Empirical Prediction of Short‐Term Annual Global Temperature Variability

Abstract Global mean surface air temperature (Tglobal) variability on subdecadal timescales can be of substantial magnitude relative to the long‐term global warming signal, and such variability has been associated with considerable environmental and societal impacts. Therefore, probabilistic forekno...

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Main Authors: Patrick T. Brown, Ken Caldeira
Format: Article
Language:English
Published: American Geophysical Union (AGU) 2020-06-01
Series:Earth and Space Science
Subjects:
Online Access:https://doi.org/10.1029/2020EA001116
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spelling doaj-1a4935123f724fd2bdd5dba7972b3b5b2020-11-25T03:10:15ZengAmerican Geophysical Union (AGU)Earth and Space Science2333-50842020-06-0176n/an/a10.1029/2020EA001116Empirical Prediction of Short‐Term Annual Global Temperature VariabilityPatrick T. Brown0Ken Caldeira1Department of Meteorology and Climate Science San Jose State University San Jose CA USADepartment of Global Ecology Carnegie Institution for Science Stanford CA USAAbstract Global mean surface air temperature (Tglobal) variability on subdecadal timescales can be of substantial magnitude relative to the long‐term global warming signal, and such variability has been associated with considerable environmental and societal impacts. Therefore, probabilistic foreknowledge of short‐term Tglobal evolution may be of value for anticipating and mitigating some course‐resolution climate‐related risks. Here we present a simple, empirically based methodology that utilizes only global spatial patterns of annual mean surface air temperature anomalies to predict subsequent annual Tglobal anomalies via partial least squares regression. The method's skill is primarily achieved via information on the state of long‐term global warming as well as the state and recent evolution of the El Niño–Southern Oscillation and the Interdecadal Pacific Oscillation. We test the out‐of‐sample skill of the methodology using cross validation and in a forecast mode where statistical predictions are made precisely as they would have been if the procedure had been operationalized starting in the year 2000. The average forecast errors for lead times of 1 to 4 years are smaller than naïve benchmarks on average, and they perform favorably relative to most dynamical Global Climate Models retrospectively initialized to the observed state of the climate system. Thus, this method can be used as a computationally efficient benchmark for dynamical model forecast systems.https://doi.org/10.1029/2020EA001116Statistical forecastingGlobal temperature variabilityGlobal WarmingEl NinoGlobal Climate ModelsTeleconnections
collection DOAJ
language English
format Article
sources DOAJ
author Patrick T. Brown
Ken Caldeira
spellingShingle Patrick T. Brown
Ken Caldeira
Empirical Prediction of Short‐Term Annual Global Temperature Variability
Earth and Space Science
Statistical forecasting
Global temperature variability
Global Warming
El Nino
Global Climate Models
Teleconnections
author_facet Patrick T. Brown
Ken Caldeira
author_sort Patrick T. Brown
title Empirical Prediction of Short‐Term Annual Global Temperature Variability
title_short Empirical Prediction of Short‐Term Annual Global Temperature Variability
title_full Empirical Prediction of Short‐Term Annual Global Temperature Variability
title_fullStr Empirical Prediction of Short‐Term Annual Global Temperature Variability
title_full_unstemmed Empirical Prediction of Short‐Term Annual Global Temperature Variability
title_sort empirical prediction of short‐term annual global temperature variability
publisher American Geophysical Union (AGU)
series Earth and Space Science
issn 2333-5084
publishDate 2020-06-01
description Abstract Global mean surface air temperature (Tglobal) variability on subdecadal timescales can be of substantial magnitude relative to the long‐term global warming signal, and such variability has been associated with considerable environmental and societal impacts. Therefore, probabilistic foreknowledge of short‐term Tglobal evolution may be of value for anticipating and mitigating some course‐resolution climate‐related risks. Here we present a simple, empirically based methodology that utilizes only global spatial patterns of annual mean surface air temperature anomalies to predict subsequent annual Tglobal anomalies via partial least squares regression. The method's skill is primarily achieved via information on the state of long‐term global warming as well as the state and recent evolution of the El Niño–Southern Oscillation and the Interdecadal Pacific Oscillation. We test the out‐of‐sample skill of the methodology using cross validation and in a forecast mode where statistical predictions are made precisely as they would have been if the procedure had been operationalized starting in the year 2000. The average forecast errors for lead times of 1 to 4 years are smaller than naïve benchmarks on average, and they perform favorably relative to most dynamical Global Climate Models retrospectively initialized to the observed state of the climate system. Thus, this method can be used as a computationally efficient benchmark for dynamical model forecast systems.
topic Statistical forecasting
Global temperature variability
Global Warming
El Nino
Global Climate Models
Teleconnections
url https://doi.org/10.1029/2020EA001116
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