Climate change projections of maximum temperature in the pre-monsoon season in Bangladesh using statistical downscaling of global climate models
The climate of Bangladesh is very likely to be influenced by global climate change. To quantify the influence on the climate of Bangladesh, Global Climate Models were downscaled statistically to produce future climate projections of maximum temperature during the pre-monsoon season (March–May) for t...
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Published in | Advances in science and research Vol. 18; pp. 99 - 114 |
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Main Authors | , , , , , , |
Format | Journal Article |
Language | English |
Published |
Katlenburg-Lindau
Copernicus GmbH
13.07.2021
Copernicus Publications |
Subjects | |
Online Access | Get full text |
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Summary: | The climate of Bangladesh is very likely to be influenced by global climate change. To quantify the influence on the climate of Bangladesh, Global Climate Models were downscaled statistically to produce future climate projections of maximum temperature during the pre-monsoon season (March–May) for the 21st century for Bangladesh. The future climate
projections are generated based on three emission scenarios (RCP2.6, RCP4.5
and RCP8.5) provided by the fifth Coupled Model Intercomparison Project. The downscaling process is undertaken by relating the large-scale seasonal mean temperature, taken from the ERA5 reanalysis data set, to the leading principal components of the observed maximum temperature at stations under
Bangladesh Meteorological Department in Bangladesh, and applying the
relationship to the GCM ensemble. The in-situ temperature data has only
recently been digitised, and this is the first time they have been used in
statistical downscaling of local climate projections for Bangladesh. This
analysis also provides an evaluation of the local data, and the local
temperatures in Bangladesh show a close match with the ERA5 reanalysis.
Compared to the reference period of 1981–2010, the projected maximum
pre-monsoon temperature in Bangladesh indicate an increase by 0.7/0.7/0.7 ∘C in the near future (2021–2050) and 2.2/1.2/0.8 ∘C in the far future (2071–2100) assuming the RCP8.5/RCP4.5/RCP2.6 scenario, respectively. |
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ISSN: | 1992-0636 1992-0628 1992-0636 |
DOI: | 10.5194/asr-18-99-2021 |