Tracking regional temperature projections from the early 1990s in light of variations in regional warming, including ‘warming holes’

Abstract The perception of the accuracy of regional climate projections made in the early 1990s about climate change by 2030 may be influenced by how the temperature trend has changed in the 25 years since their publication. However, temperature trends over this period were influenced not only by ex...

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Main Authors: Michael R. Grose, James S. Risbey, Penny H. Whetton
Format: Article in Journal/Newspaper
Language:unknown
Subjects:
Online Access:http://link.springer.com/10.1007/s10584-016-1840-9
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spelling ftrepec:oai:RePEc:spr:climat:v:140:y:2017:i:2:d:10.1007_s10584-016-1840-9 2023-05-15T18:25:41+02:00 Tracking regional temperature projections from the early 1990s in light of variations in regional warming, including ‘warming holes’ Michael R. Grose James S. Risbey Penny H. Whetton http://link.springer.com/10.1007/s10584-016-1840-9 unknown http://link.springer.com/10.1007/s10584-016-1840-9 article ftrepec 2020-12-04T13:43:13Z Abstract The perception of the accuracy of regional climate projections made in the early 1990s about climate change by 2030 may be influenced by how the temperature trend has changed in the 25 years since their publication. However, temperature trends over this period were influenced not only by external forcings such as greenhouse gases but also natural variations. The temperature of Southern Australia, the Sahel, South Asia and Southern Europe are currently within the warming estimates from statements in the early 1990s from the IPCC and CSIRO, assuming a linear trend between 1990 and 2030. However, northern Australia and central North America are currently at the lower limit or below these projections, having featured areas of multi-year regional cooling during global warming, sometimes called ‘warming holes’. Recent climate model simulations suggest that cooling can be expected in the recent past and near future in some regions, including in Australia and the US, and that cooling is less likely over 1990–2030 than in 1990–2015, bringing observations closer to the IPCC and CSIRO warming estimates by 2030. Cooling at the 25-year scale in some regions can be associated with cyclic variability such as the Inter-decadal Pacific Oscillation, or low trend such as in the Southern Ocean. Explicitly communicating the variability in regional warming rates in climate projections, including the possibility of regional warming ‘holes’ (or the opposite of ‘surges’ or ‘peaks’) would help to set more reliable expectations by users of those projections. Regional climate change, Climate variability, Climate projections Article in Journal/Newspaper Southern Ocean RePEc (Research Papers in Economics) Pacific Southern Ocean
institution Open Polar
collection RePEc (Research Papers in Economics)
op_collection_id ftrepec
language unknown
description Abstract The perception of the accuracy of regional climate projections made in the early 1990s about climate change by 2030 may be influenced by how the temperature trend has changed in the 25 years since their publication. However, temperature trends over this period were influenced not only by external forcings such as greenhouse gases but also natural variations. The temperature of Southern Australia, the Sahel, South Asia and Southern Europe are currently within the warming estimates from statements in the early 1990s from the IPCC and CSIRO, assuming a linear trend between 1990 and 2030. However, northern Australia and central North America are currently at the lower limit or below these projections, having featured areas of multi-year regional cooling during global warming, sometimes called ‘warming holes’. Recent climate model simulations suggest that cooling can be expected in the recent past and near future in some regions, including in Australia and the US, and that cooling is less likely over 1990–2030 than in 1990–2015, bringing observations closer to the IPCC and CSIRO warming estimates by 2030. Cooling at the 25-year scale in some regions can be associated with cyclic variability such as the Inter-decadal Pacific Oscillation, or low trend such as in the Southern Ocean. Explicitly communicating the variability in regional warming rates in climate projections, including the possibility of regional warming ‘holes’ (or the opposite of ‘surges’ or ‘peaks’) would help to set more reliable expectations by users of those projections. Regional climate change, Climate variability, Climate projections
format Article in Journal/Newspaper
author Michael R. Grose
James S. Risbey
Penny H. Whetton
spellingShingle Michael R. Grose
James S. Risbey
Penny H. Whetton
Tracking regional temperature projections from the early 1990s in light of variations in regional warming, including ‘warming holes’
author_facet Michael R. Grose
James S. Risbey
Penny H. Whetton
author_sort Michael R. Grose
title Tracking regional temperature projections from the early 1990s in light of variations in regional warming, including ‘warming holes’
title_short Tracking regional temperature projections from the early 1990s in light of variations in regional warming, including ‘warming holes’
title_full Tracking regional temperature projections from the early 1990s in light of variations in regional warming, including ‘warming holes’
title_fullStr Tracking regional temperature projections from the early 1990s in light of variations in regional warming, including ‘warming holes’
title_full_unstemmed Tracking regional temperature projections from the early 1990s in light of variations in regional warming, including ‘warming holes’
title_sort tracking regional temperature projections from the early 1990s in light of variations in regional warming, including ‘warming holes’
url http://link.springer.com/10.1007/s10584-016-1840-9
geographic Pacific
Southern Ocean
geographic_facet Pacific
Southern Ocean
genre Southern Ocean
genre_facet Southern Ocean
op_relation http://link.springer.com/10.1007/s10584-016-1840-9
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