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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Main Authors: Csaba Torma, Filippo Giorgi
Format: Article
Language:English
Published: Wiley 2020-06-01
Series:Atmospheric Science Letters
Subjects:
Online Access:https://doi.org/10.1002/asl.967
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spelling 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
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