Analysis of the daily rainfall events over India using a new long period (1901-2010) high resolution (0.25°×0.25°) gridded rainfall data set
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| 024 | 7 | 0 | |a 10.1007/s00382-014-2307-1 |2 doi |
| 035 | |a (NATIONALLICENCE)springer-10.1007/s00382-014-2307-1 | ||
| 245 | 0 | 0 | |a Analysis of the daily rainfall events over India using a new long period (1901-2010) high resolution (0.25°×0.25°) gridded rainfall data set |h [Elektronische Daten] |c [D. Pai, Latha Sridhar, M. Badwaik, M. Rajeevan] |
| 520 | 3 | |a In this study, analysis of the long term climatology, variability and trends in the daily rainfall events of ≥5mm [or daily rainfall (DR) events] during the southwest monsoon season (June-September) over four regions of India; south central India (SCI), north central India (NCI), northeast India (NEI) and west coast (WC) have been presented. For this purpose, a new high spatial resolution (0.25°×0.25°) daily gridded rainfall data set covering 110years (1901-2010) over the Indian main land has been used. The association of monsoon low pressure systems (LPSs) with the DR events of various intensities has also been examined. Major portion of the rainfall over these regions during the season was received in the form of medium rainfall (≥5-100mm) or moderate rainfall (MR) events. The mean seasonal cycle of the daily frequency of heavy rainfall (HR) (≥100-150mm) or HR events and very heavy rainfall (VHR) (≥150mm) or VHR events over each of the four regions showed peak at different parts of the season. The peak in the mean daily HR and VHR events occurred during middle of July to middle of August over SCI, during late part of June to early part of July over NCI, during middle of June to early July over NEI, and during late June to middle July over WC. Significant long term trends in the frequency and intensity of the DR events were observed in all the four geographical regions. Whereas the intensity of the DR events over all the four regions showed significant positive trends during the second half and the total period, the signs and magnitude of the long term trends in the frequency of the various categories of DR events during the total period and its two halves differed from the region to the region. The trend analysis revealed increased disaster potential for instant flooding over SCI and NCI during the recent years due to significant increasing trends in the frequency (areal coverage) and intensity of the HR and VHR events during the recent half of the data period. However, there is increased disaster potential over NEI and WC due to the increasing trends in the intensity of the rainfall events. There is strong association between the LPS days and the DR events in both the spatial and temporal scales. In all the four regions, the contributions to the total MR events by the LPS days were nearly equal. On the other hand, there was relatively large regional difference in the number of combined HR and VHR events associated with LPS days particularly that associated with monsoon depression (LPS stronger than monsoon depression) days. The possible reasons for the same have also been discussed. The increasing trend in the monsoon low (low pressure) days post 1970s is the primary reason for the observed significant increasing trends in the HR and VHR events over SCI and NCI and decreasing trend in HR events over NEI during the recent half (1956-2010). This is in spite of the decreasing trend in the MD days. | |
| 540 | |a Springer-Verlag Berlin Heidelberg, 2014 | ||
| 690 | 7 | |a Daily rainfall events |2 nationallicence | |
| 690 | 7 | |a Trends in the extreme rainfall events |2 nationallicence | |
| 690 | 7 | |a SW monsoon |2 nationallicence | |
| 690 | 7 | |a Long term trends |2 nationallicence | |
| 690 | 7 | |a Low pressure systems |2 nationallicence | |
| 700 | 1 | |a Pai |D D. |u India Meteorological Department, Pune, India |4 aut | |
| 700 | 1 | |a Sridhar |D Latha |u India Meteorological Department, Pune, India |4 aut | |
| 700 | 1 | |a Badwaik |D M. |u India Meteorological Department, Pune, India |4 aut | |
| 700 | 1 | |a Rajeevan |D M. |u Earth System Science Organization, Ministry of Earth Sciences, New Delhi, India |4 aut | |
| 773 | 0 | |t Climate Dynamics |d Springer Berlin Heidelberg |g 45/3-4(2015-08-01), 755-776 |x 0930-7575 |q 45:3-4<755 |1 2015 |2 45 |o 382 | |
| 856 | 4 | 0 | |u https://doi.org/10.1007/s00382-014-2307-1 |q text/html |z Onlinezugriff via DOI |
| 898 | |a BK010053 |b XK010053 |c XK010000 | ||
| 900 | 7 | |a Metadata rights reserved |b Springer special CC-BY-NC licence |2 nationallicence | |
| 908 | |D 1 |a research-article |2 jats | ||
| 949 | |B NATIONALLICENCE |F NATIONALLICENCE |b NL-springer | ||
| 950 | |B NATIONALLICENCE |P 856 |E 40 |u https://doi.org/10.1007/s00382-014-2307-1 |q text/html |z Onlinezugriff via DOI | ||
| 950 | |B NATIONALLICENCE |P 700 |E 1- |a Pai |D D. |u India Meteorological Department, Pune, India |4 aut | ||
| 950 | |B NATIONALLICENCE |P 700 |E 1- |a Sridhar |D Latha |u India Meteorological Department, Pune, India |4 aut | ||
| 950 | |B NATIONALLICENCE |P 700 |E 1- |a Badwaik |D M. |u India Meteorological Department, Pune, India |4 aut | ||
| 950 | |B NATIONALLICENCE |P 700 |E 1- |a Rajeevan |D M. |u Earth System Science Organization, Ministry of Earth Sciences, New Delhi, India |4 aut | ||
| 950 | |B NATIONALLICENCE |P 773 |E 0- |t Climate Dynamics |d Springer Berlin Heidelberg |g 45/3-4(2015-08-01), 755-776 |x 0930-7575 |q 45:3-4<755 |1 2015 |2 45 |o 382 | ||