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Hydroscience Journal
Volume 108, 2022 - Issue 1
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Research Article

Performance evaluation of CORDEX South Asia models for projections of precipitation over the Kabul basin, Afghanistan

Évaluation de la performance des modèles CORDEX d’Asie du Sud pour les projections climatiques de prècipitations sur le bassin de Kaboul, Afghanistan

ORCID Icon, , &
Article: 2095936 | Published online: 22 Aug 2022

Figures & data

Figure 1. Topographic map of the Kabul basin, Afghanistan, with climate grid used in this study.

Figure 1. Topographic map of the Kabul basin, Afghanistan, with climate grid used in this study.

Table 1. Data used in this study.

Figure 2. Taylor diagram for comparison of monthly precipitation in CORDEX SA (Coordinated Regional Downscaling Experiment South Asia) with APHRODITE (Asian Precipitation – Highly-Resolved Observational Data Integration Towards Evaluation) for the baseline period (1986–2005). IDs refer to .

Figure 2. Taylor diagram for comparison of monthly precipitation in CORDEX SA (Coordinated Regional Downscaling Experiment South Asia) with APHRODITE (Asian Precipitation – Highly-Resolved Observational Data Integration Towards Evaluation) for the baseline period (1986–2005). IDs refer to Table 1.

Figure 3. Long-term average of monthly precipitation in CORDEX SA (Coordinated Regional Downscaling Experiment South Asia) and APHRODITE (Asian Precipitation – Highly-Resolved Observational Data Integration Towards Evaluation) for the baseline period (1986–2005).IDs refer to .

Figure 3. Long-term average of monthly precipitation in CORDEX SA (Coordinated Regional Downscaling Experiment South Asia) and APHRODITE (Asian Precipitation – Highly-Resolved Observational Data Integration Towards Evaluation) for the baseline period (1986–2005).IDs refer to Table 1.

Figure 4. Spatial distribution of annual precipitation in CORDEX SA (Coordinated Regional Downscaling Experiment South Asia) and APHRODITE (Asian Precipitation – Highly-Resolved Observational Data Integration Towards Evaluation) for the baseline period (1986–2005).IDs refer to .

Figure 4. Spatial distribution of annual precipitation in CORDEX SA (Coordinated Regional Downscaling Experiment South Asia) and APHRODITE (Asian Precipitation – Highly-Resolved Observational Data Integration Towards Evaluation) for the baseline period (1986–2005).IDs refer to Table 1.

Table 2. Verification statistics of monthly precipitation in CORDEX SA compared with APHRODITE for the baseline period (1986 to 2005).

Table 3. Monthly changes in future precipitation (%) for the Kabul basin using six selected RCMs under 2 RCP scenarios.

Figure 5. Future precipitation projections of Kabul basin.

Figure 5. Future precipitation projections of Kabul basin.

Figure 6. Average seasonal changes of precipitation from six selected RCMs (Regional Climate Models) over the baseline period (1986–2005).

Figure 6. Average seasonal changes of precipitation from six selected RCMs (Regional Climate Models) over the baseline period (1986–2005).

Figure 7. Spatial distribution of future projected precipitation changes over the baseline period (1986–2005) in the Kabul basin.

Figure 7. Spatial distribution of future projected precipitation changes over the baseline period (1986–2005) in the Kabul basin.

Data availability statement

In this study, two different types of data were used: (a) the APHRODITE global precipitation dataset available in the public domain at http://www.chikyu.ac.jp/precip/english/products.html; and (b) regional circulation model (RCM) datasets from the Coordinated Regional Downscaling Experiment (CORDEX) program (see Jones et al., Citation2011) https://cordex.org/data-access/.