Hydroclimate reconstruction in central Japan over the past four centuries from tree-ring cellulose δ18O

被引：11

作者：

Sakashita, Wataru ^{[1
,2
,3
]}

Miyahara, Hiroko ^{[1
]}

Yokoyama, Yusuke ^{[2
,3
,4
]}

Aze, Takahiro ^{[5
]}

Nakatsuka, Takeshi ^{[6
]}

Hoshino, Yasuharu ^{[7
]}

Ohyama, Motonari ^{[8
]}

Yonenobu, Hitoshi ^{[9
]}

Takemura, Keiji ^{[10
]}

机构：

[1] Musashino Art Univ, Humanities & Sci, 1-736 Ogawa Cho, Tokyo 1878505, Japan

[2] Univ Tokyo, Atmosphere & Ocean Res Inst, Analyt Ctr Environm Study, 5-1-5 Kashiwanoha, Kashiwa, Chiba 2778564, Japan

[3] Univ Tokyo, Grad Sch Sci, Dept Earth & Planetary Sci, 7-3-1 Hongo, Tokyo 1130033, Japan

[4] Japan Agcy Marine Earth Sci & Technol JAMSTEC, Dept Biogeochem, 2-15 Natsushima Cho, Yokosuka, Kanagawa 2370061, Japan

[5] Univ Tokyo, Atmosphere & Ocean Res Inst, Ctr Cooperat Res Promot, 5-1-5 Kashiwanoha, Kashiwa, Chiba 2778564, Japan

[6] Res Inst Humanity & Nat, Kita Ku, 457-4 Motoyama, Kyoto 6038047, Japan

[7] Natl Res Inst Cultural Properties, 247-1 Saki Cho, Nara 6308577, Japan

[8] Tohoku Univ, Bot Gardens, Aoba Ku, 12-2 Kawauchi, Sendai, Miyagi 9800862, Japan

[9] Naruto Univ Educ, Coll Educ, 748 Nakashima, Naruto 7728502, Japan

[10] Kyoto Univ, Grad Sch Sci, Inst Geothermal Sci, Beppu, Oita 8740903, Japan

来源：

QUATERNARY INTERNATIONAL | 2017年 / 455卷

基金：

日本学术振兴会;

关键词：

Monsoon; Little Ice Age; Tree-ring; Oxygen isotope; Japan; LAST MILLENNIUM; WESTERN PACIFIC; STABLE-ISOTOPES; ICE-AGE; CLIMATE; MONSOON; PRECIPITATION; VARIABILITY; RATIOS; WATER;

D O I：

10.1016/j.quaint.2017.06.020

中图分类号：

P9 [自然地理学];

学科分类号：

0705 ; 070501 ;

摘要：

The East Asian summer monsoon is an important part of the Earth's climate system that is characterized by variations in the strength and expansion of the summer rain band. Rainfall reconstructions in China have revealed changing patterns of rainfall during the Little Ice Age (LIA), but limited hydroclimate reconstruction around Japan have hindered detailed understanding of physical processes associated with the atmospheric system in the western North Pacific. Here, we report relative humidity variations in the Meiyu/Baiu season from 1600-1959 CE by using tree-ring cellulose oxygen isotopes from central Japan; this is the first record of the LIA from the easternmost regions of the East Asian monsoon domain. Our data suggest that the wettest period occurred around 1780-1880 CE corresponding to the final stage of the LIA. This shift was concurrent with sea surface temperature negative (positive) anomalies around the Philippines (off eastern Japan). We suggest that meridional atmospheric circulation was weak during the last stage of the LIA. (C) 2017 Elsevier Ltd and INQUA. All rights reserved.

引用

页码：1 / 7

页数：7

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