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The long-lived monsoon depressions of 2006 and their linkage with the Indian Ocean Dipole

Krishnan, R and Ayantika, DC and Kumar, V and Pokhrel, S (2011) The long-lived monsoon depressions of 2006 and their linkage with the Indian Ocean Dipole. International Journal of Climatology, 31 (9). pp. 1334-1352.

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Abstract

A highlight of the 2006 boreal summer monsoon season was the enhanced activity of long-lived monsoon depressions and low-pressure systems (LPS) over the Indian region. Another important phenomenon during this period was the evolution of a positive Indian Ocean Dipole (PIOD) event. Although previous studies have investigated the impact of PIOD on the large-scale monsoon response, their influence on monsoon LPS activity is not well understood. Based on detailed diagnostic analyses of monsoon LPS during 2006, as well as those associated with other PIOD events during 1958-2007, the present work addresses two specific issues concerning the roles of (a) PIOD-induced large-scale circulation changes and (b) internal feedbacks between latent heating and dynamics, in sustaining the monsoon LPS activity. The results show that PIOD conditions generally favour increased propensity of long-lived (>5 days) LPS with long westward tracks extending into northwest India. The average contribution of long-lived monsoon LPS to the total is found to be approximately 12 higher during PIOD episodes as compared to non-PIOD. The PIOD events showed two important large-scale elements conducive for enhancement of LPS activity: (a) strengthening of cross-equatorial moisture transport from south-eastern tropical Indian Ocean into the Bay of Bengal and (b) enrichment of barotropic instability of monsoon flow. Estimates of latent-heating profiles from TRMM-satellite products during the 2006 LPS showed heating in the mesoscale updrafts above 600 hPa with maximum approximately 400 hPa; while cooling prevailed in lower levels. Stratiform precipitation covered approximately 70-85 of rain area during the prolonged LPS; and the large-scale monsoon Hadley-type circulation was found to be intensified with strong mid-level inflows entering the stratiform rain region. The overall findings suggest that the PIOD-induced background circulation together with internal feedbacks between mesoscale convective systems and large-scale circulation can effectively enhance the longevity of monsoon LPS. These results should serve as important inputs for numerical weather forecasting of extreme rainfall events associated with the regional monsoon phenomenon.

Item Type: Article
Additional Information: Copyright of this article belongs to Royal Meteorological Society.
Uncontrolled Keywords: Barotropic; Bay of Bengal; Diagnostic analysis; Extreme rainfall; Indian Ocean dipole; Internal feedback; Large-scale circulation; Life period; Low pressure systems; Mesoscale; Mesoscale Convective System; Moisture transport; Monsoon depressions; Numerical weather forecasting; Rain region; Stratiform precipitation; Summer monsoon; Tropical Indian ocean, Heating; Oceanography; Rain; Rain gages; Storms; Weather forecasting, Atmospheric thermodynamics, barotropic instability; convective system; low pressure system; moisture transfer; monsoon; sea surface temperature; summer; temperature anomaly; weather forecasting, Bay of Bengal; Indian Ocean
Subjects: Meteorology and Climatology
Depositing User: IITM Library
Date Deposited: 11 Aug 2014 11:00
Last Modified: 11 Aug 2014 11:00
URI: http://moeseprints.incois.gov.in/id/eprint/685

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