to offer the following constructive feedback to the authors, which could potentially enhance the overall quality of their manuscript.
My main comment is regarding the use of surface water only. Most irrigation in the USA is from groundwater. How are the results impacted by this assumption? Groundwater pumping can be considered an adaptation strategy when surface water runs out.
Line 30: Please quantify how much water is consumed and withdrawn by irrigation in the world and the USA.
Line 32-33: There is extensive work on irrigation expansion done by Rosa and colleagues. Elliot et al., 2014 did not quantify irrigation expansion, but impacts of climate change on current irrigation.
https://www.science.org/doi/full/10.1126/sciadv.aaz6031
https://iopscience.iop.org/article/10.1088/1748-9326/aadeef/meta
https://www.pnas.org/doi/abs/10.1073/pnas.2017796117
https://iopscience.iop.org/article/10.1088/1748-9326/ac7408/meta
Line 35: Recent literature that quantified the contribution of dam-based water storage on irrigation: https://www.pnas.org/doi/abs/10.1073/pnas.2214291119
Citation: https://doi.org/10.5194/egusphere-2023-1604-RC2
Jim Yoon et al.
Jim Yoon et al.
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