Reorganization of the Spatial Dependence Structure of Indian Summer Monsoon Rainfall Extremes, 1951–2025

Point-wise intensification of daily rainfall extremes over India is well established, yet whether their joint spatial behavior is also changing has not been tested. We address this with 75 years (1951–2025) of 0.25° gridded India Meteorological Department daily rainfall, quantifying June–September (JJAS) extremal dependence through the extremal-coefficient function θ(h) and the dependence range ρ of a Brown–Resnick curve fitted to F-madogram estimates on rank-transformed fields; the rank transform strips out marginal trends, so any surviving signal belongs to the joint structure. The all-India range over the full record is 65.6 km (95% CI 62.0–69.5 km). Across 21 sliding 15-year windows, θ at 50 and 100 km fell significantly (p = 0.033 and 0.010 after serial-correlation correction): extremes co-occur more strongly at the storm scale. The signal is regional: Peninsular India’s dependence range grew from 56 km to 76 km between the 1951–1975 and 2001–2025 blocks, a 36% expansion (p = 0.002), and Central India’s window trend is +1.7 km decade−1 (p = 0.017). Independently, the largest connected daily exceedance cluster expanded in area by roughly 40% (p ≤ 0.0006). A Pettitt test dates the step in the footprint series to 1986 (p ≤ 0.0001), whereas the dependence series show progressive trends without a detectable break. Spatial reorganization is compounding marginal intensification: across Peninsular India, joint flood risk is growing faster than cell-wise return levels indicate.

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Journal
Atmosphere
Published
2026-09-13
DOI
https://doi.org/10.3390/atmos17090892
Primary Topic
Climate variability and models
Type
article
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Reorganization of the Spatial Dependence Structure of Indian Summer Monsoon Rainfall Extremes, 1951–2025

Sushil Kumar, Mohamed Zhran, Fahdah Falah Ben Hasher, Nitin Lohan
Atmosphere
Climate variability and models
article

Reorganization of the Spatial Dependence Structure of Indian Summer Monsoon Rainfall Extremes, 1951–2025

Sushil Kumar, Mohamed Zhran, Fahdah Falah Ben Hasher, Nitin Lohan
article en

Abstract

Point-wise intensification of daily rainfall extremes over India is well established, yet whether their joint spatial behavior is also changing has not been tested. We address this with 75 years (1951–2025) of 0.25° gridded India Meteorological Department daily rainfall, quantifying June–September (JJAS) extremal dependence through the extremal-coefficient function θ(h) and the dependence range ρ of a Brown–Resnick curve fitted to F-madogram estimates on rank-transformed fields; the rank transform strips out marginal trends, so any surviving signal belongs to the joint structure. The all-India range over the full record is 65.6 km (95% CI 62.0–69.5 km). Across 21 sliding 15-year windows, θ at 50 and 100 km fell significantly (p = 0.033 and 0.010 after serial-correlation correction): extremes co-occur more strongly at the storm scale. The signal is regional: Peninsular India’s dependence range grew from 56 km to 76 km between the 1951–1975 and 2001–2025 blocks, a 36% expansion (p = 0.002), and Central India’s window trend is +1.7 km decade−1 (p = 0.017). Independently, the largest connected daily exceedance cluster expanded in area by roughly 40% (p ≤ 0.0006). A Pettitt test dates the step in the footprint series to 1986 (p ≤ 0.0001), whereas the dependence series show progressive trends without a detectable break. Spatial reorganization is compounding marginal intensification: across Peninsular India, joint flood risk is growing faster than cell-wise return levels indicate.

AtmosphereVol. 17(9)
Princess Nourah bint Abdulrahman University (SA), Mansoura University (EG), Institute of Technology Management (IN), Gautam Buddha University (IN)
Climate action
Openalex Percentile: Top 13%
Climate variability and models
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Reorganization of the Spatial Dependence Structure of Indian Summer Monsoon Rainfall Extremes, 1951–2025 — Sushil Kumar, Mohamed Zhran, et al. · Atmosphere (2026) | TGRS Research Map | TGRS