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...
Published in: | Atmosphere |
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Main Authors: | , |
Format: | Text |
Language: | English |
Published: |
Multidisciplinary Digital Publishing Institute
2020
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Subjects: | |
Online Access: | https://doi.org/10.3390/atmos11020195 |
_version_ | 1821650446659354624 |
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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 |