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...
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Autor*in:	Wang, Lei [verfasserIn] Wu, Zhengfang [verfasserIn] Wang, Fuxue [verfasserIn] Du, Haibo [verfasserIn] Zong, Shengwei [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2015

Schlagwörter:	Extreme Temperature East Asian Summer Monsoon East Asian Monsoon Liaoning Province East Asian Winter Monsoon

Übergeordnetes Werk:	Enthalten in: Theoretical and applied climatology - Wien [u.a.] : Springer, 1948, 124(2015), 1-2 vom: 14. März, Seite 375-384
Übergeordnetes Werk:	volume:124 ; year:2015 ; number:1-2 ; day:14 ; month:03 ; pages:375-384

Links:	Volltext

DOI / URN:	10.1007/s00704-015-1425-y

Katalog-ID:	SPR007337892

Internformat


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245	1	0	\|a Comparative analysis of the extreme temperature event change over Northeast China and Hokkaido, Japan from 1951 to 2011
264		1	\|c 2015
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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.
650		4	\|a Extreme Temperature \|7 (dpeaa)DE-He213
650		4	\|a East Asian Summer Monsoon \|7 (dpeaa)DE-He213
650		4	\|a East Asian Monsoon \|7 (dpeaa)DE-He213
650		4	\|a Liaoning Province \|7 (dpeaa)DE-He213
650		4	\|a East Asian Winter Monsoon \|7 (dpeaa)DE-He213
700	1		\|a Wu, Zhengfang \|e verfasserin \|4 aut
700	1		\|a Wang, Fuxue \|e verfasserin \|4 aut
700	1		\|a Du, Haibo \|e verfasserin \|4 aut
700	1		\|a Zong, Shengwei \|e verfasserin \|4 aut
773	0	8	\|i Enthalten in \|t Theoretical and applied climatology \|d Wien [u.a.] : Springer, 1948 \|g 124(2015), 1-2 vom: 14. März, Seite 375-384 \|w (DE-627)25490968X \|w (DE-600)1463177-5 \|x 1434-4483 \|7 nnns
773	1	8	\|g volume:124 \|g year:2015 \|g number:1-2 \|g day:14 \|g month:03 \|g pages:375-384
856	4	0	\|u https://dx.doi.org/10.1007/s00704-015-1425-y \|z lizenzpflichtig \|3 Volltext
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912			\|a GBV_ILN_40
912			\|a GBV_ILN_60
912			\|a GBV_ILN_62
912			\|a GBV_ILN_63
912			\|a GBV_ILN_69
912			\|a GBV_ILN_70
912			\|a GBV_ILN_73
912			\|a GBV_ILN_74
912			\|a GBV_ILN_90
912			\|a GBV_ILN_95
912			\|a GBV_ILN_100
912			\|a GBV_ILN_105
912			\|a GBV_ILN_110
912			\|a GBV_ILN_120
912			\|a GBV_ILN_138
912			\|a GBV_ILN_150
912			\|a GBV_ILN_151
912			\|a GBV_ILN_152
912			\|a GBV_ILN_161
912			\|a GBV_ILN_170
912			\|a GBV_ILN_171
912			\|a GBV_ILN_187
912			\|a GBV_ILN_206
912			\|a GBV_ILN_213
912			\|a GBV_ILN_224
912			\|a GBV_ILN_230
912			\|a GBV_ILN_250
912			\|a GBV_ILN_267
912			\|a GBV_ILN_281
912			\|a GBV_ILN_285
912			\|a GBV_ILN_293
912			\|a GBV_ILN_370
912			\|a GBV_ILN_602
912			\|a GBV_ILN_636
912			\|a GBV_ILN_702
912			\|a GBV_ILN_2001
912			\|a GBV_ILN_2003
912			\|a GBV_ILN_2004
912			\|a GBV_ILN_2005
912			\|a GBV_ILN_2006
912			\|a GBV_ILN_2007
912			\|a GBV_ILN_2008
912			\|a GBV_ILN_2009
912			\|a GBV_ILN_2010
912			\|a GBV_ILN_2011
912			\|a GBV_ILN_2014
912			\|a GBV_ILN_2015
912			\|a GBV_ILN_2020
912			\|a GBV_ILN_2021
912			\|a GBV_ILN_2025
912			\|a GBV_ILN_2026
912			\|a GBV_ILN_2027
912			\|a GBV_ILN_2031
912			\|a GBV_ILN_2034
912			\|a GBV_ILN_2037
912			\|a GBV_ILN_2038
912			\|a GBV_ILN_2039
912			\|a GBV_ILN_2044
912			\|a GBV_ILN_2048
912			\|a GBV_ILN_2049
912			\|a GBV_ILN_2050
912			\|a GBV_ILN_2055
912			\|a GBV_ILN_2056
912			\|a GBV_ILN_2057
912			\|a GBV_ILN_2059
912			\|a GBV_ILN_2061
912			\|a GBV_ILN_2064
912			\|a GBV_ILN_2065
912			\|a GBV_ILN_2068
912			\|a GBV_ILN_2070
912			\|a GBV_ILN_2086
912			\|a GBV_ILN_2088
912			\|a GBV_ILN_2093
912			\|a GBV_ILN_2106
912			\|a GBV_ILN_2107
912			\|a GBV_ILN_2108
912			\|a GBV_ILN_2110
912			\|a GBV_ILN_2111
912			\|a GBV_ILN_2112
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912			\|a GBV_ILN_2336
912			\|a GBV_ILN_2446
912			\|a GBV_ILN_2470
912			\|a GBV_ILN_2472
912			\|a GBV_ILN_2507
912			\|a GBV_ILN_2522
912			\|a GBV_ILN_2548
912			\|a GBV_ILN_4012
912			\|a GBV_ILN_4035
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912			\|a GBV_ILN_4307
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912			\|a GBV_ILN_4323
912			\|a GBV_ILN_4324
912			\|a GBV_ILN_4325
912			\|a GBV_ILN_4326
912			\|a GBV_ILN_4328
912			\|a GBV_ILN_4333
912			\|a GBV_ILN_4334
912			\|a GBV_ILN_4335
912			\|a GBV_ILN_4336
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912			\|a GBV_ILN_4393
912			\|a GBV_ILN_4700
936	b	k	\|a 38.82 \|q ASE
951			\|a AR
952			\|d 124 \|j 2015 \|e 1-2 \|b 14 \|c 03 \|h 375-384

Indexfelder

author_variant	l w lw z w zw f w fw h d hd s z sz
matchkey_str	article:14344483:2015----::oprtvaayiotexrmtmeauevncagoenrhathnad
hierarchy_sort_str	2015
bklnumber	38.82
publishDate	2015
allfields	10.1007/s00704-015-1425-y doi (DE-627)SPR007337892 (SPR)s00704-015-1425-y-e DE-627 ger DE-627 rakwb eng 550 ASE 38.82 bkl 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 Computermedien c rdamedia Online-Ressource cr rdacarrier 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 (dpeaa)DE-He213 East Asian Summer Monsoon (dpeaa)DE-He213 East Asian Monsoon (dpeaa)DE-He213 Liaoning Province (dpeaa)DE-He213 East Asian Winter Monsoon (dpeaa)DE-He213 Wu, Zhengfang verfasserin aut Wang, Fuxue verfasserin aut Du, Haibo verfasserin aut Zong, Shengwei verfasserin aut Enthalten in Theoretical and applied climatology Wien [u.a.] : Springer, 1948 124(2015), 1-2 vom: 14. März, Seite 375-384 (DE-627)25490968X (DE-600)1463177-5 1434-4483 nnns volume:124 year:2015 number:1-2 day:14 month:03 pages:375-384 https://dx.doi.org/10.1007/s00704-015-1425-y lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GEO SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.82 ASE AR 124 2015 1-2 14 03 375-384
spelling	10.1007/s00704-015-1425-y doi (DE-627)SPR007337892 (SPR)s00704-015-1425-y-e DE-627 ger DE-627 rakwb eng 550 ASE 38.82 bkl 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 Computermedien c rdamedia Online-Ressource cr rdacarrier 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 (dpeaa)DE-He213 East Asian Summer Monsoon (dpeaa)DE-He213 East Asian Monsoon (dpeaa)DE-He213 Liaoning Province (dpeaa)DE-He213 East Asian Winter Monsoon (dpeaa)DE-He213 Wu, Zhengfang verfasserin aut Wang, Fuxue verfasserin aut Du, Haibo verfasserin aut Zong, Shengwei verfasserin aut Enthalten in Theoretical and applied climatology Wien [u.a.] : Springer, 1948 124(2015), 1-2 vom: 14. März, Seite 375-384 (DE-627)25490968X (DE-600)1463177-5 1434-4483 nnns volume:124 year:2015 number:1-2 day:14 month:03 pages:375-384 https://dx.doi.org/10.1007/s00704-015-1425-y lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GEO SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.82 ASE AR 124 2015 1-2 14 03 375-384
allfields_unstemmed	10.1007/s00704-015-1425-y doi (DE-627)SPR007337892 (SPR)s00704-015-1425-y-e DE-627 ger DE-627 rakwb eng 550 ASE 38.82 bkl 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 Computermedien c rdamedia Online-Ressource cr rdacarrier 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 (dpeaa)DE-He213 East Asian Summer Monsoon (dpeaa)DE-He213 East Asian Monsoon (dpeaa)DE-He213 Liaoning Province (dpeaa)DE-He213 East Asian Winter Monsoon (dpeaa)DE-He213 Wu, Zhengfang verfasserin aut Wang, Fuxue verfasserin aut Du, Haibo verfasserin aut Zong, Shengwei verfasserin aut Enthalten in Theoretical and applied climatology Wien [u.a.] : Springer, 1948 124(2015), 1-2 vom: 14. März, Seite 375-384 (DE-627)25490968X (DE-600)1463177-5 1434-4483 nnns volume:124 year:2015 number:1-2 day:14 month:03 pages:375-384 https://dx.doi.org/10.1007/s00704-015-1425-y lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GEO SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.82 ASE AR 124 2015 1-2 14 03 375-384
allfieldsGer	10.1007/s00704-015-1425-y doi (DE-627)SPR007337892 (SPR)s00704-015-1425-y-e DE-627 ger DE-627 rakwb eng 550 ASE 38.82 bkl 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 Computermedien c rdamedia Online-Ressource cr rdacarrier 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 (dpeaa)DE-He213 East Asian Summer Monsoon (dpeaa)DE-He213 East Asian Monsoon (dpeaa)DE-He213 Liaoning Province (dpeaa)DE-He213 East Asian Winter Monsoon (dpeaa)DE-He213 Wu, Zhengfang verfasserin aut Wang, Fuxue verfasserin aut Du, Haibo verfasserin aut Zong, Shengwei verfasserin aut Enthalten in Theoretical and applied climatology Wien [u.a.] : Springer, 1948 124(2015), 1-2 vom: 14. März, Seite 375-384 (DE-627)25490968X (DE-600)1463177-5 1434-4483 nnns volume:124 year:2015 number:1-2 day:14 month:03 pages:375-384 https://dx.doi.org/10.1007/s00704-015-1425-y lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GEO SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.82 ASE AR 124 2015 1-2 14 03 375-384
allfieldsSound	10.1007/s00704-015-1425-y doi (DE-627)SPR007337892 (SPR)s00704-015-1425-y-e DE-627 ger DE-627 rakwb eng 550 ASE 38.82 bkl 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 Computermedien c rdamedia Online-Ressource cr rdacarrier 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 (dpeaa)DE-He213 East Asian Summer Monsoon (dpeaa)DE-He213 East Asian Monsoon (dpeaa)DE-He213 Liaoning Province (dpeaa)DE-He213 East Asian Winter Monsoon (dpeaa)DE-He213 Wu, Zhengfang verfasserin aut Wang, Fuxue verfasserin aut Du, Haibo verfasserin aut Zong, Shengwei verfasserin aut Enthalten in Theoretical and applied climatology Wien [u.a.] : Springer, 1948 124(2015), 1-2 vom: 14. März, Seite 375-384 (DE-627)25490968X (DE-600)1463177-5 1434-4483 nnns volume:124 year:2015 number:1-2 day:14 month:03 pages:375-384 https://dx.doi.org/10.1007/s00704-015-1425-y lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GEO SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.82 ASE AR 124 2015 1-2 14 03 375-384
language	English
source	Enthalten in Theoretical and applied climatology 124(2015), 1-2 vom: 14. März, Seite 375-384 volume:124 year:2015 number:1-2 day:14 month:03 pages:375-384
sourceStr	Enthalten in Theoretical and applied climatology 124(2015), 1-2 vom: 14. März, Seite 375-384 volume:124 year:2015 number:1-2 day:14 month:03 pages:375-384
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Extreme Temperature East Asian Summer Monsoon East Asian Monsoon Liaoning Province East Asian Winter Monsoon
dewey-raw	550
isfreeaccess_bool	false
container_title	Theoretical and applied climatology
authorswithroles_txt_mv	Wang, Lei @@aut@@ Wu, Zhengfang @@aut@@ Wang, Fuxue @@aut@@ Du, Haibo @@aut@@ Zong, Shengwei @@aut@@
publishDateDaySort_date	2015-03-14T00:00:00Z
hierarchy_top_id	25490968X
dewey-sort	3550
id	SPR007337892
language_de	englisch
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author	Wang, Lei
spellingShingle	Wang, Lei ddc 550 bkl 38.82 misc Extreme Temperature misc East Asian Summer Monsoon misc East Asian Monsoon misc Liaoning Province misc East Asian Winter Monsoon Comparative analysis of the extreme temperature event change over Northeast China and Hokkaido, Japan from 1951 to 2011
authorStr	Wang, Lei
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topic_title	550 ASE 38.82 bkl Comparative analysis of the extreme temperature event change over Northeast China and Hokkaido, Japan from 1951 to 2011 Extreme Temperature (dpeaa)DE-He213 East Asian Summer Monsoon (dpeaa)DE-He213 East Asian Monsoon (dpeaa)DE-He213 Liaoning Province (dpeaa)DE-He213 East Asian Winter Monsoon (dpeaa)DE-He213
topic	ddc 550 bkl 38.82 misc Extreme Temperature misc East Asian Summer Monsoon misc East Asian Monsoon misc Liaoning Province misc East Asian Winter Monsoon
topic_unstemmed	ddc 550 bkl 38.82 misc Extreme Temperature misc East Asian Summer Monsoon misc East Asian Monsoon misc Liaoning Province misc East Asian Winter Monsoon
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title	Comparative analysis of the extreme temperature event change over Northeast China and Hokkaido, Japan from 1951 to 2011
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title_full	Comparative analysis of the extreme temperature event change over Northeast China and Hokkaido, Japan from 1951 to 2011
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journal	Theoretical and applied climatology
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author_browse	Wang, Lei Wu, Zhengfang Wang, Fuxue Du, Haibo Zong, Shengwei
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title_sort	comparative analysis of the extreme temperature event change over northeast china and hokkaido, japan from 1951 to 2011
title_auth	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.
abstractGer	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.
abstract_unstemmed	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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title_short	Comparative analysis of the extreme temperature event change over Northeast China and Hokkaido, Japan from 1951 to 2011
url	https://dx.doi.org/10.1007/s00704-015-1425-y
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author2	Wu, Zhengfang Wang, Fuxue Du, Haibo Zong, Shengwei
author2Str	Wu, Zhengfang Wang, Fuxue Du, Haibo Zong, Shengwei
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doi_str	10.1007/s00704-015-1425-y
up_date	2024-07-04T02:53:03.304Z
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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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