Nonlinear characteristics of hydroclimate variability in the mid-latitude Asia over the past seven centuries
Abstract Hydroclimate variations in the mid-latitude Asia have received considerable attention due to its significance for the regional ecosystem and livelihood, while its nonlinear characteristics over the past centuries are not fully understood yet. Hydroclimate patterns for the mid-latitude Asia...
Ausführliche Beschreibung
Autor*in: |
Zhou, Feifei [verfasserIn] |
---|
Format: |
Artikel |
---|---|
Sprache: |
Englisch |
Erschienen: |
2015 |
---|
Schlagwörter: |
Ensemble Empirical Mode Decomposition |
---|
Systematik: |
|
---|
Anmerkung: |
© Springer-Verlag Wien 2015 |
---|
Übergeordnetes Werk: |
Enthalten in: Theoretical and applied climatology - Springer Vienna, 1986, 126(2015), 1-2 vom: 25. Juli, Seite 151-159 |
---|---|
Übergeordnetes Werk: |
volume:126 ; year:2015 ; number:1-2 ; day:25 ; month:07 ; pages:151-159 |
Links: |
---|
DOI / URN: |
10.1007/s00704-015-1565-0 |
---|
Katalog-ID: |
OLC2048457436 |
---|
LEADER | 01000caa a22002652 4500 | ||
---|---|---|---|
001 | OLC2048457436 | ||
003 | DE-627 | ||
005 | 20230502135840.0 | ||
007 | tu | ||
008 | 200820s2015 xx ||||| 00| ||eng c | ||
024 | 7 | |a 10.1007/s00704-015-1565-0 |2 doi | |
035 | |a (DE-627)OLC2048457436 | ||
035 | |a (DE-He213)s00704-015-1565-0-p | ||
040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
041 | |a eng | ||
082 | 0 | 4 | |a 550 |q VZ |
084 | |a 14 |2 ssgn | ||
084 | |a RA 1000 |q VZ |2 rvk | ||
100 | 1 | |a Zhou, Feifei |e verfasserin |4 aut | |
245 | 1 | 0 | |a Nonlinear characteristics of hydroclimate variability in the mid-latitude Asia over the past seven centuries |
264 | 1 | |c 2015 | |
336 | |a Text |b txt |2 rdacontent | ||
337 | |a ohne Hilfsmittel zu benutzen |b n |2 rdamedia | ||
338 | |a Band |b nc |2 rdacarrier | ||
500 | |a © Springer-Verlag Wien 2015 | ||
520 | |a Abstract Hydroclimate variations in the mid-latitude Asia have received considerable attention due to its significance for the regional ecosystem and livelihood, while its nonlinear characteristics over the past centuries are not fully understood yet. Hydroclimate patterns for the mid-latitude Asia are classified into eastern and western modes based on a network of the reconstructed Palmer drought severity index (PDSI) of 197 grids spanning since 1300. The hydroclimate variations of western mode are more complex than that of eastern mode based on the Higuchi’s fractal dimension (HFD) analysis, which may be related to the complex atmospheric circulation patterns that dominate them. The relationships of the hydroclimate variations between western and eastern modes at different time scales extracted by ensemble empirical mode decomposition method (EEMD) are detected. The anti-phase relationship of the hydroclimatic variations between western and eastern modes at the interdecadal variations occurs during the periods with the enhanced El Nino Southern Oscillation (ENSO) variance. Similarly, the multidecadal hydroclimate variations are anti-phase when the Pacific Decadal Oscillation (PDO) is in its warm phases. The inverse relationship between western and eastern modes is stable for the centennial scale. | ||
650 | 4 | |a Pacific Decadal Oscillation | |
650 | 4 | |a Palmer Drought Severity Index | |
650 | 4 | |a Ensemble Empirical Mode Decomposition | |
650 | 4 | |a Ensemble Empirical Mode Decomposition Method | |
650 | 4 | |a Hydroclimate Variation | |
700 | 1 | |a Fang, Keyan |4 aut | |
700 | 1 | |a Li, Yingjun |4 aut | |
700 | 1 | |a Chen, Qiuyan |4 aut | |
700 | 1 | |a Chen, Dan |4 aut | |
773 | 0 | 8 | |i Enthalten in |t Theoretical and applied climatology |d Springer Vienna, 1986 |g 126(2015), 1-2 vom: 25. Juli, Seite 151-159 |w (DE-627)129958808 |w (DE-600)405799-5 |w (DE-576)01552857X |x 0177-798X |7 nnns |
773 | 1 | 8 | |g volume:126 |g year:2015 |g number:1-2 |g day:25 |g month:07 |g pages:151-159 |
856 | 4 | 1 | |u https://doi.org/10.1007/s00704-015-1565-0 |z lizenzpflichtig |3 Volltext |
912 | |a GBV_USEFLAG_A | ||
912 | |a SYSFLAG_A | ||
912 | |a GBV_OLC | ||
912 | |a SSG-OLC-GEO | ||
912 | |a SSG-OPC-GGO | ||
912 | |a GBV_ILN_70 | ||
912 | |a GBV_ILN_4012 | ||
912 | |a GBV_ILN_4313 | ||
936 | r | v | |a RA 1000 |
951 | |a AR | ||
952 | |d 126 |j 2015 |e 1-2 |b 25 |c 07 |h 151-159 |
author_variant |
f z fz k f kf y l yl q c qc d c dc |
---|---|
matchkey_str |
article:0177798X:2015----::olnacaatrsisfyrciaeaibltiteilttdai |
hierarchy_sort_str |
2015 |
publishDate |
2015 |
allfields |
10.1007/s00704-015-1565-0 doi (DE-627)OLC2048457436 (DE-He213)s00704-015-1565-0-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Zhou, Feifei verfasserin aut Nonlinear characteristics of hydroclimate variability in the mid-latitude Asia over the past seven centuries 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Wien 2015 Abstract Hydroclimate variations in the mid-latitude Asia have received considerable attention due to its significance for the regional ecosystem and livelihood, while its nonlinear characteristics over the past centuries are not fully understood yet. Hydroclimate patterns for the mid-latitude Asia are classified into eastern and western modes based on a network of the reconstructed Palmer drought severity index (PDSI) of 197 grids spanning since 1300. The hydroclimate variations of western mode are more complex than that of eastern mode based on the Higuchi’s fractal dimension (HFD) analysis, which may be related to the complex atmospheric circulation patterns that dominate them. The relationships of the hydroclimate variations between western and eastern modes at different time scales extracted by ensemble empirical mode decomposition method (EEMD) are detected. The anti-phase relationship of the hydroclimatic variations between western and eastern modes at the interdecadal variations occurs during the periods with the enhanced El Nino Southern Oscillation (ENSO) variance. Similarly, the multidecadal hydroclimate variations are anti-phase when the Pacific Decadal Oscillation (PDO) is in its warm phases. The inverse relationship between western and eastern modes is stable for the centennial scale. Pacific Decadal Oscillation Palmer Drought Severity Index Ensemble Empirical Mode Decomposition Ensemble Empirical Mode Decomposition Method Hydroclimate Variation Fang, Keyan aut Li, Yingjun aut Chen, Qiuyan aut Chen, Dan aut Enthalten in Theoretical and applied climatology Springer Vienna, 1986 126(2015), 1-2 vom: 25. Juli, Seite 151-159 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:126 year:2015 number:1-2 day:25 month:07 pages:151-159 https://doi.org/10.1007/s00704-015-1565-0 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 126 2015 1-2 25 07 151-159 |
spelling |
10.1007/s00704-015-1565-0 doi (DE-627)OLC2048457436 (DE-He213)s00704-015-1565-0-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Zhou, Feifei verfasserin aut Nonlinear characteristics of hydroclimate variability in the mid-latitude Asia over the past seven centuries 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Wien 2015 Abstract Hydroclimate variations in the mid-latitude Asia have received considerable attention due to its significance for the regional ecosystem and livelihood, while its nonlinear characteristics over the past centuries are not fully understood yet. Hydroclimate patterns for the mid-latitude Asia are classified into eastern and western modes based on a network of the reconstructed Palmer drought severity index (PDSI) of 197 grids spanning since 1300. The hydroclimate variations of western mode are more complex than that of eastern mode based on the Higuchi’s fractal dimension (HFD) analysis, which may be related to the complex atmospheric circulation patterns that dominate them. The relationships of the hydroclimate variations between western and eastern modes at different time scales extracted by ensemble empirical mode decomposition method (EEMD) are detected. The anti-phase relationship of the hydroclimatic variations between western and eastern modes at the interdecadal variations occurs during the periods with the enhanced El Nino Southern Oscillation (ENSO) variance. Similarly, the multidecadal hydroclimate variations are anti-phase when the Pacific Decadal Oscillation (PDO) is in its warm phases. The inverse relationship between western and eastern modes is stable for the centennial scale. Pacific Decadal Oscillation Palmer Drought Severity Index Ensemble Empirical Mode Decomposition Ensemble Empirical Mode Decomposition Method Hydroclimate Variation Fang, Keyan aut Li, Yingjun aut Chen, Qiuyan aut Chen, Dan aut Enthalten in Theoretical and applied climatology Springer Vienna, 1986 126(2015), 1-2 vom: 25. Juli, Seite 151-159 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:126 year:2015 number:1-2 day:25 month:07 pages:151-159 https://doi.org/10.1007/s00704-015-1565-0 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 126 2015 1-2 25 07 151-159 |
allfields_unstemmed |
10.1007/s00704-015-1565-0 doi (DE-627)OLC2048457436 (DE-He213)s00704-015-1565-0-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Zhou, Feifei verfasserin aut Nonlinear characteristics of hydroclimate variability in the mid-latitude Asia over the past seven centuries 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Wien 2015 Abstract Hydroclimate variations in the mid-latitude Asia have received considerable attention due to its significance for the regional ecosystem and livelihood, while its nonlinear characteristics over the past centuries are not fully understood yet. Hydroclimate patterns for the mid-latitude Asia are classified into eastern and western modes based on a network of the reconstructed Palmer drought severity index (PDSI) of 197 grids spanning since 1300. The hydroclimate variations of western mode are more complex than that of eastern mode based on the Higuchi’s fractal dimension (HFD) analysis, which may be related to the complex atmospheric circulation patterns that dominate them. The relationships of the hydroclimate variations between western and eastern modes at different time scales extracted by ensemble empirical mode decomposition method (EEMD) are detected. The anti-phase relationship of the hydroclimatic variations between western and eastern modes at the interdecadal variations occurs during the periods with the enhanced El Nino Southern Oscillation (ENSO) variance. Similarly, the multidecadal hydroclimate variations are anti-phase when the Pacific Decadal Oscillation (PDO) is in its warm phases. The inverse relationship between western and eastern modes is stable for the centennial scale. Pacific Decadal Oscillation Palmer Drought Severity Index Ensemble Empirical Mode Decomposition Ensemble Empirical Mode Decomposition Method Hydroclimate Variation Fang, Keyan aut Li, Yingjun aut Chen, Qiuyan aut Chen, Dan aut Enthalten in Theoretical and applied climatology Springer Vienna, 1986 126(2015), 1-2 vom: 25. Juli, Seite 151-159 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:126 year:2015 number:1-2 day:25 month:07 pages:151-159 https://doi.org/10.1007/s00704-015-1565-0 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 126 2015 1-2 25 07 151-159 |
allfieldsGer |
10.1007/s00704-015-1565-0 doi (DE-627)OLC2048457436 (DE-He213)s00704-015-1565-0-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Zhou, Feifei verfasserin aut Nonlinear characteristics of hydroclimate variability in the mid-latitude Asia over the past seven centuries 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Wien 2015 Abstract Hydroclimate variations in the mid-latitude Asia have received considerable attention due to its significance for the regional ecosystem and livelihood, while its nonlinear characteristics over the past centuries are not fully understood yet. Hydroclimate patterns for the mid-latitude Asia are classified into eastern and western modes based on a network of the reconstructed Palmer drought severity index (PDSI) of 197 grids spanning since 1300. The hydroclimate variations of western mode are more complex than that of eastern mode based on the Higuchi’s fractal dimension (HFD) analysis, which may be related to the complex atmospheric circulation patterns that dominate them. The relationships of the hydroclimate variations between western and eastern modes at different time scales extracted by ensemble empirical mode decomposition method (EEMD) are detected. The anti-phase relationship of the hydroclimatic variations between western and eastern modes at the interdecadal variations occurs during the periods with the enhanced El Nino Southern Oscillation (ENSO) variance. Similarly, the multidecadal hydroclimate variations are anti-phase when the Pacific Decadal Oscillation (PDO) is in its warm phases. The inverse relationship between western and eastern modes is stable for the centennial scale. Pacific Decadal Oscillation Palmer Drought Severity Index Ensemble Empirical Mode Decomposition Ensemble Empirical Mode Decomposition Method Hydroclimate Variation Fang, Keyan aut Li, Yingjun aut Chen, Qiuyan aut Chen, Dan aut Enthalten in Theoretical and applied climatology Springer Vienna, 1986 126(2015), 1-2 vom: 25. Juli, Seite 151-159 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:126 year:2015 number:1-2 day:25 month:07 pages:151-159 https://doi.org/10.1007/s00704-015-1565-0 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 126 2015 1-2 25 07 151-159 |
allfieldsSound |
10.1007/s00704-015-1565-0 doi (DE-627)OLC2048457436 (DE-He213)s00704-015-1565-0-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Zhou, Feifei verfasserin aut Nonlinear characteristics of hydroclimate variability in the mid-latitude Asia over the past seven centuries 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Wien 2015 Abstract Hydroclimate variations in the mid-latitude Asia have received considerable attention due to its significance for the regional ecosystem and livelihood, while its nonlinear characteristics over the past centuries are not fully understood yet. Hydroclimate patterns for the mid-latitude Asia are classified into eastern and western modes based on a network of the reconstructed Palmer drought severity index (PDSI) of 197 grids spanning since 1300. The hydroclimate variations of western mode are more complex than that of eastern mode based on the Higuchi’s fractal dimension (HFD) analysis, which may be related to the complex atmospheric circulation patterns that dominate them. The relationships of the hydroclimate variations between western and eastern modes at different time scales extracted by ensemble empirical mode decomposition method (EEMD) are detected. The anti-phase relationship of the hydroclimatic variations between western and eastern modes at the interdecadal variations occurs during the periods with the enhanced El Nino Southern Oscillation (ENSO) variance. Similarly, the multidecadal hydroclimate variations are anti-phase when the Pacific Decadal Oscillation (PDO) is in its warm phases. The inverse relationship between western and eastern modes is stable for the centennial scale. Pacific Decadal Oscillation Palmer Drought Severity Index Ensemble Empirical Mode Decomposition Ensemble Empirical Mode Decomposition Method Hydroclimate Variation Fang, Keyan aut Li, Yingjun aut Chen, Qiuyan aut Chen, Dan aut Enthalten in Theoretical and applied climatology Springer Vienna, 1986 126(2015), 1-2 vom: 25. Juli, Seite 151-159 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:126 year:2015 number:1-2 day:25 month:07 pages:151-159 https://doi.org/10.1007/s00704-015-1565-0 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 126 2015 1-2 25 07 151-159 |
language |
English |
source |
Enthalten in Theoretical and applied climatology 126(2015), 1-2 vom: 25. Juli, Seite 151-159 volume:126 year:2015 number:1-2 day:25 month:07 pages:151-159 |
sourceStr |
Enthalten in Theoretical and applied climatology 126(2015), 1-2 vom: 25. Juli, Seite 151-159 volume:126 year:2015 number:1-2 day:25 month:07 pages:151-159 |
format_phy_str_mv |
Article |
institution |
findex.gbv.de |
topic_facet |
Pacific Decadal Oscillation Palmer Drought Severity Index Ensemble Empirical Mode Decomposition Ensemble Empirical Mode Decomposition Method Hydroclimate Variation |
dewey-raw |
550 |
isfreeaccess_bool |
false |
container_title |
Theoretical and applied climatology |
authorswithroles_txt_mv |
Zhou, Feifei @@aut@@ Fang, Keyan @@aut@@ Li, Yingjun @@aut@@ Chen, Qiuyan @@aut@@ Chen, Dan @@aut@@ |
publishDateDaySort_date |
2015-07-25T00:00:00Z |
hierarchy_top_id |
129958808 |
dewey-sort |
3550 |
id |
OLC2048457436 |
language_de |
englisch |
fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2048457436</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230502135840.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200820s2015 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s00704-015-1565-0</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2048457436</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)s00704-015-1565-0-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">14</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">RA 1000</subfield><subfield code="q">VZ</subfield><subfield code="2">rvk</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Zhou, Feifei</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Nonlinear characteristics of hydroclimate variability in the mid-latitude Asia over the past seven centuries</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2015</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Springer-Verlag Wien 2015</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Hydroclimate variations in the mid-latitude Asia have received considerable attention due to its significance for the regional ecosystem and livelihood, while its nonlinear characteristics over the past centuries are not fully understood yet. Hydroclimate patterns for the mid-latitude Asia are classified into eastern and western modes based on a network of the reconstructed Palmer drought severity index (PDSI) of 197 grids spanning since 1300. The hydroclimate variations of western mode are more complex than that of eastern mode based on the Higuchi’s fractal dimension (HFD) analysis, which may be related to the complex atmospheric circulation patterns that dominate them. The relationships of the hydroclimate variations between western and eastern modes at different time scales extracted by ensemble empirical mode decomposition method (EEMD) are detected. The anti-phase relationship of the hydroclimatic variations between western and eastern modes at the interdecadal variations occurs during the periods with the enhanced El Nino Southern Oscillation (ENSO) variance. Similarly, the multidecadal hydroclimate variations are anti-phase when the Pacific Decadal Oscillation (PDO) is in its warm phases. The inverse relationship between western and eastern modes is stable for the centennial scale.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Pacific Decadal Oscillation</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Palmer Drought Severity Index</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Ensemble Empirical Mode Decomposition</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Ensemble Empirical Mode Decomposition Method</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Hydroclimate Variation</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Fang, Keyan</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Li, Yingjun</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Chen, Qiuyan</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Chen, Dan</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Theoretical and applied climatology</subfield><subfield code="d">Springer Vienna, 1986</subfield><subfield code="g">126(2015), 1-2 vom: 25. Juli, Seite 151-159</subfield><subfield code="w">(DE-627)129958808</subfield><subfield code="w">(DE-600)405799-5</subfield><subfield code="w">(DE-576)01552857X</subfield><subfield code="x">0177-798X</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:126</subfield><subfield code="g">year:2015</subfield><subfield code="g">number:1-2</subfield><subfield code="g">day:25</subfield><subfield code="g">month:07</subfield><subfield code="g">pages:151-159</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/s00704-015-1565-0</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4012</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4313</subfield></datafield><datafield tag="936" ind1="r" ind2="v"><subfield code="a">RA 1000</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">126</subfield><subfield code="j">2015</subfield><subfield code="e">1-2</subfield><subfield code="b">25</subfield><subfield code="c">07</subfield><subfield code="h">151-159</subfield></datafield></record></collection>
|
author |
Zhou, Feifei |
spellingShingle |
Zhou, Feifei ddc 550 ssgn 14 rvk RA 1000 misc Pacific Decadal Oscillation misc Palmer Drought Severity Index misc Ensemble Empirical Mode Decomposition misc Ensemble Empirical Mode Decomposition Method misc Hydroclimate Variation Nonlinear characteristics of hydroclimate variability in the mid-latitude Asia over the past seven centuries |
authorStr |
Zhou, Feifei |
ppnlink_with_tag_str_mv |
@@773@@(DE-627)129958808 |
format |
Article |
dewey-ones |
550 - Earth sciences |
delete_txt_mv |
keep |
author_role |
aut aut aut aut aut |
collection |
OLC |
remote_str |
false |
illustrated |
Not Illustrated |
issn |
0177-798X |
topic_title |
550 VZ 14 ssgn RA 1000 VZ rvk Nonlinear characteristics of hydroclimate variability in the mid-latitude Asia over the past seven centuries Pacific Decadal Oscillation Palmer Drought Severity Index Ensemble Empirical Mode Decomposition Ensemble Empirical Mode Decomposition Method Hydroclimate Variation |
topic |
ddc 550 ssgn 14 rvk RA 1000 misc Pacific Decadal Oscillation misc Palmer Drought Severity Index misc Ensemble Empirical Mode Decomposition misc Ensemble Empirical Mode Decomposition Method misc Hydroclimate Variation |
topic_unstemmed |
ddc 550 ssgn 14 rvk RA 1000 misc Pacific Decadal Oscillation misc Palmer Drought Severity Index misc Ensemble Empirical Mode Decomposition misc Ensemble Empirical Mode Decomposition Method misc Hydroclimate Variation |
topic_browse |
ddc 550 ssgn 14 rvk RA 1000 misc Pacific Decadal Oscillation misc Palmer Drought Severity Index misc Ensemble Empirical Mode Decomposition misc Ensemble Empirical Mode Decomposition Method misc Hydroclimate Variation |
format_facet |
Aufsätze Gedruckte Aufsätze |
format_main_str_mv |
Text Zeitschrift/Artikel |
carriertype_str_mv |
nc |
hierarchy_parent_title |
Theoretical and applied climatology |
hierarchy_parent_id |
129958808 |
dewey-tens |
550 - Earth sciences & geology |
hierarchy_top_title |
Theoretical and applied climatology |
isfreeaccess_txt |
false |
familylinks_str_mv |
(DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X |
title |
Nonlinear characteristics of hydroclimate variability in the mid-latitude Asia over the past seven centuries |
ctrlnum |
(DE-627)OLC2048457436 (DE-He213)s00704-015-1565-0-p |
title_full |
Nonlinear characteristics of hydroclimate variability in the mid-latitude Asia over the past seven centuries |
author_sort |
Zhou, Feifei |
journal |
Theoretical and applied climatology |
journalStr |
Theoretical and applied climatology |
lang_code |
eng |
isOA_bool |
false |
dewey-hundreds |
500 - Science |
recordtype |
marc |
publishDateSort |
2015 |
contenttype_str_mv |
txt |
container_start_page |
151 |
author_browse |
Zhou, Feifei Fang, Keyan Li, Yingjun Chen, Qiuyan Chen, Dan |
container_volume |
126 |
class |
550 VZ 14 ssgn RA 1000 VZ rvk |
format_se |
Aufsätze |
author-letter |
Zhou, Feifei |
doi_str_mv |
10.1007/s00704-015-1565-0 |
dewey-full |
550 |
title_sort |
nonlinear characteristics of hydroclimate variability in the mid-latitude asia over the past seven centuries |
title_auth |
Nonlinear characteristics of hydroclimate variability in the mid-latitude Asia over the past seven centuries |
abstract |
Abstract Hydroclimate variations in the mid-latitude Asia have received considerable attention due to its significance for the regional ecosystem and livelihood, while its nonlinear characteristics over the past centuries are not fully understood yet. Hydroclimate patterns for the mid-latitude Asia are classified into eastern and western modes based on a network of the reconstructed Palmer drought severity index (PDSI) of 197 grids spanning since 1300. The hydroclimate variations of western mode are more complex than that of eastern mode based on the Higuchi’s fractal dimension (HFD) analysis, which may be related to the complex atmospheric circulation patterns that dominate them. The relationships of the hydroclimate variations between western and eastern modes at different time scales extracted by ensemble empirical mode decomposition method (EEMD) are detected. The anti-phase relationship of the hydroclimatic variations between western and eastern modes at the interdecadal variations occurs during the periods with the enhanced El Nino Southern Oscillation (ENSO) variance. Similarly, the multidecadal hydroclimate variations are anti-phase when the Pacific Decadal Oscillation (PDO) is in its warm phases. The inverse relationship between western and eastern modes is stable for the centennial scale. © Springer-Verlag Wien 2015 |
abstractGer |
Abstract Hydroclimate variations in the mid-latitude Asia have received considerable attention due to its significance for the regional ecosystem and livelihood, while its nonlinear characteristics over the past centuries are not fully understood yet. Hydroclimate patterns for the mid-latitude Asia are classified into eastern and western modes based on a network of the reconstructed Palmer drought severity index (PDSI) of 197 grids spanning since 1300. The hydroclimate variations of western mode are more complex than that of eastern mode based on the Higuchi’s fractal dimension (HFD) analysis, which may be related to the complex atmospheric circulation patterns that dominate them. The relationships of the hydroclimate variations between western and eastern modes at different time scales extracted by ensemble empirical mode decomposition method (EEMD) are detected. The anti-phase relationship of the hydroclimatic variations between western and eastern modes at the interdecadal variations occurs during the periods with the enhanced El Nino Southern Oscillation (ENSO) variance. Similarly, the multidecadal hydroclimate variations are anti-phase when the Pacific Decadal Oscillation (PDO) is in its warm phases. The inverse relationship between western and eastern modes is stable for the centennial scale. © Springer-Verlag Wien 2015 |
abstract_unstemmed |
Abstract Hydroclimate variations in the mid-latitude Asia have received considerable attention due to its significance for the regional ecosystem and livelihood, while its nonlinear characteristics over the past centuries are not fully understood yet. Hydroclimate patterns for the mid-latitude Asia are classified into eastern and western modes based on a network of the reconstructed Palmer drought severity index (PDSI) of 197 grids spanning since 1300. The hydroclimate variations of western mode are more complex than that of eastern mode based on the Higuchi’s fractal dimension (HFD) analysis, which may be related to the complex atmospheric circulation patterns that dominate them. The relationships of the hydroclimate variations between western and eastern modes at different time scales extracted by ensemble empirical mode decomposition method (EEMD) are detected. The anti-phase relationship of the hydroclimatic variations between western and eastern modes at the interdecadal variations occurs during the periods with the enhanced El Nino Southern Oscillation (ENSO) variance. Similarly, the multidecadal hydroclimate variations are anti-phase when the Pacific Decadal Oscillation (PDO) is in its warm phases. The inverse relationship between western and eastern modes is stable for the centennial scale. © Springer-Verlag Wien 2015 |
collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 GBV_ILN_4012 GBV_ILN_4313 |
container_issue |
1-2 |
title_short |
Nonlinear characteristics of hydroclimate variability in the mid-latitude Asia over the past seven centuries |
url |
https://doi.org/10.1007/s00704-015-1565-0 |
remote_bool |
false |
author2 |
Fang, Keyan Li, Yingjun Chen, Qiuyan Chen, Dan |
author2Str |
Fang, Keyan Li, Yingjun Chen, Qiuyan Chen, Dan |
ppnlink |
129958808 |
mediatype_str_mv |
n |
isOA_txt |
false |
hochschulschrift_bool |
false |
doi_str |
10.1007/s00704-015-1565-0 |
up_date |
2024-07-03T18:48:53.084Z |
_version_ |
1803584833414234112 |
fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2048457436</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230502135840.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200820s2015 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s00704-015-1565-0</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2048457436</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)s00704-015-1565-0-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">14</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">RA 1000</subfield><subfield code="q">VZ</subfield><subfield code="2">rvk</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Zhou, Feifei</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Nonlinear characteristics of hydroclimate variability in the mid-latitude Asia over the past seven centuries</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2015</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Springer-Verlag Wien 2015</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Hydroclimate variations in the mid-latitude Asia have received considerable attention due to its significance for the regional ecosystem and livelihood, while its nonlinear characteristics over the past centuries are not fully understood yet. Hydroclimate patterns for the mid-latitude Asia are classified into eastern and western modes based on a network of the reconstructed Palmer drought severity index (PDSI) of 197 grids spanning since 1300. The hydroclimate variations of western mode are more complex than that of eastern mode based on the Higuchi’s fractal dimension (HFD) analysis, which may be related to the complex atmospheric circulation patterns that dominate them. The relationships of the hydroclimate variations between western and eastern modes at different time scales extracted by ensemble empirical mode decomposition method (EEMD) are detected. The anti-phase relationship of the hydroclimatic variations between western and eastern modes at the interdecadal variations occurs during the periods with the enhanced El Nino Southern Oscillation (ENSO) variance. Similarly, the multidecadal hydroclimate variations are anti-phase when the Pacific Decadal Oscillation (PDO) is in its warm phases. The inverse relationship between western and eastern modes is stable for the centennial scale.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Pacific Decadal Oscillation</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Palmer Drought Severity Index</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Ensemble Empirical Mode Decomposition</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Ensemble Empirical Mode Decomposition Method</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Hydroclimate Variation</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Fang, Keyan</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Li, Yingjun</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Chen, Qiuyan</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Chen, Dan</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Theoretical and applied climatology</subfield><subfield code="d">Springer Vienna, 1986</subfield><subfield code="g">126(2015), 1-2 vom: 25. Juli, Seite 151-159</subfield><subfield code="w">(DE-627)129958808</subfield><subfield code="w">(DE-600)405799-5</subfield><subfield code="w">(DE-576)01552857X</subfield><subfield code="x">0177-798X</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:126</subfield><subfield code="g">year:2015</subfield><subfield code="g">number:1-2</subfield><subfield code="g">day:25</subfield><subfield code="g">month:07</subfield><subfield code="g">pages:151-159</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/s00704-015-1565-0</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4012</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4313</subfield></datafield><datafield tag="936" ind1="r" ind2="v"><subfield code="a">RA 1000</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">126</subfield><subfield code="j">2015</subfield><subfield code="e">1-2</subfield><subfield code="b">25</subfield><subfield code="c">07</subfield><subfield code="h">151-159</subfield></datafield></record></collection>
|
score |
7.399641 |