Contribution of precipitation events with different consecutive days to summer rainfall change over China
Abstract The climatological features, regional trends, and interdecadal changes of summer precipitation over China are investigated in this study from the perspective of four types of precipitation events with different consecutive days. The precipitation events are classified based on the consecuti...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
You, Ting [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2020 |
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| Schlagwörter: |
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| Systematik: |
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| Anmerkung: |
© Springer-Verlag GmbH Austria, part of Springer Nature 2020 |
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| Übergeordnetes Werk: |
Enthalten in: Theoretical and applied climatology - Springer Vienna, 1986, 141(2020), 3-4 vom: 13. Juni, Seite 1493-1510 |
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| Übergeordnetes Werk: |
volume:141 ; year:2020 ; number:3-4 ; day:13 ; month:06 ; pages:1493-1510 |
| Links: |
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| DOI / URN: |
10.1007/s00704-020-03290-5 |
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| Katalog-ID: |
OLC2118395396 |
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| 520 | |a Abstract The climatological features, regional trends, and interdecadal changes of summer precipitation over China are investigated in this study from the perspective of four types of precipitation events with different consecutive days. The precipitation events are classified based on the consecutive days of precipitation into 1-to-3-, 4-to-7-, 8-to-14-, and over-14-day events. The contribution of 1-to-3-day events to climatological precipitation is larger than the other events over central Asia. Longer duration events contributed more than the shorter duration events to precipitation in tropical regions. The positive precipitation trend in northwestern and southern China is mainly due to 4-to-7-day and 8-to-14-day events, respectively; and the negative precipitation trend in North China is largely related to 4-to-7-day events. In general, the frequency change of precipitation events is a major reason for the precipitation change of these events in the concerned regions. The precipitation decrease in northern China around the mid-1960s is attributed to the reduction in 4-to-7-day events. The precipitation increase in northeastern and central China in the late 1970s is due to a combination of increases in 4-to-7-day and 8-to-14-day events. The precipitation increase in southern China around 1993 is mainly contributed by over-14-day events. The precipitation decrease in the mid-latitude Asia is due to the decrease in 4-to-7-day events. Most of the interdecadal precipitation changes are related to decrease or increase in the activity of anomalous cyclones. Results suggest that the frequency of occurrence of cyclonic perturbations is a major factor for interdecadal changes in summer precipitation over China. | ||
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10.1007/s00704-020-03290-5 doi (DE-627)OLC2118395396 (DE-He213)s00704-020-03290-5-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk You, Ting verfasserin aut Contribution of precipitation events with different consecutive days to summer rainfall change over China 2020 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag GmbH Austria, part of Springer Nature 2020 Abstract The climatological features, regional trends, and interdecadal changes of summer precipitation over China are investigated in this study from the perspective of four types of precipitation events with different consecutive days. The precipitation events are classified based on the consecutive days of precipitation into 1-to-3-, 4-to-7-, 8-to-14-, and over-14-day events. The contribution of 1-to-3-day events to climatological precipitation is larger than the other events over central Asia. Longer duration events contributed more than the shorter duration events to precipitation in tropical regions. The positive precipitation trend in northwestern and southern China is mainly due to 4-to-7-day and 8-to-14-day events, respectively; and the negative precipitation trend in North China is largely related to 4-to-7-day events. In general, the frequency change of precipitation events is a major reason for the precipitation change of these events in the concerned regions. The precipitation decrease in northern China around the mid-1960s is attributed to the reduction in 4-to-7-day events. The precipitation increase in northeastern and central China in the late 1970s is due to a combination of increases in 4-to-7-day and 8-to-14-day events. The precipitation increase in southern China around 1993 is mainly contributed by over-14-day events. The precipitation decrease in the mid-latitude Asia is due to the decrease in 4-to-7-day events. Most of the interdecadal precipitation changes are related to decrease or increase in the activity of anomalous cyclones. Results suggest that the frequency of occurrence of cyclonic perturbations is a major factor for interdecadal changes in summer precipitation over China. Types of precipitation events Summer precipitation trends Interdecadal changes Frequency of precipitation events Wu, Renguang (orcid)0000-0003-4712-2251 aut Liu, Ge aut Chai, Zhaoyang aut Enthalten in Theoretical and applied climatology Springer Vienna, 1986 141(2020), 3-4 vom: 13. Juni, Seite 1493-1510 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:141 year:2020 number:3-4 day:13 month:06 pages:1493-1510 https://doi.org/10.1007/s00704-020-03290-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_4313 RA 1000 AR 141 2020 3-4 13 06 1493-1510 |
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10.1007/s00704-020-03290-5 doi (DE-627)OLC2118395396 (DE-He213)s00704-020-03290-5-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk You, Ting verfasserin aut Contribution of precipitation events with different consecutive days to summer rainfall change over China 2020 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag GmbH Austria, part of Springer Nature 2020 Abstract The climatological features, regional trends, and interdecadal changes of summer precipitation over China are investigated in this study from the perspective of four types of precipitation events with different consecutive days. The precipitation events are classified based on the consecutive days of precipitation into 1-to-3-, 4-to-7-, 8-to-14-, and over-14-day events. The contribution of 1-to-3-day events to climatological precipitation is larger than the other events over central Asia. Longer duration events contributed more than the shorter duration events to precipitation in tropical regions. The positive precipitation trend in northwestern and southern China is mainly due to 4-to-7-day and 8-to-14-day events, respectively; and the negative precipitation trend in North China is largely related to 4-to-7-day events. In general, the frequency change of precipitation events is a major reason for the precipitation change of these events in the concerned regions. The precipitation decrease in northern China around the mid-1960s is attributed to the reduction in 4-to-7-day events. The precipitation increase in northeastern and central China in the late 1970s is due to a combination of increases in 4-to-7-day and 8-to-14-day events. The precipitation increase in southern China around 1993 is mainly contributed by over-14-day events. The precipitation decrease in the mid-latitude Asia is due to the decrease in 4-to-7-day events. Most of the interdecadal precipitation changes are related to decrease or increase in the activity of anomalous cyclones. Results suggest that the frequency of occurrence of cyclonic perturbations is a major factor for interdecadal changes in summer precipitation over China. Types of precipitation events Summer precipitation trends Interdecadal changes Frequency of precipitation events Wu, Renguang (orcid)0000-0003-4712-2251 aut Liu, Ge aut Chai, Zhaoyang aut Enthalten in Theoretical and applied climatology Springer Vienna, 1986 141(2020), 3-4 vom: 13. Juni, Seite 1493-1510 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:141 year:2020 number:3-4 day:13 month:06 pages:1493-1510 https://doi.org/10.1007/s00704-020-03290-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_4313 RA 1000 AR 141 2020 3-4 13 06 1493-1510 |
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10.1007/s00704-020-03290-5 doi (DE-627)OLC2118395396 (DE-He213)s00704-020-03290-5-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk You, Ting verfasserin aut Contribution of precipitation events with different consecutive days to summer rainfall change over China 2020 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag GmbH Austria, part of Springer Nature 2020 Abstract The climatological features, regional trends, and interdecadal changes of summer precipitation over China are investigated in this study from the perspective of four types of precipitation events with different consecutive days. The precipitation events are classified based on the consecutive days of precipitation into 1-to-3-, 4-to-7-, 8-to-14-, and over-14-day events. The contribution of 1-to-3-day events to climatological precipitation is larger than the other events over central Asia. Longer duration events contributed more than the shorter duration events to precipitation in tropical regions. The positive precipitation trend in northwestern and southern China is mainly due to 4-to-7-day and 8-to-14-day events, respectively; and the negative precipitation trend in North China is largely related to 4-to-7-day events. In general, the frequency change of precipitation events is a major reason for the precipitation change of these events in the concerned regions. The precipitation decrease in northern China around the mid-1960s is attributed to the reduction in 4-to-7-day events. The precipitation increase in northeastern and central China in the late 1970s is due to a combination of increases in 4-to-7-day and 8-to-14-day events. The precipitation increase in southern China around 1993 is mainly contributed by over-14-day events. The precipitation decrease in the mid-latitude Asia is due to the decrease in 4-to-7-day events. Most of the interdecadal precipitation changes are related to decrease or increase in the activity of anomalous cyclones. Results suggest that the frequency of occurrence of cyclonic perturbations is a major factor for interdecadal changes in summer precipitation over China. Types of precipitation events Summer precipitation trends Interdecadal changes Frequency of precipitation events Wu, Renguang (orcid)0000-0003-4712-2251 aut Liu, Ge aut Chai, Zhaoyang aut Enthalten in Theoretical and applied climatology Springer Vienna, 1986 141(2020), 3-4 vom: 13. Juni, Seite 1493-1510 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:141 year:2020 number:3-4 day:13 month:06 pages:1493-1510 https://doi.org/10.1007/s00704-020-03290-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_4313 RA 1000 AR 141 2020 3-4 13 06 1493-1510 |
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10.1007/s00704-020-03290-5 doi (DE-627)OLC2118395396 (DE-He213)s00704-020-03290-5-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk You, Ting verfasserin aut Contribution of precipitation events with different consecutive days to summer rainfall change over China 2020 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag GmbH Austria, part of Springer Nature 2020 Abstract The climatological features, regional trends, and interdecadal changes of summer precipitation over China are investigated in this study from the perspective of four types of precipitation events with different consecutive days. The precipitation events are classified based on the consecutive days of precipitation into 1-to-3-, 4-to-7-, 8-to-14-, and over-14-day events. The contribution of 1-to-3-day events to climatological precipitation is larger than the other events over central Asia. Longer duration events contributed more than the shorter duration events to precipitation in tropical regions. The positive precipitation trend in northwestern and southern China is mainly due to 4-to-7-day and 8-to-14-day events, respectively; and the negative precipitation trend in North China is largely related to 4-to-7-day events. In general, the frequency change of precipitation events is a major reason for the precipitation change of these events in the concerned regions. The precipitation decrease in northern China around the mid-1960s is attributed to the reduction in 4-to-7-day events. The precipitation increase in northeastern and central China in the late 1970s is due to a combination of increases in 4-to-7-day and 8-to-14-day events. The precipitation increase in southern China around 1993 is mainly contributed by over-14-day events. The precipitation decrease in the mid-latitude Asia is due to the decrease in 4-to-7-day events. Most of the interdecadal precipitation changes are related to decrease or increase in the activity of anomalous cyclones. Results suggest that the frequency of occurrence of cyclonic perturbations is a major factor for interdecadal changes in summer precipitation over China. Types of precipitation events Summer precipitation trends Interdecadal changes Frequency of precipitation events Wu, Renguang (orcid)0000-0003-4712-2251 aut Liu, Ge aut Chai, Zhaoyang aut Enthalten in Theoretical and applied climatology Springer Vienna, 1986 141(2020), 3-4 vom: 13. Juni, Seite 1493-1510 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:141 year:2020 number:3-4 day:13 month:06 pages:1493-1510 https://doi.org/10.1007/s00704-020-03290-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_4313 RA 1000 AR 141 2020 3-4 13 06 1493-1510 |
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10.1007/s00704-020-03290-5 doi (DE-627)OLC2118395396 (DE-He213)s00704-020-03290-5-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk You, Ting verfasserin aut Contribution of precipitation events with different consecutive days to summer rainfall change over China 2020 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag GmbH Austria, part of Springer Nature 2020 Abstract The climatological features, regional trends, and interdecadal changes of summer precipitation over China are investigated in this study from the perspective of four types of precipitation events with different consecutive days. The precipitation events are classified based on the consecutive days of precipitation into 1-to-3-, 4-to-7-, 8-to-14-, and over-14-day events. The contribution of 1-to-3-day events to climatological precipitation is larger than the other events over central Asia. Longer duration events contributed more than the shorter duration events to precipitation in tropical regions. The positive precipitation trend in northwestern and southern China is mainly due to 4-to-7-day and 8-to-14-day events, respectively; and the negative precipitation trend in North China is largely related to 4-to-7-day events. In general, the frequency change of precipitation events is a major reason for the precipitation change of these events in the concerned regions. The precipitation decrease in northern China around the mid-1960s is attributed to the reduction in 4-to-7-day events. The precipitation increase in northeastern and central China in the late 1970s is due to a combination of increases in 4-to-7-day and 8-to-14-day events. The precipitation increase in southern China around 1993 is mainly contributed by over-14-day events. The precipitation decrease in the mid-latitude Asia is due to the decrease in 4-to-7-day events. Most of the interdecadal precipitation changes are related to decrease or increase in the activity of anomalous cyclones. Results suggest that the frequency of occurrence of cyclonic perturbations is a major factor for interdecadal changes in summer precipitation over China. Types of precipitation events Summer precipitation trends Interdecadal changes Frequency of precipitation events Wu, Renguang (orcid)0000-0003-4712-2251 aut Liu, Ge aut Chai, Zhaoyang aut Enthalten in Theoretical and applied climatology Springer Vienna, 1986 141(2020), 3-4 vom: 13. Juni, Seite 1493-1510 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:141 year:2020 number:3-4 day:13 month:06 pages:1493-1510 https://doi.org/10.1007/s00704-020-03290-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_4313 RA 1000 AR 141 2020 3-4 13 06 1493-1510 |
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550 VZ 14 ssgn RA 1000 VZ rvk Contribution of precipitation events with different consecutive days to summer rainfall change over China Types of precipitation events Summer precipitation trends Interdecadal changes Frequency of precipitation events |
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Contribution of precipitation events with different consecutive days to summer rainfall change over China |
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Contribution of precipitation events with different consecutive days to summer rainfall change over China |
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You, Ting |
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You, Ting Wu, Renguang Liu, Ge Chai, Zhaoyang |
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contribution of precipitation events with different consecutive days to summer rainfall change over china |
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Contribution of precipitation events with different consecutive days to summer rainfall change over China |
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Abstract The climatological features, regional trends, and interdecadal changes of summer precipitation over China are investigated in this study from the perspective of four types of precipitation events with different consecutive days. The precipitation events are classified based on the consecutive days of precipitation into 1-to-3-, 4-to-7-, 8-to-14-, and over-14-day events. The contribution of 1-to-3-day events to climatological precipitation is larger than the other events over central Asia. Longer duration events contributed more than the shorter duration events to precipitation in tropical regions. The positive precipitation trend in northwestern and southern China is mainly due to 4-to-7-day and 8-to-14-day events, respectively; and the negative precipitation trend in North China is largely related to 4-to-7-day events. In general, the frequency change of precipitation events is a major reason for the precipitation change of these events in the concerned regions. The precipitation decrease in northern China around the mid-1960s is attributed to the reduction in 4-to-7-day events. The precipitation increase in northeastern and central China in the late 1970s is due to a combination of increases in 4-to-7-day and 8-to-14-day events. The precipitation increase in southern China around 1993 is mainly contributed by over-14-day events. The precipitation decrease in the mid-latitude Asia is due to the decrease in 4-to-7-day events. Most of the interdecadal precipitation changes are related to decrease or increase in the activity of anomalous cyclones. Results suggest that the frequency of occurrence of cyclonic perturbations is a major factor for interdecadal changes in summer precipitation over China. © Springer-Verlag GmbH Austria, part of Springer Nature 2020 |
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Abstract The climatological features, regional trends, and interdecadal changes of summer precipitation over China are investigated in this study from the perspective of four types of precipitation events with different consecutive days. The precipitation events are classified based on the consecutive days of precipitation into 1-to-3-, 4-to-7-, 8-to-14-, and over-14-day events. The contribution of 1-to-3-day events to climatological precipitation is larger than the other events over central Asia. Longer duration events contributed more than the shorter duration events to precipitation in tropical regions. The positive precipitation trend in northwestern and southern China is mainly due to 4-to-7-day and 8-to-14-day events, respectively; and the negative precipitation trend in North China is largely related to 4-to-7-day events. In general, the frequency change of precipitation events is a major reason for the precipitation change of these events in the concerned regions. The precipitation decrease in northern China around the mid-1960s is attributed to the reduction in 4-to-7-day events. The precipitation increase in northeastern and central China in the late 1970s is due to a combination of increases in 4-to-7-day and 8-to-14-day events. The precipitation increase in southern China around 1993 is mainly contributed by over-14-day events. The precipitation decrease in the mid-latitude Asia is due to the decrease in 4-to-7-day events. Most of the interdecadal precipitation changes are related to decrease or increase in the activity of anomalous cyclones. Results suggest that the frequency of occurrence of cyclonic perturbations is a major factor for interdecadal changes in summer precipitation over China. © Springer-Verlag GmbH Austria, part of Springer Nature 2020 |
| abstract_unstemmed |
Abstract The climatological features, regional trends, and interdecadal changes of summer precipitation over China are investigated in this study from the perspective of four types of precipitation events with different consecutive days. The precipitation events are classified based on the consecutive days of precipitation into 1-to-3-, 4-to-7-, 8-to-14-, and over-14-day events. The contribution of 1-to-3-day events to climatological precipitation is larger than the other events over central Asia. Longer duration events contributed more than the shorter duration events to precipitation in tropical regions. The positive precipitation trend in northwestern and southern China is mainly due to 4-to-7-day and 8-to-14-day events, respectively; and the negative precipitation trend in North China is largely related to 4-to-7-day events. In general, the frequency change of precipitation events is a major reason for the precipitation change of these events in the concerned regions. The precipitation decrease in northern China around the mid-1960s is attributed to the reduction in 4-to-7-day events. The precipitation increase in northeastern and central China in the late 1970s is due to a combination of increases in 4-to-7-day and 8-to-14-day events. The precipitation increase in southern China around 1993 is mainly contributed by over-14-day events. The precipitation decrease in the mid-latitude Asia is due to the decrease in 4-to-7-day events. Most of the interdecadal precipitation changes are related to decrease or increase in the activity of anomalous cyclones. Results suggest that the frequency of occurrence of cyclonic perturbations is a major factor for interdecadal changes in summer precipitation over China. © Springer-Verlag GmbH Austria, part of Springer Nature 2020 |
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Contribution of precipitation events with different consecutive days to summer rainfall change over China |
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