Relationship between the Northern Pacific Gyre Oscillation and tree-ring cellulose oxygen isotopes in northeastern Japan

Abstract The North Pacific Gyre Oscillation (NPGO) significantly imprints on hydrological fluctuations of the East Asian summer monsoon (EASM) region, but this has not yet been observed in proxy-based hydroclimate reconstructions. This study reports a tree-ring cellulose oxygen isotope ($ δ^{18} $O)...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Sakashita, Wataru [verfasserIn] Miyahara, Hiroko Yokoyama, Yusuke Aze, Takahiro Obrochta, Stephen P. Nakatsuka, Takeshi

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2017

Schlagwörter:	Tree-ring Oxygen isotope Northeastern Japan North Pacific Gyre Oscillation North Pacific Oscillation

Anmerkung:	© The Author(s) 2017

Übergeordnetes Werk:	Enthalten in: Geoscience Letters - Berlin : SpringerOpen, 2014, 4(2017), 1 vom: 12. Dez.
Übergeordnetes Werk:	volume:4 ; year:2017 ; number:1 ; day:12 ; month:12

Links:	Volltext

DOI / URN:	10.1186/s40562-017-0095-2

Katalog-ID:	SPR036666181

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520			\|a Abstract The North Pacific Gyre Oscillation (NPGO) significantly imprints on hydrological fluctuations of the East Asian summer monsoon (EASM) region, but this has not yet been observed in proxy-based hydroclimate reconstructions. This study reports a tree-ring cellulose oxygen isotope ($ δ^{18} $O) record from northeastern Japan spanning A.D. 1927–2010, overlapping with instrumental data, which we analyzed to determine if tree-ring $ δ^{18} $O in northeastern Japan records a signal consistent with the NPGO. Our results indicate that the tree-ring $ δ^{18} $O has a significant negative correlation with May–June (MJ) precipitation, as well as with short-term MJ relative humidity variation. Time-lagged temporal-domain comparisons indicate that the tree-ring $ δ^{18} $O is significantly correlated with the following year March–April (MA) and MJ NPGO index before the North Pacific climate transition in the late 1980s, particularly on decadal timescales. These relationships between our tree-ring $ δ^{18} $O and the climate patterns in the North Pacific are consistent with the actual early-summer precipitation. Spatial spring and early-summer sea-surface temperature anomalies exhibit a NPGO-like pattern in the following year. Spatial early-summer sea-level pressure anomalies also indicate North Pacific Oscillation (NPO) like patterns in the western North Pacific. These results suggest a lagged response of the NPGO to the EASM climate changes, and tree-ring $ δ^{18} $O in northeast Japan has a potential linkage with NPGO index from winter to early summer of the following year.
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allfields	10.1186/s40562-017-0095-2 doi (DE-627)SPR036666181 (SPR)s40562-017-0095-2-e DE-627 ger DE-627 rakwb eng Sakashita, Wataru verfasserin aut Relationship between the Northern Pacific Gyre Oscillation and tree-ring cellulose oxygen isotopes in northeastern Japan 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2017 Abstract The North Pacific Gyre Oscillation (NPGO) significantly imprints on hydrological fluctuations of the East Asian summer monsoon (EASM) region, but this has not yet been observed in proxy-based hydroclimate reconstructions. This study reports a tree-ring cellulose oxygen isotope ($ δ^{18} $O) record from northeastern Japan spanning A.D. 1927–2010, overlapping with instrumental data, which we analyzed to determine if tree-ring $ δ^{18} $O in northeastern Japan records a signal consistent with the NPGO. Our results indicate that the tree-ring $ δ^{18} $O has a significant negative correlation with May–June (MJ) precipitation, as well as with short-term MJ relative humidity variation. Time-lagged temporal-domain comparisons indicate that the tree-ring $ δ^{18} $O is significantly correlated with the following year March–April (MA) and MJ NPGO index before the North Pacific climate transition in the late 1980s, particularly on decadal timescales. These relationships between our tree-ring $ δ^{18} $O and the climate patterns in the North Pacific are consistent with the actual early-summer precipitation. Spatial spring and early-summer sea-surface temperature anomalies exhibit a NPGO-like pattern in the following year. Spatial early-summer sea-level pressure anomalies also indicate North Pacific Oscillation (NPO) like patterns in the western North Pacific. These results suggest a lagged response of the NPGO to the EASM climate changes, and tree-ring $ δ^{18} $O in northeast Japan has a potential linkage with NPGO index from winter to early summer of the following year. Tree-ring (dpeaa)DE-He213 Oxygen isotope (dpeaa)DE-He213 Northeastern Japan (dpeaa)DE-He213 North Pacific Gyre Oscillation (dpeaa)DE-He213 North Pacific Oscillation (dpeaa)DE-He213 Miyahara, Hiroko aut Yokoyama, Yusuke aut Aze, Takahiro aut Obrochta, Stephen P. aut Nakatsuka, Takeshi aut Enthalten in Geoscience Letters Berlin : SpringerOpen, 2014 4(2017), 1 vom: 12. Dez. (DE-627)780381343 (DE-600)2760757-4 2196-4092 nnns volume:4 year:2017 number:1 day:12 month:12 https://dx.doi.org/10.1186/s40562-017-0095-2 kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 4 2017 1 12 12
spelling	10.1186/s40562-017-0095-2 doi (DE-627)SPR036666181 (SPR)s40562-017-0095-2-e DE-627 ger DE-627 rakwb eng Sakashita, Wataru verfasserin aut Relationship between the Northern Pacific Gyre Oscillation and tree-ring cellulose oxygen isotopes in northeastern Japan 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2017 Abstract The North Pacific Gyre Oscillation (NPGO) significantly imprints on hydrological fluctuations of the East Asian summer monsoon (EASM) region, but this has not yet been observed in proxy-based hydroclimate reconstructions. This study reports a tree-ring cellulose oxygen isotope ($ δ^{18} $O) record from northeastern Japan spanning A.D. 1927–2010, overlapping with instrumental data, which we analyzed to determine if tree-ring $ δ^{18} $O in northeastern Japan records a signal consistent with the NPGO. Our results indicate that the tree-ring $ δ^{18} $O has a significant negative correlation with May–June (MJ) precipitation, as well as with short-term MJ relative humidity variation. Time-lagged temporal-domain comparisons indicate that the tree-ring $ δ^{18} $O is significantly correlated with the following year March–April (MA) and MJ NPGO index before the North Pacific climate transition in the late 1980s, particularly on decadal timescales. These relationships between our tree-ring $ δ^{18} $O and the climate patterns in the North Pacific are consistent with the actual early-summer precipitation. Spatial spring and early-summer sea-surface temperature anomalies exhibit a NPGO-like pattern in the following year. Spatial early-summer sea-level pressure anomalies also indicate North Pacific Oscillation (NPO) like patterns in the western North Pacific. These results suggest a lagged response of the NPGO to the EASM climate changes, and tree-ring $ δ^{18} $O in northeast Japan has a potential linkage with NPGO index from winter to early summer of the following year. Tree-ring (dpeaa)DE-He213 Oxygen isotope (dpeaa)DE-He213 Northeastern Japan (dpeaa)DE-He213 North Pacific Gyre Oscillation (dpeaa)DE-He213 North Pacific Oscillation (dpeaa)DE-He213 Miyahara, Hiroko aut Yokoyama, Yusuke aut Aze, Takahiro aut Obrochta, Stephen P. aut Nakatsuka, Takeshi aut Enthalten in Geoscience Letters Berlin : SpringerOpen, 2014 4(2017), 1 vom: 12. Dez. (DE-627)780381343 (DE-600)2760757-4 2196-4092 nnns volume:4 year:2017 number:1 day:12 month:12 https://dx.doi.org/10.1186/s40562-017-0095-2 kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 4 2017 1 12 12
allfields_unstemmed	10.1186/s40562-017-0095-2 doi (DE-627)SPR036666181 (SPR)s40562-017-0095-2-e DE-627 ger DE-627 rakwb eng Sakashita, Wataru verfasserin aut Relationship between the Northern Pacific Gyre Oscillation and tree-ring cellulose oxygen isotopes in northeastern Japan 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2017 Abstract The North Pacific Gyre Oscillation (NPGO) significantly imprints on hydrological fluctuations of the East Asian summer monsoon (EASM) region, but this has not yet been observed in proxy-based hydroclimate reconstructions. This study reports a tree-ring cellulose oxygen isotope ($ δ^{18} $O) record from northeastern Japan spanning A.D. 1927–2010, overlapping with instrumental data, which we analyzed to determine if tree-ring $ δ^{18} $O in northeastern Japan records a signal consistent with the NPGO. Our results indicate that the tree-ring $ δ^{18} $O has a significant negative correlation with May–June (MJ) precipitation, as well as with short-term MJ relative humidity variation. Time-lagged temporal-domain comparisons indicate that the tree-ring $ δ^{18} $O is significantly correlated with the following year March–April (MA) and MJ NPGO index before the North Pacific climate transition in the late 1980s, particularly on decadal timescales. These relationships between our tree-ring $ δ^{18} $O and the climate patterns in the North Pacific are consistent with the actual early-summer precipitation. Spatial spring and early-summer sea-surface temperature anomalies exhibit a NPGO-like pattern in the following year. Spatial early-summer sea-level pressure anomalies also indicate North Pacific Oscillation (NPO) like patterns in the western North Pacific. These results suggest a lagged response of the NPGO to the EASM climate changes, and tree-ring $ δ^{18} $O in northeast Japan has a potential linkage with NPGO index from winter to early summer of the following year. Tree-ring (dpeaa)DE-He213 Oxygen isotope (dpeaa)DE-He213 Northeastern Japan (dpeaa)DE-He213 North Pacific Gyre Oscillation (dpeaa)DE-He213 North Pacific Oscillation (dpeaa)DE-He213 Miyahara, Hiroko aut Yokoyama, Yusuke aut Aze, Takahiro aut Obrochta, Stephen P. aut Nakatsuka, Takeshi aut Enthalten in Geoscience Letters Berlin : SpringerOpen, 2014 4(2017), 1 vom: 12. Dez. (DE-627)780381343 (DE-600)2760757-4 2196-4092 nnns volume:4 year:2017 number:1 day:12 month:12 https://dx.doi.org/10.1186/s40562-017-0095-2 kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 4 2017 1 12 12
allfieldsGer	10.1186/s40562-017-0095-2 doi (DE-627)SPR036666181 (SPR)s40562-017-0095-2-e DE-627 ger DE-627 rakwb eng Sakashita, Wataru verfasserin aut Relationship between the Northern Pacific Gyre Oscillation and tree-ring cellulose oxygen isotopes in northeastern Japan 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2017 Abstract The North Pacific Gyre Oscillation (NPGO) significantly imprints on hydrological fluctuations of the East Asian summer monsoon (EASM) region, but this has not yet been observed in proxy-based hydroclimate reconstructions. This study reports a tree-ring cellulose oxygen isotope ($ δ^{18} $O) record from northeastern Japan spanning A.D. 1927–2010, overlapping with instrumental data, which we analyzed to determine if tree-ring $ δ^{18} $O in northeastern Japan records a signal consistent with the NPGO. Our results indicate that the tree-ring $ δ^{18} $O has a significant negative correlation with May–June (MJ) precipitation, as well as with short-term MJ relative humidity variation. Time-lagged temporal-domain comparisons indicate that the tree-ring $ δ^{18} $O is significantly correlated with the following year March–April (MA) and MJ NPGO index before the North Pacific climate transition in the late 1980s, particularly on decadal timescales. These relationships between our tree-ring $ δ^{18} $O and the climate patterns in the North Pacific are consistent with the actual early-summer precipitation. Spatial spring and early-summer sea-surface temperature anomalies exhibit a NPGO-like pattern in the following year. Spatial early-summer sea-level pressure anomalies also indicate North Pacific Oscillation (NPO) like patterns in the western North Pacific. These results suggest a lagged response of the NPGO to the EASM climate changes, and tree-ring $ δ^{18} $O in northeast Japan has a potential linkage with NPGO index from winter to early summer of the following year. Tree-ring (dpeaa)DE-He213 Oxygen isotope (dpeaa)DE-He213 Northeastern Japan (dpeaa)DE-He213 North Pacific Gyre Oscillation (dpeaa)DE-He213 North Pacific Oscillation (dpeaa)DE-He213 Miyahara, Hiroko aut Yokoyama, Yusuke aut Aze, Takahiro aut Obrochta, Stephen P. aut Nakatsuka, Takeshi aut Enthalten in Geoscience Letters Berlin : SpringerOpen, 2014 4(2017), 1 vom: 12. Dez. (DE-627)780381343 (DE-600)2760757-4 2196-4092 nnns volume:4 year:2017 number:1 day:12 month:12 https://dx.doi.org/10.1186/s40562-017-0095-2 kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 4 2017 1 12 12
allfieldsSound	10.1186/s40562-017-0095-2 doi (DE-627)SPR036666181 (SPR)s40562-017-0095-2-e DE-627 ger DE-627 rakwb eng Sakashita, Wataru verfasserin aut Relationship between the Northern Pacific Gyre Oscillation and tree-ring cellulose oxygen isotopes in northeastern Japan 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2017 Abstract The North Pacific Gyre Oscillation (NPGO) significantly imprints on hydrological fluctuations of the East Asian summer monsoon (EASM) region, but this has not yet been observed in proxy-based hydroclimate reconstructions. This study reports a tree-ring cellulose oxygen isotope ($ δ^{18} $O) record from northeastern Japan spanning A.D. 1927–2010, overlapping with instrumental data, which we analyzed to determine if tree-ring $ δ^{18} $O in northeastern Japan records a signal consistent with the NPGO. Our results indicate that the tree-ring $ δ^{18} $O has a significant negative correlation with May–June (MJ) precipitation, as well as with short-term MJ relative humidity variation. Time-lagged temporal-domain comparisons indicate that the tree-ring $ δ^{18} $O is significantly correlated with the following year March–April (MA) and MJ NPGO index before the North Pacific climate transition in the late 1980s, particularly on decadal timescales. These relationships between our tree-ring $ δ^{18} $O and the climate patterns in the North Pacific are consistent with the actual early-summer precipitation. Spatial spring and early-summer sea-surface temperature anomalies exhibit a NPGO-like pattern in the following year. Spatial early-summer sea-level pressure anomalies also indicate North Pacific Oscillation (NPO) like patterns in the western North Pacific. These results suggest a lagged response of the NPGO to the EASM climate changes, and tree-ring $ δ^{18} $O in northeast Japan has a potential linkage with NPGO index from winter to early summer of the following year. Tree-ring (dpeaa)DE-He213 Oxygen isotope (dpeaa)DE-He213 Northeastern Japan (dpeaa)DE-He213 North Pacific Gyre Oscillation (dpeaa)DE-He213 North Pacific Oscillation (dpeaa)DE-He213 Miyahara, Hiroko aut Yokoyama, Yusuke aut Aze, Takahiro aut Obrochta, Stephen P. aut Nakatsuka, Takeshi aut Enthalten in Geoscience Letters Berlin : SpringerOpen, 2014 4(2017), 1 vom: 12. Dez. (DE-627)780381343 (DE-600)2760757-4 2196-4092 nnns volume:4 year:2017 number:1 day:12 month:12 https://dx.doi.org/10.1186/s40562-017-0095-2 kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4338 GBV_ILN_4367 GBV_ILN_4700 AR 4 2017 1 12 12
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source	Enthalten in Geoscience Letters 4(2017), 1 vom: 12. Dez. volume:4 year:2017 number:1 day:12 month:12
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author	Sakashita, Wataru
spellingShingle	Sakashita, Wataru misc Tree-ring misc Oxygen isotope misc Northeastern Japan misc North Pacific Gyre Oscillation misc North Pacific Oscillation Relationship between the Northern Pacific Gyre Oscillation and tree-ring cellulose oxygen isotopes in northeastern Japan
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topic_title	Relationship between the Northern Pacific Gyre Oscillation and tree-ring cellulose oxygen isotopes in northeastern Japan Tree-ring (dpeaa)DE-He213 Oxygen isotope (dpeaa)DE-He213 Northeastern Japan (dpeaa)DE-He213 North Pacific Gyre Oscillation (dpeaa)DE-He213 North Pacific Oscillation (dpeaa)DE-He213
topic	misc Tree-ring misc Oxygen isotope misc Northeastern Japan misc North Pacific Gyre Oscillation misc North Pacific Oscillation
topic_unstemmed	misc Tree-ring misc Oxygen isotope misc Northeastern Japan misc North Pacific Gyre Oscillation misc North Pacific Oscillation
topic_browse	misc Tree-ring misc Oxygen isotope misc Northeastern Japan misc North Pacific Gyre Oscillation misc North Pacific Oscillation
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title	Relationship between the Northern Pacific Gyre Oscillation and tree-ring cellulose oxygen isotopes in northeastern Japan
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title_full	Relationship between the Northern Pacific Gyre Oscillation and tree-ring cellulose oxygen isotopes in northeastern Japan
author_sort	Sakashita, Wataru
journal	Geoscience Letters
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author_browse	Sakashita, Wataru Miyahara, Hiroko Yokoyama, Yusuke Aze, Takahiro Obrochta, Stephen P. Nakatsuka, Takeshi
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title_sort	relationship between the northern pacific gyre oscillation and tree-ring cellulose oxygen isotopes in northeastern japan
title_auth	Relationship between the Northern Pacific Gyre Oscillation and tree-ring cellulose oxygen isotopes in northeastern Japan
abstract	Abstract The North Pacific Gyre Oscillation (NPGO) significantly imprints on hydrological fluctuations of the East Asian summer monsoon (EASM) region, but this has not yet been observed in proxy-based hydroclimate reconstructions. This study reports a tree-ring cellulose oxygen isotope ($ δ^{18} $O) record from northeastern Japan spanning A.D. 1927–2010, overlapping with instrumental data, which we analyzed to determine if tree-ring $ δ^{18} $O in northeastern Japan records a signal consistent with the NPGO. Our results indicate that the tree-ring $ δ^{18} $O has a significant negative correlation with May–June (MJ) precipitation, as well as with short-term MJ relative humidity variation. Time-lagged temporal-domain comparisons indicate that the tree-ring $ δ^{18} $O is significantly correlated with the following year March–April (MA) and MJ NPGO index before the North Pacific climate transition in the late 1980s, particularly on decadal timescales. These relationships between our tree-ring $ δ^{18} $O and the climate patterns in the North Pacific are consistent with the actual early-summer precipitation. Spatial spring and early-summer sea-surface temperature anomalies exhibit a NPGO-like pattern in the following year. Spatial early-summer sea-level pressure anomalies also indicate North Pacific Oscillation (NPO) like patterns in the western North Pacific. These results suggest a lagged response of the NPGO to the EASM climate changes, and tree-ring $ δ^{18} $O in northeast Japan has a potential linkage with NPGO index from winter to early summer of the following year. © The Author(s) 2017
abstractGer	Abstract The North Pacific Gyre Oscillation (NPGO) significantly imprints on hydrological fluctuations of the East Asian summer monsoon (EASM) region, but this has not yet been observed in proxy-based hydroclimate reconstructions. This study reports a tree-ring cellulose oxygen isotope ($ δ^{18} $O) record from northeastern Japan spanning A.D. 1927–2010, overlapping with instrumental data, which we analyzed to determine if tree-ring $ δ^{18} $O in northeastern Japan records a signal consistent with the NPGO. Our results indicate that the tree-ring $ δ^{18} $O has a significant negative correlation with May–June (MJ) precipitation, as well as with short-term MJ relative humidity variation. Time-lagged temporal-domain comparisons indicate that the tree-ring $ δ^{18} $O is significantly correlated with the following year March–April (MA) and MJ NPGO index before the North Pacific climate transition in the late 1980s, particularly on decadal timescales. These relationships between our tree-ring $ δ^{18} $O and the climate patterns in the North Pacific are consistent with the actual early-summer precipitation. Spatial spring and early-summer sea-surface temperature anomalies exhibit a NPGO-like pattern in the following year. Spatial early-summer sea-level pressure anomalies also indicate North Pacific Oscillation (NPO) like patterns in the western North Pacific. These results suggest a lagged response of the NPGO to the EASM climate changes, and tree-ring $ δ^{18} $O in northeast Japan has a potential linkage with NPGO index from winter to early summer of the following year. © The Author(s) 2017
abstract_unstemmed	Abstract The North Pacific Gyre Oscillation (NPGO) significantly imprints on hydrological fluctuations of the East Asian summer monsoon (EASM) region, but this has not yet been observed in proxy-based hydroclimate reconstructions. This study reports a tree-ring cellulose oxygen isotope ($ δ^{18} $O) record from northeastern Japan spanning A.D. 1927–2010, overlapping with instrumental data, which we analyzed to determine if tree-ring $ δ^{18} $O in northeastern Japan records a signal consistent with the NPGO. Our results indicate that the tree-ring $ δ^{18} $O has a significant negative correlation with May–June (MJ) precipitation, as well as with short-term MJ relative humidity variation. Time-lagged temporal-domain comparisons indicate that the tree-ring $ δ^{18} $O is significantly correlated with the following year March–April (MA) and MJ NPGO index before the North Pacific climate transition in the late 1980s, particularly on decadal timescales. These relationships between our tree-ring $ δ^{18} $O and the climate patterns in the North Pacific are consistent with the actual early-summer precipitation. Spatial spring and early-summer sea-surface temperature anomalies exhibit a NPGO-like pattern in the following year. Spatial early-summer sea-level pressure anomalies also indicate North Pacific Oscillation (NPO) like patterns in the western North Pacific. These results suggest a lagged response of the NPGO to the EASM climate changes, and tree-ring $ δ^{18} $O in northeast Japan has a potential linkage with NPGO index from winter to early summer of the following year. © The Author(s) 2017
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title_short	Relationship between the Northern Pacific Gyre Oscillation and tree-ring cellulose oxygen isotopes in northeastern Japan
url	https://dx.doi.org/10.1186/s40562-017-0095-2
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author2	Miyahara, Hiroko Yokoyama, Yusuke Aze, Takahiro Obrochta, Stephen P. Nakatsuka, Takeshi
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up_date	2024-07-03T18:58:52.817Z
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Relationship between the Northern Pacific Gyre Oscillation and tree-ring cellulose oxygen isotopes in northeastern Japan

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