Please use this identifier to cite or link to this item: http://dr.iiserpune.ac.in:8080/xmlui/handle/123456789/10674
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dc.contributor.authorSandhyavijayan, K.en_US
dc.contributor.authorSooraj, K. P.en_US
dc.contributor.authorETTAMMAL, SUHASen_US
dc.contributor.authorTerray, Pascalen_US
dc.date.accessioned2026-01-30T06:35:08Z
dc.date.available2026-01-30T06:35:08Z
dc.date.issued2026-01en_US
dc.identifier.citationClimate Dynamics, 64(57).en_US
dc.identifier.issn1432-0894en_US
dc.identifier.issn0930-7575en_US
dc.identifier.urihttps://doi.org/10.1007/s00382-025-08014-xen_US
dc.identifier.urihttp://dr.iiserpune.ac.in:8080/xmlui/handle/123456789/10674
dc.description.abstractDespite the decisive role of Bay of Bengal Monsoon Depressions (MDs) in contributing to the Indian summer monsoon mean rainfall, the exact mechanisms and processes contributing to their prolonged residence over the Indian landmass remain still elusive. So, a comprehensive analysis on the factors affecting the inland penetration length of MDs after landfall over the Indian landmass, is presented here using MDs identified from Indian Meteorology Department weather reports over 3 decades (1991–2020). Exploration of large-scale atmospheric circulation features using ERA-5 reanalysis data shed new insights on the processes contributing to the maintenance and sustenance of land penetrating MDs. Notably, all Higher Inland Propagating (HIP) MDs were preceded by Mid-Tropospheric Cyclones (MTCs, with cyclonic circulation in the lower and mid-troposphere) over North-West (NW) India, with this entire region experiencing increased moisture flux convergence, thus facilitating the deep intrusion of MDs into the Indian landmass. In contrast, the Lower Inland Propagating (LIP) MDs experience dry air intrusion from the adjacent desert region, creating unfavorable moisture conditions and leading to their rapid dissipation. Intriguingly, the HIP MDs were further found to cluster with the westward propagating large-scale intraseasonal mode (i.e.,10–20 days). Using the updated GLDAS soil moisture reanalysis, it is further revealed that the precipitation caused by both the MTC, and the 10–20 days intraseasonal oscillation mode saturates the land surfaces before the arrival of MDs in the northwestern central Indian region during HIP events. In short, our results show that the presence of cyclonic vorticity over NW India, in association with the large-scale westward propagating (10–20 days) mode of variability, creates favorable conditions for the inland penetration of HIP events. Further, the results highlighting the importance of 10–20 days mode and its propensity to cluster with the land penetrating MDs, assume significance in a changing climate, as the subseasonal Indian monsoon rainfall variability is projected to increase in the future.en_US
dc.language.isoenen_US
dc.publisherSpringer Natureen_US
dc.subjectMonsoon depressions (MDs)en_US
dc.subjectHigher inland propagating (HIP) MDsen_US
dc.subjectLower inland propagating (LIP) MDsen_US
dc.subjectMid-tropospheric cyclonesen_US
dc.subjectSoil moistureen_US
dc.subjectIntraseasonal oscillationen_US
dc.subject2026-JAN-WEEK4en_US
dc.subjectTOC-JAN-2026en_US
dc.subject2026en_US
dc.titleDynamics of the inland penetrating Indian monsoon depressionsen_US
dc.typeArticleen_US
dc.contributor.departmentDept. of Earth and Climate Scienceen_US
dc.identifier.sourcetitleClimate Dynamicsen_US
dc.publication.originofpublisherForeignen_US
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