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Past and future changes in climate and hydrological indicators in the US Northeast

Past and future changes in climate and hydrological indicators in the US Northeast
Past and future changes in climate and hydrological indicators in the US Northeast

To assess the influence of global climate change at the regional scale, we examine past and future changes in key climate, hydrological, and biophysical indicators across the US Northeast (NE). We first consider the extent to which simulations of twentieth century climate from nine atmosphere-ocean general circulation models (AOGCMs) are able to reproduce observed changes in these indicators. We then evaluate projected future trends in primary climate characteristics and indicators of change, including seasonal temperatures, rainfall and drought, snow cover, soil moisture, streamflow, and changes in biometeorological indicators that depend on threshold or accumulated temperatures such as growing season, frost days, and Spring Indices (SI). Changes in indicators for which temperature-related signals have already been observed (seasonal warming patterns, advances in high-spring streamflow, decreases in snow depth, extended growing seasons, earlier bloom dates) are generally reproduced by past model simulations and are projected to continue in the future. Other indicators for which trends have not yet been observed also show projected future changes consistent with a warmer climate (shrinking snow cover, more frequent droughts, and extended low-flow periods in summer). The magnitude of temperature-driven trends in the future are generally projected to be higher under the Special Report on Emission Scenarios (SRES) mid-high (A2) and higher (A1FI) emissions scenarios than under the lower (B1) scenario. These results provide confidence regarding the direction of many regional climate trends, and highlight the fundamental role of future emissions in determining the potential magnitude of changes we can expect over the coming century.

0930-7575
381-407
Hayhoe, Katharine
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Wake, Cameron P.
42df31f8-5438-430e-b0b6-7d56ecd2ea9b
Huntington, Thomas G.
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Luo, Lifeng
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Schwartz, Mark D.
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Sheffield, Justin
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Wood, Eric
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Anderson, Bruce
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Bradbury, James
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DeGaetano, Art
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Troy, Tara J.
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Wolfe, David
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Hayhoe, Katharine
d4a5a568-d714-4233-a6eb-f4c1935bcaf5
Wake, Cameron P.
42df31f8-5438-430e-b0b6-7d56ecd2ea9b
Huntington, Thomas G.
e2b2f6a9-f2bf-4b03-9a01-07afd4507332
Luo, Lifeng
e9b25aa8-e877-45a6-bdca-53aba9bbde84
Schwartz, Mark D.
f663a32d-3a53-4c08-92a5-5da2f3a629a2
Sheffield, Justin
dd66575b-a4dc-4190-ad95-df2d6aaaaa6b
Wood, Eric
8352c1b4-4fd3-42fe-bd23-46619024f1cf
Anderson, Bruce
710831bd-e4bc-4348-a547-c5bc3f80336a
Bradbury, James
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DeGaetano, Art
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Troy, Tara J.
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Wolfe, David
bc578ec5-4e7c-4182-a8e3-9ac17d2f6fa9

Hayhoe, Katharine, Wake, Cameron P., Huntington, Thomas G., Luo, Lifeng, Schwartz, Mark D., Sheffield, Justin, Wood, Eric, Anderson, Bruce, Bradbury, James, DeGaetano, Art, Troy, Tara J. and Wolfe, David (2006) Past and future changes in climate and hydrological indicators in the US Northeast. Climate Dynamics, 28 (4), 381-407. (doi:10.1007/s00382-006-0187-8).

Record type: Article

Abstract

To assess the influence of global climate change at the regional scale, we examine past and future changes in key climate, hydrological, and biophysical indicators across the US Northeast (NE). We first consider the extent to which simulations of twentieth century climate from nine atmosphere-ocean general circulation models (AOGCMs) are able to reproduce observed changes in these indicators. We then evaluate projected future trends in primary climate characteristics and indicators of change, including seasonal temperatures, rainfall and drought, snow cover, soil moisture, streamflow, and changes in biometeorological indicators that depend on threshold or accumulated temperatures such as growing season, frost days, and Spring Indices (SI). Changes in indicators for which temperature-related signals have already been observed (seasonal warming patterns, advances in high-spring streamflow, decreases in snow depth, extended growing seasons, earlier bloom dates) are generally reproduced by past model simulations and are projected to continue in the future. Other indicators for which trends have not yet been observed also show projected future changes consistent with a warmer climate (shrinking snow cover, more frequent droughts, and extended low-flow periods in summer). The magnitude of temperature-driven trends in the future are generally projected to be higher under the Special Report on Emission Scenarios (SRES) mid-high (A2) and higher (A1FI) emissions scenarios than under the lower (B1) scenario. These results provide confidence regarding the direction of many regional climate trends, and highlight the fundamental role of future emissions in determining the potential magnitude of changes we can expect over the coming century.

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More information

Accepted/In Press date: 1 August 2006
e-pub ahead of print date: 16 November 2006

Identifiers

Local EPrints ID: 480920
URI: http://eprints.soton.ac.uk/id/eprint/480920
ISSN: 0930-7575
PURE UUID: b5d2df56-47ed-4507-9a80-dbca95761726
ORCID for Justin Sheffield: ORCID iD orcid.org/0000-0003-2400-0630

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Date deposited: 10 Aug 2023 16:58
Last modified: 17 Mar 2024 03:40

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Contributors

Author: Katharine Hayhoe
Author: Cameron P. Wake
Author: Thomas G. Huntington
Author: Lifeng Luo
Author: Mark D. Schwartz
Author: Eric Wood
Author: Bruce Anderson
Author: James Bradbury
Author: Art DeGaetano
Author: Tara J. Troy
Author: David Wolfe

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