Changing hydroclimate dynamics and the 19th to 20th century wetting trend in the English Channel region of northwest Europe

Northwestern Europe has experienced a trend of increasingly wet winters over the past 150 years, with few explanations for what may have driven this hydroclimatic change. Here we use the Old World Drought Atlas (OWDA), a tree-ring based reconstruction of the self-calibrating Palmer Drought Severity...

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Main Authors: Scholz, Serena R., Seager, Richard, Ting, Mingfang, Kushnir, Yochanan, Smerdon, Jason E., Cook, Benjamin I., Cook, Edward R., Baek, Seung Hun
Format: Article in Journal/Newspaper
Language:English
Published: 2021
Subjects:
Online Access:https://doi.org/10.7916/d8-vcvx-ep50
id ftcolumbiauniv:oai:academiccommons.columbia.edu:10.7916/d8-vcvx-ep50
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spelling ftcolumbiauniv:oai:academiccommons.columbia.edu:10.7916/d8-vcvx-ep50 2023-05-15T17:34:55+02:00 Changing hydroclimate dynamics and the 19th to 20th century wetting trend in the English Channel region of northwest Europe Scholz, Serena R. Seager, Richard Ting, Mingfang Kushnir, Yochanan Smerdon, Jason E. Cook, Benjamin I. Cook, Edward R. Baek, Seung Hun 2021 https://doi.org/10.7916/d8-vcvx-ep50 English eng https://doi.org/10.7916/d8-vcvx-ep50 Paleoclimatology Hydrology Droughts Precipitation (Meteorology) Articles 2021 ftcolumbiauniv https://doi.org/10.7916/d8-vcvx-ep50 2021-10-02T22:19:53Z Northwestern Europe has experienced a trend of increasingly wet winters over the past 150 years, with few explanations for what may have driven this hydroclimatic change. Here we use the Old World Drought Atlas (OWDA), a tree-ring based reconstruction of the self-calibrating Palmer Drought Severity Index (scPDSI), to examine this wetting trend and place it in a longer hydroclimatic context. We find that scPDSI variability in northwestern Europe is strongly correlated with the leading mode of the OWDA during the last millennium (1000–2012). This leading mode, here named the ‘English Channel’ (EC) mode, has pronounced variability on interannual to centennial timescales and has an expression in scPDSI similar to that of the East Atlantic teleconnection pattern. A shift in the EC mode from a prolonged negative phase to more neutral conditions during the 19th and 20th centuries is associated with the wetting trend over its area of influence in England, Wales, and much of northern continental Europe. The EC mode is the dominant scPDSI mode from approximately 1000–1850, after which its dominance waned in favor of the secondary ‘North–South’ (NS) mode, which has an expression in scPDSI similar to that of the winter North Atlantic Oscillation (NAO). We examine the dynamical nature of both of these modes and how they vary on interannual to centennial timescales. Our results provide insight into the nature of hydroclimate variability in Europe before the widespread availability of instrumental observations. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Columbia University: Academic Commons
institution Open Polar
collection Columbia University: Academic Commons
op_collection_id ftcolumbiauniv
language English
topic Paleoclimatology
Hydrology
Droughts
Precipitation (Meteorology)
spellingShingle Paleoclimatology
Hydrology
Droughts
Precipitation (Meteorology)
Scholz, Serena R.
Seager, Richard
Ting, Mingfang
Kushnir, Yochanan
Smerdon, Jason E.
Cook, Benjamin I.
Cook, Edward R.
Baek, Seung Hun
Changing hydroclimate dynamics and the 19th to 20th century wetting trend in the English Channel region of northwest Europe
topic_facet Paleoclimatology
Hydrology
Droughts
Precipitation (Meteorology)
description Northwestern Europe has experienced a trend of increasingly wet winters over the past 150 years, with few explanations for what may have driven this hydroclimatic change. Here we use the Old World Drought Atlas (OWDA), a tree-ring based reconstruction of the self-calibrating Palmer Drought Severity Index (scPDSI), to examine this wetting trend and place it in a longer hydroclimatic context. We find that scPDSI variability in northwestern Europe is strongly correlated with the leading mode of the OWDA during the last millennium (1000–2012). This leading mode, here named the ‘English Channel’ (EC) mode, has pronounced variability on interannual to centennial timescales and has an expression in scPDSI similar to that of the East Atlantic teleconnection pattern. A shift in the EC mode from a prolonged negative phase to more neutral conditions during the 19th and 20th centuries is associated with the wetting trend over its area of influence in England, Wales, and much of northern continental Europe. The EC mode is the dominant scPDSI mode from approximately 1000–1850, after which its dominance waned in favor of the secondary ‘North–South’ (NS) mode, which has an expression in scPDSI similar to that of the winter North Atlantic Oscillation (NAO). We examine the dynamical nature of both of these modes and how they vary on interannual to centennial timescales. Our results provide insight into the nature of hydroclimate variability in Europe before the widespread availability of instrumental observations.
format Article in Journal/Newspaper
author Scholz, Serena R.
Seager, Richard
Ting, Mingfang
Kushnir, Yochanan
Smerdon, Jason E.
Cook, Benjamin I.
Cook, Edward R.
Baek, Seung Hun
author_facet Scholz, Serena R.
Seager, Richard
Ting, Mingfang
Kushnir, Yochanan
Smerdon, Jason E.
Cook, Benjamin I.
Cook, Edward R.
Baek, Seung Hun
author_sort Scholz, Serena R.
title Changing hydroclimate dynamics and the 19th to 20th century wetting trend in the English Channel region of northwest Europe
title_short Changing hydroclimate dynamics and the 19th to 20th century wetting trend in the English Channel region of northwest Europe
title_full Changing hydroclimate dynamics and the 19th to 20th century wetting trend in the English Channel region of northwest Europe
title_fullStr Changing hydroclimate dynamics and the 19th to 20th century wetting trend in the English Channel region of northwest Europe
title_full_unstemmed Changing hydroclimate dynamics and the 19th to 20th century wetting trend in the English Channel region of northwest Europe
title_sort changing hydroclimate dynamics and the 19th to 20th century wetting trend in the english channel region of northwest europe
publishDate 2021
url https://doi.org/10.7916/d8-vcvx-ep50
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_relation https://doi.org/10.7916/d8-vcvx-ep50
op_doi https://doi.org/10.7916/d8-vcvx-ep50
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