A coupled agent-based model to analyse human-drought feedbacks for agropastoralists in dryland regions

被引:13
作者
Streefkerk, Ileen N. [1 ]
de Bruijn, Jens [1 ,2 ]
Haer, Toon [1 ]
Van Loon, Anne F. [1 ]
Quichimbo, Edisson A. [3 ]
Wens, Marthe [1 ]
Hassaballah, Khalid [4 ]
Aerts, Jeroen C. J. H. [1 ,5 ]
机构
[1] Vrije Univ Amsterdam, Inst Environm Studies IVM, Amsterdam, Netherlands
[2] Int Inst Appl Syst Anal IIASA, Water Secur, Laxenburg, Austria
[3] Cardiff Univ, Sch Earth & Environm Sci, Cardiff, Wales
[4] IGAD Climate Predict & Applicat Ctr ICPAC, Dept Climate & Water Applicat, Nairobi, Kenya
[5] Deltares, Dept IRP, Delft, Netherlands
来源
FRONTIERS IN WATER | 2023年 / 4卷
基金
欧洲研究理事会;
关键词
drought; feedbacks; agent-based model (ABM); socio-hydrology; agropastoralists; drylands; SMALLHOLDER FARMERS; ADAPTATION; HYDROLOGY; RISK; FRAMEWORK;
D O I
10.3389/frwa.2022.1037971
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Drought is a persistent hazard that impacts the environment, people's livelihoods, access to education and food security. Adaptation choices made by people can influence the propagation of this drought hazard. However, few drought models incorporate adaptive behavior and feedbacks between adaptations and drought. In this research, we present a dynamic drought adaptation modeling framework, ADOPT-AP, which combines socio-hydrological and agent-based modeling approaches. This approach is applied to agropastoral communities in dryland regions in Kenya. We couple the spatially explicit hydrological Dryland Water Partitioning (DRYP) model with a behavioral model capable of simulating different bounded rational behavioral theories (ADOPT). The results demonstrate that agropastoralists respond differently to drought due to differences in (perceptions of) their hydrological environment. Downstream communities are impacted more heavily and implement more short-term adaptation measures than upstream communities in the same catchment. Additional drivers of drought adaptation concern socio-economic factors such as wealth and distance to wells. We show that the uptake of drought adaptation influences soil moisture (positively through irrigation) and groundwater (negatively through abstraction) and, thus, the drought propagation through the hydrological cycle.
引用
收藏
页数:18
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