Rise in Northeast US extreme precipitation caused by Atlantic variability and climate change

Extreme precipitation (EP) in the Northeastern United States increased abruptly after 1996, coinciding with warming Atlantic sea surface temperatures (SSTs). We examine the importance of internal variability and external forcings (including anthropogenic and natural forcings) to these EP and SST inc...

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Main Authors: Huang, H, Patricola, CM, Winter, JM, Osterberg, EC, Mankin, JS
Format: Article in Journal/Newspaper
Language:unknown
Published: eScholarship, University of California 2021
Subjects:
Online Access:https://escholarship.org/uc/item/0kx0b7h0
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spelling ftcdlib:oai:escholarship.org/ark:/13030/qt0kx0b7h0 2023-05-15T17:29:56+02:00 Rise in Northeast US extreme precipitation caused by Atlantic variability and climate change Huang, H Patricola, CM Winter, JM Osterberg, EC Mankin, JS 2021-09-01 application/pdf https://escholarship.org/uc/item/0kx0b7h0 unknown eScholarship, University of California qt0kx0b7h0 https://escholarship.org/uc/item/0kx0b7h0 public Extreme precipitation Atlantic sea surface temperatures Anthropogenic forcings Atlantic multidecadal variability Optimal fingerprinting Time of detection Atmospheric Sciences article 2021 ftcdlib 2021-10-18T17:16:20Z Extreme precipitation (EP) in the Northeastern United States increased abruptly after 1996, coinciding with warming Atlantic sea surface temperatures (SSTs). We examine the importance of internal variability and external forcings (including anthropogenic and natural forcings) to these EP and SST increases by using the Community Earth System Model large ensembles and an optimal fingerprint method to isolate the effects of different forcings on 1929–2018 Northeast EP and North Atlantic SSTs. We find that external forcings have significantly influenced both Northeast EP and North Atlantic SSTs, with a time of detection in 2008 and 1968, respectively. Beyond SST changes attributable to internal variability of the Atlantic, anthropogenic aerosols and greenhouse gases are important drivers of SST changes, first detected in 1968 and 1983, respectively. Greenhouse gases are the only anthropogenic forcing exerting substantial influence on EP, first detected in 2008. We therefore attribute the 1996 EP shift to both unforced Atlantic variability and anthropogenic forcings. Article in Journal/Newspaper North Atlantic University of California: eScholarship
institution Open Polar
collection University of California: eScholarship
op_collection_id ftcdlib
language unknown
topic Extreme precipitation
Atlantic sea surface temperatures
Anthropogenic forcings
Atlantic multidecadal variability
Optimal fingerprinting
Time of detection
Atmospheric Sciences
spellingShingle Extreme precipitation
Atlantic sea surface temperatures
Anthropogenic forcings
Atlantic multidecadal variability
Optimal fingerprinting
Time of detection
Atmospheric Sciences
Huang, H
Patricola, CM
Winter, JM
Osterberg, EC
Mankin, JS
Rise in Northeast US extreme precipitation caused by Atlantic variability and climate change
topic_facet Extreme precipitation
Atlantic sea surface temperatures
Anthropogenic forcings
Atlantic multidecadal variability
Optimal fingerprinting
Time of detection
Atmospheric Sciences
description Extreme precipitation (EP) in the Northeastern United States increased abruptly after 1996, coinciding with warming Atlantic sea surface temperatures (SSTs). We examine the importance of internal variability and external forcings (including anthropogenic and natural forcings) to these EP and SST increases by using the Community Earth System Model large ensembles and an optimal fingerprint method to isolate the effects of different forcings on 1929–2018 Northeast EP and North Atlantic SSTs. We find that external forcings have significantly influenced both Northeast EP and North Atlantic SSTs, with a time of detection in 2008 and 1968, respectively. Beyond SST changes attributable to internal variability of the Atlantic, anthropogenic aerosols and greenhouse gases are important drivers of SST changes, first detected in 1968 and 1983, respectively. Greenhouse gases are the only anthropogenic forcing exerting substantial influence on EP, first detected in 2008. We therefore attribute the 1996 EP shift to both unforced Atlantic variability and anthropogenic forcings.
format Article in Journal/Newspaper
author Huang, H
Patricola, CM
Winter, JM
Osterberg, EC
Mankin, JS
author_facet Huang, H
Patricola, CM
Winter, JM
Osterberg, EC
Mankin, JS
author_sort Huang, H
title Rise in Northeast US extreme precipitation caused by Atlantic variability and climate change
title_short Rise in Northeast US extreme precipitation caused by Atlantic variability and climate change
title_full Rise in Northeast US extreme precipitation caused by Atlantic variability and climate change
title_fullStr Rise in Northeast US extreme precipitation caused by Atlantic variability and climate change
title_full_unstemmed Rise in Northeast US extreme precipitation caused by Atlantic variability and climate change
title_sort rise in northeast us extreme precipitation caused by atlantic variability and climate change
publisher eScholarship, University of California
publishDate 2021
url https://escholarship.org/uc/item/0kx0b7h0
genre North Atlantic
genre_facet North Atlantic
op_relation qt0kx0b7h0
https://escholarship.org/uc/item/0kx0b7h0
op_rights public
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