Comparative analysis of the extreme temperature event change over Northeast China and Hokkaido, Japan from 1951 to 2011
Abstract On the basis of the daily minimum (Tmin), mean (Tmean), and maximum (Tmax) temperature records of 25 meteorological stations in Northeast China (NEC) and 10 weather stations in Hokkaido, Japan (HKD), from 1951 to 2011, we comparatively analyzed the change in extreme temperature events and t...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Wang, Lei [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2015 |
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| Systematik: |
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| Anmerkung: |
© Springer-Verlag Wien 2015 |
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| Übergeordnetes Werk: |
Enthalten in: Theoretical and applied climatology - Springer Vienna, 1986, 124(2015), 1-2 vom: 14. März, Seite 375-384 |
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| Übergeordnetes Werk: |
volume:124 ; year:2015 ; number:1-2 ; day:14 ; month:03 ; pages:375-384 |
| Links: |
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| DOI / URN: |
10.1007/s00704-015-1425-y |
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OLC2048455816 |
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| 520 | |a Abstract On the basis of the daily minimum (Tmin), mean (Tmean), and maximum (Tmax) temperature records of 25 meteorological stations in Northeast China (NEC) and 10 weather stations in Hokkaido, Japan (HKD), from 1951 to 2011, we comparatively analyzed the change in extreme temperature events and the relationship of these events with the mean value. Results showed that for the extreme lowest temperature (ELT) frequency, approximately 96 % of the stations exhibited decreasing trends ranging from −0.63 to 0 days/decade in NEC, whereas all the stations in HKD showed decreasing trends ranging from −0.4 to 0 days/decade. However, the average decrease in amplitude of 0.24 days/decade in HKD was significantly less than the 0.27 days/decade average in NEC. The extreme highest temperature (EHT) frequency trends in the two regions showed insignificant increases. Notable decreasing trends for the ELT intensity were found at −0.9 to 0 %/decade in 92 % of the stations in NEC and −1.1 to 0 %/decade in 90 % of the stations in HKD. Inversely, increasing trends in EHT intensity were observed in 80 % of the stations over HKD, ranging from 0.06 to 0.32 %/decade, and the majority of the stations (64 %) showed increasing trends in NEC. Tmean and Tmin had strong negative correlations with the ELT intensity in NEC, whereas Tmean and Tmin had strong significant negative correlations with the ELT frequency in HKD. Tmin, Tmean, and Tmax between NEC and HKD exhibited strong significant positive correlations. The frequency and intensity of the ELT in both regions showed significant positive correlations. | ||
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10.1007/s00704-015-1425-y doi (DE-627)OLC2048455816 (DE-He213)s00704-015-1425-y-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Wang, Lei verfasserin aut Comparative analysis of the extreme temperature event change over Northeast China and Hokkaido, Japan from 1951 to 2011 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Wien 2015 Abstract On the basis of the daily minimum (Tmin), mean (Tmean), and maximum (Tmax) temperature records of 25 meteorological stations in Northeast China (NEC) and 10 weather stations in Hokkaido, Japan (HKD), from 1951 to 2011, we comparatively analyzed the change in extreme temperature events and the relationship of these events with the mean value. Results showed that for the extreme lowest temperature (ELT) frequency, approximately 96 % of the stations exhibited decreasing trends ranging from −0.63 to 0 days/decade in NEC, whereas all the stations in HKD showed decreasing trends ranging from −0.4 to 0 days/decade. However, the average decrease in amplitude of 0.24 days/decade in HKD was significantly less than the 0.27 days/decade average in NEC. The extreme highest temperature (EHT) frequency trends in the two regions showed insignificant increases. Notable decreasing trends for the ELT intensity were found at −0.9 to 0 %/decade in 92 % of the stations in NEC and −1.1 to 0 %/decade in 90 % of the stations in HKD. Inversely, increasing trends in EHT intensity were observed in 80 % of the stations over HKD, ranging from 0.06 to 0.32 %/decade, and the majority of the stations (64 %) showed increasing trends in NEC. Tmean and Tmin had strong negative correlations with the ELT intensity in NEC, whereas Tmean and Tmin had strong significant negative correlations with the ELT frequency in HKD. Tmin, Tmean, and Tmax between NEC and HKD exhibited strong significant positive correlations. The frequency and intensity of the ELT in both regions showed significant positive correlations. Extreme Temperature East Asian Summer Monsoon East Asian Monsoon Liaoning Province East Asian Winter Monsoon Wu, Zhengfang aut Wang, Fuxue aut Du, Haibo aut Zong, Shengwei aut Enthalten in Theoretical and applied climatology Springer Vienna, 1986 124(2015), 1-2 vom: 14. März, Seite 375-384 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:124 year:2015 number:1-2 day:14 month:03 pages:375-384 https://doi.org/10.1007/s00704-015-1425-y lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 GBV_ILN_4012 GBV_ILN_4313 RA 1000 AR 124 2015 1-2 14 03 375-384 |
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10.1007/s00704-015-1425-y doi (DE-627)OLC2048455816 (DE-He213)s00704-015-1425-y-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Wang, Lei verfasserin aut Comparative analysis of the extreme temperature event change over Northeast China and Hokkaido, Japan from 1951 to 2011 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Wien 2015 Abstract On the basis of the daily minimum (Tmin), mean (Tmean), and maximum (Tmax) temperature records of 25 meteorological stations in Northeast China (NEC) and 10 weather stations in Hokkaido, Japan (HKD), from 1951 to 2011, we comparatively analyzed the change in extreme temperature events and the relationship of these events with the mean value. Results showed that for the extreme lowest temperature (ELT) frequency, approximately 96 % of the stations exhibited decreasing trends ranging from −0.63 to 0 days/decade in NEC, whereas all the stations in HKD showed decreasing trends ranging from −0.4 to 0 days/decade. However, the average decrease in amplitude of 0.24 days/decade in HKD was significantly less than the 0.27 days/decade average in NEC. The extreme highest temperature (EHT) frequency trends in the two regions showed insignificant increases. Notable decreasing trends for the ELT intensity were found at −0.9 to 0 %/decade in 92 % of the stations in NEC and −1.1 to 0 %/decade in 90 % of the stations in HKD. Inversely, increasing trends in EHT intensity were observed in 80 % of the stations over HKD, ranging from 0.06 to 0.32 %/decade, and the majority of the stations (64 %) showed increasing trends in NEC. Tmean and Tmin had strong negative correlations with the ELT intensity in NEC, whereas Tmean and Tmin had strong significant negative correlations with the ELT frequency in HKD. Tmin, Tmean, and Tmax between NEC and HKD exhibited strong significant positive correlations. The frequency and intensity of the ELT in both regions showed significant positive correlations. Extreme Temperature East Asian Summer Monsoon East Asian Monsoon Liaoning Province East Asian Winter Monsoon Wu, Zhengfang aut Wang, Fuxue aut Du, Haibo aut Zong, Shengwei aut Enthalten in Theoretical and applied climatology Springer Vienna, 1986 124(2015), 1-2 vom: 14. März, Seite 375-384 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:124 year:2015 number:1-2 day:14 month:03 pages:375-384 https://doi.org/10.1007/s00704-015-1425-y lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 GBV_ILN_4012 GBV_ILN_4313 RA 1000 AR 124 2015 1-2 14 03 375-384 |
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10.1007/s00704-015-1425-y doi (DE-627)OLC2048455816 (DE-He213)s00704-015-1425-y-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Wang, Lei verfasserin aut Comparative analysis of the extreme temperature event change over Northeast China and Hokkaido, Japan from 1951 to 2011 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Wien 2015 Abstract On the basis of the daily minimum (Tmin), mean (Tmean), and maximum (Tmax) temperature records of 25 meteorological stations in Northeast China (NEC) and 10 weather stations in Hokkaido, Japan (HKD), from 1951 to 2011, we comparatively analyzed the change in extreme temperature events and the relationship of these events with the mean value. Results showed that for the extreme lowest temperature (ELT) frequency, approximately 96 % of the stations exhibited decreasing trends ranging from −0.63 to 0 days/decade in NEC, whereas all the stations in HKD showed decreasing trends ranging from −0.4 to 0 days/decade. However, the average decrease in amplitude of 0.24 days/decade in HKD was significantly less than the 0.27 days/decade average in NEC. The extreme highest temperature (EHT) frequency trends in the two regions showed insignificant increases. Notable decreasing trends for the ELT intensity were found at −0.9 to 0 %/decade in 92 % of the stations in NEC and −1.1 to 0 %/decade in 90 % of the stations in HKD. Inversely, increasing trends in EHT intensity were observed in 80 % of the stations over HKD, ranging from 0.06 to 0.32 %/decade, and the majority of the stations (64 %) showed increasing trends in NEC. Tmean and Tmin had strong negative correlations with the ELT intensity in NEC, whereas Tmean and Tmin had strong significant negative correlations with the ELT frequency in HKD. Tmin, Tmean, and Tmax between NEC and HKD exhibited strong significant positive correlations. The frequency and intensity of the ELT in both regions showed significant positive correlations. Extreme Temperature East Asian Summer Monsoon East Asian Monsoon Liaoning Province East Asian Winter Monsoon Wu, Zhengfang aut Wang, Fuxue aut Du, Haibo aut Zong, Shengwei aut Enthalten in Theoretical and applied climatology Springer Vienna, 1986 124(2015), 1-2 vom: 14. März, Seite 375-384 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:124 year:2015 number:1-2 day:14 month:03 pages:375-384 https://doi.org/10.1007/s00704-015-1425-y lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 GBV_ILN_4012 GBV_ILN_4313 RA 1000 AR 124 2015 1-2 14 03 375-384 |
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10.1007/s00704-015-1425-y doi (DE-627)OLC2048455816 (DE-He213)s00704-015-1425-y-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Wang, Lei verfasserin aut Comparative analysis of the extreme temperature event change over Northeast China and Hokkaido, Japan from 1951 to 2011 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Wien 2015 Abstract On the basis of the daily minimum (Tmin), mean (Tmean), and maximum (Tmax) temperature records of 25 meteorological stations in Northeast China (NEC) and 10 weather stations in Hokkaido, Japan (HKD), from 1951 to 2011, we comparatively analyzed the change in extreme temperature events and the relationship of these events with the mean value. Results showed that for the extreme lowest temperature (ELT) frequency, approximately 96 % of the stations exhibited decreasing trends ranging from −0.63 to 0 days/decade in NEC, whereas all the stations in HKD showed decreasing trends ranging from −0.4 to 0 days/decade. However, the average decrease in amplitude of 0.24 days/decade in HKD was significantly less than the 0.27 days/decade average in NEC. The extreme highest temperature (EHT) frequency trends in the two regions showed insignificant increases. Notable decreasing trends for the ELT intensity were found at −0.9 to 0 %/decade in 92 % of the stations in NEC and −1.1 to 0 %/decade in 90 % of the stations in HKD. Inversely, increasing trends in EHT intensity were observed in 80 % of the stations over HKD, ranging from 0.06 to 0.32 %/decade, and the majority of the stations (64 %) showed increasing trends in NEC. Tmean and Tmin had strong negative correlations with the ELT intensity in NEC, whereas Tmean and Tmin had strong significant negative correlations with the ELT frequency in HKD. Tmin, Tmean, and Tmax between NEC and HKD exhibited strong significant positive correlations. The frequency and intensity of the ELT in both regions showed significant positive correlations. Extreme Temperature East Asian Summer Monsoon East Asian Monsoon Liaoning Province East Asian Winter Monsoon Wu, Zhengfang aut Wang, Fuxue aut Du, Haibo aut Zong, Shengwei aut Enthalten in Theoretical and applied climatology Springer Vienna, 1986 124(2015), 1-2 vom: 14. März, Seite 375-384 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:124 year:2015 number:1-2 day:14 month:03 pages:375-384 https://doi.org/10.1007/s00704-015-1425-y lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 GBV_ILN_4012 GBV_ILN_4313 RA 1000 AR 124 2015 1-2 14 03 375-384 |
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comparative analysis of the extreme temperature event change over northeast china and hokkaido, japan from 1951 to 2011 |
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Comparative analysis of the extreme temperature event change over Northeast China and Hokkaido, Japan from 1951 to 2011 |
| abstract |
Abstract On the basis of the daily minimum (Tmin), mean (Tmean), and maximum (Tmax) temperature records of 25 meteorological stations in Northeast China (NEC) and 10 weather stations in Hokkaido, Japan (HKD), from 1951 to 2011, we comparatively analyzed the change in extreme temperature events and the relationship of these events with the mean value. Results showed that for the extreme lowest temperature (ELT) frequency, approximately 96 % of the stations exhibited decreasing trends ranging from −0.63 to 0 days/decade in NEC, whereas all the stations in HKD showed decreasing trends ranging from −0.4 to 0 days/decade. However, the average decrease in amplitude of 0.24 days/decade in HKD was significantly less than the 0.27 days/decade average in NEC. The extreme highest temperature (EHT) frequency trends in the two regions showed insignificant increases. Notable decreasing trends for the ELT intensity were found at −0.9 to 0 %/decade in 92 % of the stations in NEC and −1.1 to 0 %/decade in 90 % of the stations in HKD. Inversely, increasing trends in EHT intensity were observed in 80 % of the stations over HKD, ranging from 0.06 to 0.32 %/decade, and the majority of the stations (64 %) showed increasing trends in NEC. Tmean and Tmin had strong negative correlations with the ELT intensity in NEC, whereas Tmean and Tmin had strong significant negative correlations with the ELT frequency in HKD. Tmin, Tmean, and Tmax between NEC and HKD exhibited strong significant positive correlations. The frequency and intensity of the ELT in both regions showed significant positive correlations. © Springer-Verlag Wien 2015 |
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Abstract On the basis of the daily minimum (Tmin), mean (Tmean), and maximum (Tmax) temperature records of 25 meteorological stations in Northeast China (NEC) and 10 weather stations in Hokkaido, Japan (HKD), from 1951 to 2011, we comparatively analyzed the change in extreme temperature events and the relationship of these events with the mean value. Results showed that for the extreme lowest temperature (ELT) frequency, approximately 96 % of the stations exhibited decreasing trends ranging from −0.63 to 0 days/decade in NEC, whereas all the stations in HKD showed decreasing trends ranging from −0.4 to 0 days/decade. However, the average decrease in amplitude of 0.24 days/decade in HKD was significantly less than the 0.27 days/decade average in NEC. The extreme highest temperature (EHT) frequency trends in the two regions showed insignificant increases. Notable decreasing trends for the ELT intensity were found at −0.9 to 0 %/decade in 92 % of the stations in NEC and −1.1 to 0 %/decade in 90 % of the stations in HKD. Inversely, increasing trends in EHT intensity were observed in 80 % of the stations over HKD, ranging from 0.06 to 0.32 %/decade, and the majority of the stations (64 %) showed increasing trends in NEC. Tmean and Tmin had strong negative correlations with the ELT intensity in NEC, whereas Tmean and Tmin had strong significant negative correlations with the ELT frequency in HKD. Tmin, Tmean, and Tmax between NEC and HKD exhibited strong significant positive correlations. The frequency and intensity of the ELT in both regions showed significant positive correlations. © Springer-Verlag Wien 2015 |
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Abstract On the basis of the daily minimum (Tmin), mean (Tmean), and maximum (Tmax) temperature records of 25 meteorological stations in Northeast China (NEC) and 10 weather stations in Hokkaido, Japan (HKD), from 1951 to 2011, we comparatively analyzed the change in extreme temperature events and the relationship of these events with the mean value. Results showed that for the extreme lowest temperature (ELT) frequency, approximately 96 % of the stations exhibited decreasing trends ranging from −0.63 to 0 days/decade in NEC, whereas all the stations in HKD showed decreasing trends ranging from −0.4 to 0 days/decade. However, the average decrease in amplitude of 0.24 days/decade in HKD was significantly less than the 0.27 days/decade average in NEC. The extreme highest temperature (EHT) frequency trends in the two regions showed insignificant increases. Notable decreasing trends for the ELT intensity were found at −0.9 to 0 %/decade in 92 % of the stations in NEC and −1.1 to 0 %/decade in 90 % of the stations in HKD. Inversely, increasing trends in EHT intensity were observed in 80 % of the stations over HKD, ranging from 0.06 to 0.32 %/decade, and the majority of the stations (64 %) showed increasing trends in NEC. Tmean and Tmin had strong negative correlations with the ELT intensity in NEC, whereas Tmean and Tmin had strong significant negative correlations with the ELT frequency in HKD. Tmin, Tmean, and Tmax between NEC and HKD exhibited strong significant positive correlations. The frequency and intensity of the ELT in both regions showed significant positive correlations. © Springer-Verlag Wien 2015 |
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