Decadal-to-Multidecadal Variability of Seasonal Land Precipitation in Northern Hemisphere in Observation and CMIP6 Historical Simulations

Based on the centennial-scale observations and CMIP6 historical simulations, this paper employs the ensemble empirical mode decomposition to extract the decadal-to-multidecadal variability of land precipitation (DMVLP) in the northern hemisphere. The spatial distributions of the dominant mode from t...

Full description

Bibliographic Details
Published in:Atmosphere
Main Authors: Hua Chen, Zhenchen Xu
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2020
Subjects:
Online Access:https://doi.org/10.3390/atmos11020195
_version_ 1821650446659354624
author Hua Chen
Zhenchen Xu
author_facet Hua Chen
Zhenchen Xu
author_sort Hua Chen
collection MDPI Open Access Publishing
container_issue 2
container_start_page 195
container_title Atmosphere
container_volume 11
description Based on the centennial-scale observations and CMIP6 historical simulations, this paper employs the ensemble empirical mode decomposition to extract the decadal-to-multidecadal variability of land precipitation (DMVLP) in the northern hemisphere. The spatial distributions of the dominant mode from the empirical orthogonal function are different in four seasons. Regions with the same sign of precipitation anomalies are likely to be teleconnected through oceanic forcing. The temporal evolutions of the leading modes are similar in winter and spring, with an amplitude increasing after the late 1970s, probably related to the overlap of oceanic multidecadal signals. In winter and spring, the Interdecadal Pacific Oscillation (IPO) and the Atlantic Multidecadal Oscillation (AMO) play a joint role. They were in phase before late 1970s and out of phase after then, weakening/strengthening the impacts of the North Pacific and North Atlantic on the DMVLP before/after late 1970s. In summer and autumn, AMO alone plays a part and the amplitude of time series does not vary as in winter and spring. The ability of the coupled models from CMIP6 historical simulations is also evaluated. The good-models average largely captures the spatial structure in four seasons and the associated oceanic signals. The poor-models average is hardly or weakly correlated with observation.
format Text
genre North Atlantic
genre_facet North Atlantic
geographic Pacific
geographic_facet Pacific
id ftmdpi:oai:mdpi.com:/2073-4433/11/2/195/
institution Open Polar
language English
op_collection_id ftmdpi
op_coverage agris
op_doi https://doi.org/10.3390/atmos11020195
op_relation Climatology
https://dx.doi.org/10.3390/atmos11020195
op_rights https://creativecommons.org/licenses/by/4.0/
op_source Atmosphere; Volume 11; Issue 2; Pages: 195
publishDate 2020
publisher Multidisciplinary Digital Publishing Institute
record_format openpolar
spelling ftmdpi:oai:mdpi.com:/2073-4433/11/2/195/ 2025-01-16T23:41:45+00:00 Decadal-to-Multidecadal Variability of Seasonal Land Precipitation in Northern Hemisphere in Observation and CMIP6 Historical Simulations Hua Chen Zhenchen Xu agris 2020-02-12 application/pdf https://doi.org/10.3390/atmos11020195 EN eng Multidisciplinary Digital Publishing Institute Climatology https://dx.doi.org/10.3390/atmos11020195 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 11; Issue 2; Pages: 195 decadal-to-multidecadal variability seasonal land precipitation CMIP6 historical simulations Text 2020 ftmdpi https://doi.org/10.3390/atmos11020195 2023-07-31T23:06:33Z Based on the centennial-scale observations and CMIP6 historical simulations, this paper employs the ensemble empirical mode decomposition to extract the decadal-to-multidecadal variability of land precipitation (DMVLP) in the northern hemisphere. The spatial distributions of the dominant mode from the empirical orthogonal function are different in four seasons. Regions with the same sign of precipitation anomalies are likely to be teleconnected through oceanic forcing. The temporal evolutions of the leading modes are similar in winter and spring, with an amplitude increasing after the late 1970s, probably related to the overlap of oceanic multidecadal signals. In winter and spring, the Interdecadal Pacific Oscillation (IPO) and the Atlantic Multidecadal Oscillation (AMO) play a joint role. They were in phase before late 1970s and out of phase after then, weakening/strengthening the impacts of the North Pacific and North Atlantic on the DMVLP before/after late 1970s. In summer and autumn, AMO alone plays a part and the amplitude of time series does not vary as in winter and spring. The ability of the coupled models from CMIP6 historical simulations is also evaluated. The good-models average largely captures the spatial structure in four seasons and the associated oceanic signals. The poor-models average is hardly or weakly correlated with observation. Text North Atlantic MDPI Open Access Publishing Pacific Atmosphere 11 2 195
spellingShingle decadal-to-multidecadal variability
seasonal land precipitation
CMIP6 historical simulations
Hua Chen
Zhenchen Xu
Decadal-to-Multidecadal Variability of Seasonal Land Precipitation in Northern Hemisphere in Observation and CMIP6 Historical Simulations
title Decadal-to-Multidecadal Variability of Seasonal Land Precipitation in Northern Hemisphere in Observation and CMIP6 Historical Simulations
title_full Decadal-to-Multidecadal Variability of Seasonal Land Precipitation in Northern Hemisphere in Observation and CMIP6 Historical Simulations
title_fullStr Decadal-to-Multidecadal Variability of Seasonal Land Precipitation in Northern Hemisphere in Observation and CMIP6 Historical Simulations
title_full_unstemmed Decadal-to-Multidecadal Variability of Seasonal Land Precipitation in Northern Hemisphere in Observation and CMIP6 Historical Simulations
title_short Decadal-to-Multidecadal Variability of Seasonal Land Precipitation in Northern Hemisphere in Observation and CMIP6 Historical Simulations
title_sort decadal-to-multidecadal variability of seasonal land precipitation in northern hemisphere in observation and cmip6 historical simulations
topic decadal-to-multidecadal variability
seasonal land precipitation
CMIP6 historical simulations
topic_facet decadal-to-multidecadal variability
seasonal land precipitation
CMIP6 historical simulations
url https://doi.org/10.3390/atmos11020195