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Hydrology

Arabian Sea cyclones briefly refill desert aquifers

Saleh H, Sultan M, Yan E, et al. · Communications earth & environment · 2025

Open access · cc by · source: Europe PMC

A few intense tropical cyclones now supply most of interior Oman’s rain and can add cubic kilometres of groundwater, interrupting chronic depletion.

How this study connects

Role on claims

Each row is a claim on a concept or method page where this paper supports, challenges, or qualifies the statement. Roles are hand-checked — not a model guess.

  • SupportsHydrologyconcept

    This library holds 8 empirical papers on hydrology with measured outcomes rather than reviews.

    Evidence for the claim as stated.

  • SupportsHydrologyconcept

    A few intense tropical cyclones now supply most of interior Oman’s rain and can add cubic kilometres of groundwater, interrupting chronic depletion.

    Evidence for the claim as stated.

Study at a glance

Design
Other — IBTrACS landfalling cyclones plus GRACE, wells, and RiverFlow2D recharge estimates for interior Oman
N
Arabian Sea TCs 1990–2020; detailed recharge for Keila 2011, Mekunu 2018, and Cyclone 2020
Population
Najd aquifers of interior Oman under Arabian Sea tropical cyclones
Outcome
Intense tropical cyclones now supply most of interior Oman’s rain and can add cubic kilometres of groundwater, interrupting chronic depletion

Structured fields used in claim comparison tables when every cited study has a complete layer.

Inspect source passages

Arabian Sea cyclones briefly refill desert aquifers

These passages occur verbatim in the stored paper text. They support the points listed below; they do not verify every statement in the explanation.

How much have intense Arabian Sea TCs increased after 1995, as cited?

In the Arabian Sea (part of the North Indian Ocean basin), a regional climate shift has increased intense TCs five-fold after 1995 compared to the previous 25 years .
Read passages in the original paper

Key findings

Najd received >60% of precipitation from TCs (Mekunu 20.1 km3 rain). GRACE TWS rose 3.2 ± 1.4 km3 after Mekunu, matching modelled recharge of 3.5 km3; Keila and 2020 barely moved GRACE. Unconfined water tables rose 1.7 m after Mekunu/2020, with up to 55 m rise in confined Hanfit wells. Background GRACE depletion was −0.4 then −0.9 km3 yr−1.

Methodology

The authors tracked 1990–2020 Arabian Peninsula landfalling cyclones, then estimated Najd (200,000 km2) recharge from Keila (2011), Mekunu (2018), and Cyclone 2020 using GRACE TWS, well levels, and a calibrated RiverFlow2D model.

Limitations

Three storms cannot prove every future cyclone will recharge. GRACE cannot isolate 2020 from lingering Mekunu. Agricultural pumping (cultivated area 5 to 95 km2) still dominates the long-term budget. RiverFlow2D ran only 17–18 days per storm.

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