Show/Hide Menu
Hide/Show Apps
Logout
Türkçe
Türkçe
Search
Search
Login
Login
OpenMETU
OpenMETU
About
About
Open Science Policy
Open Science Policy
Open Access Guideline
Open Access Guideline
Postgraduate Thesis Guideline
Postgraduate Thesis Guideline
Communities & Collections
Communities & Collections
Help
Help
Frequently Asked Questions
Frequently Asked Questions
Guides
Guides
Thesis submission
Thesis submission
MS without thesis term project submission
MS without thesis term project submission
Publication submission with DOI
Publication submission with DOI
Publication submission
Publication submission
Supporting Information
Supporting Information
General Information
General Information
Copyright, Embargo and License
Copyright, Embargo and License
Contact us
Contact us
High-Resolution Climate Simulations Over the Eastern Mediterranean Black Sea Region Using the Pseudo-Global Warming Method With a CMIP6 Ensemble
Download
JGR Atmospheres - 2024 - Bağçaci - High‐Resolution Climate Simulations Over the Eastern Mediterranean Black Sea Region.pdf
Date
2024-05-28
Author
Bağçaci, S. Çağatay
Yücel, İsmail
Yılmaz, Mustafa Tuğrul
Şen, Osman Taha
Ludwig, Patrick
Metadata
Show full item record
This work is licensed under a
Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License
.
Item Usage Stats
44
views
20
downloads
Cite This
The strong drying expected in the Eastern Mediterranean with climate change could cause mass migration of people already living under water shortages. On the other hand, precipitation is expected to increase toward the region’s north, particularly those along the interior of the eastern Black Sea coasts, which could worsen existing floods. However, this double-sided adverse phenomenon and its underlying reasons have been investigated by relatively low-resolution models in the Eastern Mediterranean Black Sea (EMBS) region, where orographic precipitation prevails. This study performs 4 km resolution Weather Research and Forecasting (WRF) model simulations with and without climate change signals retrieved from a CMIP6 GCM ensemble via pseudo-global-warming (PGW). The WRF simulations captured the large-scale dynamics affecting the EMBS fairly well: an anticyclonic low-level circulation and enhancing subsidence stem from anomalous ridge development over the central Mediterranean in winter (DJF), and a cyclonic low-level circulation and weakening subsidence rise from heat-low development over the Eastern Mediterranean in summer (JJA). The resulting picture of future warming and drying over the area generally supports the literature, although new insights emerge in anomalous precipitation increase, especially in the summer season over the Greater Caucasus and nearby regions. Most likely, the warmer-than-expected Caspian Sea induces a large increase in specific humidity and, thus, a large moisture source in the lower troposphere and an extension of the heat-low effect in the mid-troposphere. In addition, the high-resolution WRF simulations provide added value over the complex topography of the Caucasian Mountain range for new insights into this region.
Subject Keywords
CMIP6
,
Eastern Mediterranean Black Sea region
,
high-resolution
,
pseudo-global-warming
,
weather research and forecasting model
URI
https://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=85193821506&origin=inward
https://hdl.handle.net/11511/109969
Journal
Journal of Geophysical Research: Atmospheres
DOI
https://doi.org/10.1029/2023jd040145
Collections
Department of Civil Engineering, Article
Citation Formats
IEEE
ACM
APA
CHICAGO
MLA
BibTeX
S. Ç. Bağçaci, İ. Yücel, M. T. Yılmaz, O. T. Şen, and P. Ludwig, “High-Resolution Climate Simulations Over the Eastern Mediterranean Black Sea Region Using the Pseudo-Global Warming Method With a CMIP6 Ensemble,”
Journal of Geophysical Research: Atmospheres
, vol. 129, no. 10, pp. 0–0, 2024, Accessed: 00, 2024. [Online]. Available: https://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=85193821506&origin=inward.