Spatial and temporal analysis of a 17-year lightning climatology over Bangladesh with LIS data
© 2017 Springer-Verlag GmbH Austria Using NASA’s TRMM Lightning Imaging Sensor (LIS) data from 1998 to 2014, this paper presents a 17-year lightning climatology of Bangladesh, at 0.5° × 0.5° spatial resolution. Diurnal, seasonal, monthly and annual variations in the occurrence of lightning flashes w...
| Main Authors: | , , , , |
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| Format: | Journal Article |
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Springer Wien
2017
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| Online Access: | http://hdl.handle.net/20.500.11937/63056 |
| _version_ | 1848760982858366976 |
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| author | Dewan, Ashraf Ongee, E. Rahman, M. Mahmood, R. Yamane, Y. |
| author_facet | Dewan, Ashraf Ongee, E. Rahman, M. Mahmood, R. Yamane, Y. |
| author_sort | Dewan, Ashraf |
| building | Curtin Institutional Repository |
| collection | Online Access |
| description | © 2017 Springer-Verlag GmbH Austria Using NASA’s TRMM Lightning Imaging Sensor (LIS) data from 1998 to 2014, this paper presents a 17-year lightning climatology of Bangladesh, at 0.5° × 0.5° spatial resolution. Diurnal, seasonal, monthly and annual variations in the occurrence of lightning flashes were explored. The diurnal regime of lightning is dominated by afternoon/evening events. Overall, peak lightning activity occurs in the early morning (0200 LST) and evening (1900 LST). The distribution of lightning flash counts by season over Bangladesh landmass is as follows: pre-monsoon (69.2%), monsoon (24.1%), post-monsoon (4.6%) and winter (2.1%). Flash rate density (FRD) hotspots were primarily located in the north and north-eastern parts of Bangladesh, with a maximum of 72 fl km -2 year -1 . Spatially, the distribution of FRD increases from the Bay of Bengal in the south to relatively higher elevations (of the Himalayan foothills) in the north. A spatial shift in FRD hotspots occurs with change in season. For example, in monsoon season, hotspots of lightning activity move in a south-westerly direction from their pre-monsoon location (i.e. north-eastern Bangladesh) towards West Bengal in India. South and south-eastern parts of Bangladesh experience high lightning activity during post-monsoon season due to regional orographic lifting and low-pressure systems (i.e. cyclone) in the Bay of Bengal. To the best of our knowledge, this is the first study focused on LIS-based lightning climatology over Bangladesh. This baseline study, therefore, is an essential first step towards effective management of lightning-related hazards in Bangladesh. |
| first_indexed | 2025-11-14T10:24:26Z |
| format | Journal Article |
| id | curtin-20.500.11937-63056 |
| institution | Curtin University Malaysia |
| institution_category | Local University |
| last_indexed | 2025-11-14T10:24:26Z |
| publishDate | 2017 |
| publisher | Springer Wien |
| recordtype | eprints |
| repository_type | Digital Repository |
| spelling | curtin-20.500.11937-630562018-02-06T06:24:16Z Spatial and temporal analysis of a 17-year lightning climatology over Bangladesh with LIS data Dewan, Ashraf Ongee, E. Rahman, M. Mahmood, R. Yamane, Y. © 2017 Springer-Verlag GmbH Austria Using NASA’s TRMM Lightning Imaging Sensor (LIS) data from 1998 to 2014, this paper presents a 17-year lightning climatology of Bangladesh, at 0.5° × 0.5° spatial resolution. Diurnal, seasonal, monthly and annual variations in the occurrence of lightning flashes were explored. The diurnal regime of lightning is dominated by afternoon/evening events. Overall, peak lightning activity occurs in the early morning (0200 LST) and evening (1900 LST). The distribution of lightning flash counts by season over Bangladesh landmass is as follows: pre-monsoon (69.2%), monsoon (24.1%), post-monsoon (4.6%) and winter (2.1%). Flash rate density (FRD) hotspots were primarily located in the north and north-eastern parts of Bangladesh, with a maximum of 72 fl km -2 year -1 . Spatially, the distribution of FRD increases from the Bay of Bengal in the south to relatively higher elevations (of the Himalayan foothills) in the north. A spatial shift in FRD hotspots occurs with change in season. For example, in monsoon season, hotspots of lightning activity move in a south-westerly direction from their pre-monsoon location (i.e. north-eastern Bangladesh) towards West Bengal in India. South and south-eastern parts of Bangladesh experience high lightning activity during post-monsoon season due to regional orographic lifting and low-pressure systems (i.e. cyclone) in the Bay of Bengal. To the best of our knowledge, this is the first study focused on LIS-based lightning climatology over Bangladesh. This baseline study, therefore, is an essential first step towards effective management of lightning-related hazards in Bangladesh. 2017 Journal Article http://hdl.handle.net/20.500.11937/63056 10.1007/s00704-017-2278-3 Springer Wien restricted |
| spellingShingle | Dewan, Ashraf Ongee, E. Rahman, M. Mahmood, R. Yamane, Y. Spatial and temporal analysis of a 17-year lightning climatology over Bangladesh with LIS data |
| title | Spatial and temporal analysis of a 17-year lightning climatology over Bangladesh with LIS data |
| title_full | Spatial and temporal analysis of a 17-year lightning climatology over Bangladesh with LIS data |
| title_fullStr | Spatial and temporal analysis of a 17-year lightning climatology over Bangladesh with LIS data |
| title_full_unstemmed | Spatial and temporal analysis of a 17-year lightning climatology over Bangladesh with LIS data |
| title_short | Spatial and temporal analysis of a 17-year lightning climatology over Bangladesh with LIS data |
| title_sort | spatial and temporal analysis of a 17-year lightning climatology over bangladesh with lis data |
| url | http://hdl.handle.net/20.500.11937/63056 |