Low-pressure systems and extreme precipitation in central India: sensitivity to temperature changes

Extreme rainfall events in the central Indian region are often related to the passage of synoptic scale monsoon low-pressure systems (LPS). This study uses the surrogate climate change method on ten monsoon LPS cases connected to observed extreme rainfall events, to investigate how sensitive the pre...

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Bibliographic Details
Published in:Climate dynamics 2016-07, Vol.47 (1-2), p.465-480
Main Authors: Sørland, Silje Lund, Sorteberg, Asgeir
Format: Article
Language:English
Subjects:
Analysis
Atmosphere
Atmospheric temperature
Boundary conditions
Climate change
Climatology
Earth and Environmental Science
Earth Sciences
Extreme weather
Geophysics/Geodesy
Marine
Monsoons
Oceanography
Precipitation
Precipitation (Meteorology)
Precipitation rate
Rainfall
Runoff
Specific humidity
Temperature
Wind
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Summary:Extreme rainfall events in the central Indian region are often related to the passage of synoptic scale monsoon low-pressure systems (LPS). This study uses the surrogate climate change method on ten monsoon LPS cases connected to observed extreme rainfall events, to investigate how sensitive the precipitation and runoff are to an idealized warmer and moister atmosphere. The ten cases are simulated with three different initial and lateral boundary conditions: the unperturbed control run, and two sets of perturbed runs where the atmospheric temperature is increased uniformly throughout the atmosphere, the specific humidity increased according to Clausius Clapeyron’s relation, but the large-scale flow is unchanged. The difference between the control and perturbed simulations are mainly due to the imposed warming and feedback influencing the synoptic flow. The mean precipitation change with warming in the central Indian region is 18–20 %/K, with largest changes at the end of the LPS tracks. The LPS in the warmer runs are bringing more moisture further inland that is released as precipitation. In the perturbed runs the precipitation rate is increasing at all percentiles, and there is more frequent rainfall with very heavy intensities. This leads to a shift in which category that contributes most to the total precipitation: more of the precipitation is coming from the category with very heavy intensities. The runoff changes are similar to the precipitation changes, except the response in intensity of very heavy runoff, which is around twice the change in intensity of very heavy precipitation.
ISSN:0930-7575
1432-0894
DOI:10.1007/s00382-015-2850-4