On the evidence of orographical modulation of regional fine scale precipitation change signals: The Carpathians
Abstract This study investigates the greenhouse gas‐induced winter and summer precipitation change signals over the Carpathian region with special focus on topographical effects and underlying processes. Six high‐resolution (~12 km grid spacing) regional climate model projections are analyzed for th...
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Online Access: | https://doi.org/10.1002/asl.967 |
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doaj-47bc2dbbed4d40e2872ffbad992caf1b2020-11-25T03:13:58ZengWileyAtmospheric Science Letters1530-261X2020-06-01216n/an/a10.1002/asl.967On the evidence of orographical modulation of regional fine scale precipitation change signals: The CarpathiansCsaba Torma0Filippo Giorgi1Department of Meteorology Eötvös Loránd University and MTA Post‐Doctoral Research Program Budapest HungaryEarth System Physics Section The Abdus Salam International Centre for Theoretical Physics Trieste ItalyAbstract This study investigates the greenhouse gas‐induced winter and summer precipitation change signals over the Carpathian region with special focus on topographical effects and underlying processes. Six high‐resolution (~12 km grid spacing) regional climate model projections are analyzed for the future period 2070–2099 with respect to the reference period 1976–2005 under the RCP8.5 scenarios. We find that the topographically induced fine scale modulation of the precipitation change signal is mostly of dynamical nature in winter (due to the precipitation shadowing effect), and thermodynamical in summer (associated with high elevation convection) over the region of interest. Additionally, elevation, size, and orientation of mountains play key roles in such processes. Our results draw attention to the fact that the high‐resolution representation of topography in climate models is crucial for the provision of fine scale precipitation projections in mountainous regions.https://doi.org/10.1002/asl.967Carpathian climateprecipitation changeregional climate modeling |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Csaba Torma Filippo Giorgi |
spellingShingle |
Csaba Torma Filippo Giorgi On the evidence of orographical modulation of regional fine scale precipitation change signals: The Carpathians Atmospheric Science Letters Carpathian climate precipitation change regional climate modeling |
author_facet |
Csaba Torma Filippo Giorgi |
author_sort |
Csaba Torma |
title |
On the evidence of orographical modulation of regional fine scale precipitation change signals: The Carpathians |
title_short |
On the evidence of orographical modulation of regional fine scale precipitation change signals: The Carpathians |
title_full |
On the evidence of orographical modulation of regional fine scale precipitation change signals: The Carpathians |
title_fullStr |
On the evidence of orographical modulation of regional fine scale precipitation change signals: The Carpathians |
title_full_unstemmed |
On the evidence of orographical modulation of regional fine scale precipitation change signals: The Carpathians |
title_sort |
on the evidence of orographical modulation of regional fine scale precipitation change signals: the carpathians |
publisher |
Wiley |
series |
Atmospheric Science Letters |
issn |
1530-261X |
publishDate |
2020-06-01 |
description |
Abstract This study investigates the greenhouse gas‐induced winter and summer precipitation change signals over the Carpathian region with special focus on topographical effects and underlying processes. Six high‐resolution (~12 km grid spacing) regional climate model projections are analyzed for the future period 2070–2099 with respect to the reference period 1976–2005 under the RCP8.5 scenarios. We find that the topographically induced fine scale modulation of the precipitation change signal is mostly of dynamical nature in winter (due to the precipitation shadowing effect), and thermodynamical in summer (associated with high elevation convection) over the region of interest. Additionally, elevation, size, and orientation of mountains play key roles in such processes. Our results draw attention to the fact that the high‐resolution representation of topography in climate models is crucial for the provision of fine scale precipitation projections in mountainous regions. |
topic |
Carpathian climate precipitation change regional climate modeling |
url |
https://doi.org/10.1002/asl.967 |
work_keys_str_mv |
AT csabatorma ontheevidenceoforographicalmodulationofregionalfinescaleprecipitationchangesignalsthecarpathians AT filippogiorgi ontheevidenceoforographicalmodulationofregionalfinescaleprecipitationchangesignalsthecarpathians |
_version_ |
1724645420218449920 |