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• W2029122292 endingPage "79" @default.
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• W2029122292 abstract "This study presents a newly compiled dataset of modern pollen and climate data from 798 sites across Japan and the Russian Far East. This comprehensive reference dataset combined with the modern analogue technique (MAT) provides a powerful tool for pollen-based reconstruction of the Quaternary Northwest Pacific climate. Pollen-derived reconstruction of the modern climate at the reference pollen-sampling sites matches well with the estimated modern climate values (R2 values vary between 0.79 and 0.95, and RMSEP values vary between 5.8 and 9.7% of the modern climatic range for all nine tested variables). The successful testing of the method encourages its application to the fossil pollen records. We used a coarse-resolution pollen record from Lake Biwa to reconstruct glacial–interglacial climate dynamics in central Japan since ~ 438 kyr and compared it to the earlier reconstruction based on a less representative reference dataset. The current and earlier results consistently demonstrate that the coldest glacial intervals experienced pronounced cooling in winter and moderate cooling in summer, supporting the growth of cool mixed forest (COMX) where warm mixed forest (WAMX) predominates today. During the last glacial, maximum (~ 24 kyr BP) mean temperatures of the coldest (MTCO) and warmest (MTWA) month were about − 13 °C (RMSEP = 2.34 °C) and 21 °C (RMSEP = 1.66 °C) respectively, and annual precipitation (PANN) was about 800 mm (RMSEP = 158.06 mm). During the thermal optimums of the interglacial intervals, the temperatures of the coldest and warmest month were above 0 °C and 25 °C respectively, leading to the reconstruction of WAMX and temperate conifer forest (TECO). Although both these vegetation types grow in the southern part of Japan today, WAMX requires warmer space. The presence of WAMX during marine isotope stages (MIS) 11 and 1, and its absence during MIS 9 and MIS 5 contradict the marine isotope and Antarctic ice records, suggesting that the latter two interglacials were the warmest of the last 800 kyr. The apparent contradiction allows at least three different explanations including low temporal resolution of the pollen record; different trends in CO2 concentrations during ‘short’ and ‘long’ interglacials; and regional climate variability and non-linear response of different regions to the global forcing. More definitive conclusions will be possible on the basis of forthcoming high-resolution pollen records from central Japan." @default.
• W2029122292 created "2016-06-24" @default.
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• W2029122292 date "2011-09-01" @default.
• W2029122292 modified "2023-10-16" @default.
• W2029122292 title "Progress in the reconstruction of Quaternary climate dynamics in the Northwest Pacific: A new modern analogue reference dataset and its application to the 430-kyr pollen record from Lake Biwa" @default.
• W2029122292 cites W1497544065 @default.
• W2029122292 cites W1631559605 @default.
• W2029122292 cites W1977505730 @default.
• W2029122292 cites W1977595786 @default.
• W2029122292 cites W1978248369 @default.
• W2029122292 cites W1978582597 @default.
• W2029122292 cites W1978912552 @default.
• W2029122292 cites W1980012339 @default.
• W2029122292 cites W1980416378 @default.
• W2029122292 cites W1982002336 @default.
• W2029122292 cites W1985949400 @default.
• W2029122292 cites W1988626367 @default.
• W2029122292 cites W1992646017 @default.
• W2029122292 cites W1993825612 @default.
• W2029122292 cites W1996047388 @default.
• W2029122292 cites W1996932107 @default.
• W2029122292 cites W2000444336 @default.
• W2029122292 cites W2000743036 @default.
• W2029122292 cites W2003501861 @default.
• W2029122292 cites W2004090951 @default.
• W2029122292 cites W2004438023 @default.
• W2029122292 cites W2005179525 @default.
• W2029122292 cites W2005192137 @default.
• W2029122292 cites W2005736516 @default.
• W2029122292 cites W2014036968 @default.
• W2029122292 cites W2016129638 @default.
• W2029122292 cites W2019732278 @default.
• W2029122292 cites W2024309015 @default.
• W2029122292 cites W2026144411 @default.
• W2029122292 cites W2027120199 @default.
• W2029122292 cites W2027385173 @default.
• W2029122292 cites W2030036317 @default.
• W2029122292 cites W2035325438 @default.
• W2029122292 cites W2037528981 @default.
• W2029122292 cites W2038243361 @default.
• W2029122292 cites W2038587151 @default.
• W2029122292 cites W2038709304 @default.
• W2029122292 cites W2039630741 @default.
• W2029122292 cites W2040529067 @default.
• W2029122292 cites W2040945899 @default.
• W2029122292 cites W2042478259 @default.
• W2029122292 cites W2046753504 @default.
• W2029122292 cites W2049826666 @default.
• W2029122292 cites W2051671961 @default.
• W2029122292 cites W2052141950 @default.
• W2029122292 cites W2054013071 @default.
• W2029122292 cites W2066390458 @default.
• W2029122292 cites W2067841771 @default.
• W2029122292 cites W2073966665 @default.
• W2029122292 cites W2076517688 @default.
• W2029122292 cites W2076889395 @default.
• W2029122292 cites W2077169411 @default.
• W2029122292 cites W2079943478 @default.
• W2029122292 cites W2081545405 @default.
• W2029122292 cites W2082130975 @default.
• W2029122292 cites W2082661503 @default.
• W2029122292 cites W2088841971 @default.
• W2029122292 cites W2089144464 @default.
• W2029122292 cites W2093519985 @default.
• W2029122292 cites W2094431815 @default.
• W2029122292 cites W2099035636 @default.
• W2029122292 cites W2099358694 @default.
• W2029122292 cites W2103983252 @default.
• W2029122292 cites W2107691545 @default.
• W2029122292 cites W2110116713 @default.
• W2029122292 cites W2113660406 @default.
• W2029122292 cites W2114771431 @default.
• W2029122292 cites W2117779820 @default.
• W2029122292 cites W2123200166 @default.
• W2029122292 cites W2135101535 @default.
• W2029122292 cites W2136246993 @default.
• W2029122292 cites W2140958901 @default.
• W2029122292 cites W2141459972 @default.
• W2029122292 cites W2142644033 @default.
• W2029122292 cites W2145725460 @default.
• W2029122292 cites W2146485648 @default.
• W2029122292 cites W2150352749 @default.
• W2029122292 cites W2153625482 @default.

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