FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2084705566> ?p ?o ?g. }

• W2084705566 endingPage "253" @default.
• W2084705566 startingPage "242" @default.
• W2084705566 abstract "Accurate prediction of future climate requires an understanding of the mechanisms of the Holocene climate; however, the driving forces, mechanisms, and processes of climate change in the Holocene associated with different time scales remain unclear. We investigated the drivers of Holocene sea surface temperature (SST) and sea ice extent in the North Pacific Ocean, and the Okhotsk and Bering Seas, as inferred from sediment core records, by using the alkenone unsaturation index as a biomarker of SST and abundances of sea ice-related diatoms (F. cylindrus and F. oceanica) as an indicator of sea ice extent to explore controlling mechanisms in the high-latitude Pacific. Temporal changes in alkenone content suggest that alkenone production was relatively high during the middle Holocene in the Okhotsk Sea and the western North Pacific, but highest in the late Holocene in the eastern Bering Sea and the eastern North Pacific. The Holocene variations of alkenone-SSTs at sites near Kamchatka in the Northwest Pacific, as well as in the western and eastern regions of the Bering Sea, and in the eastern North Pacific track the changes of Holocene summer insolation at 50°N, but at other sites in the western North Pacific, in the southern Okhotsk Sea, and the eastern Bering Sea they do not. In addition to insolation, other atmosphere and ocean climate drivers, such as sea ice distribution and changes in the position and activity of the Aleutian Low, may have systematically influenced the timing and magnitude of warming and cooling during the Holocene within the subarctic North Pacific. Periods of high sea ice extent in both the Okhotsk and Bering Seas may correspond to some periods of frequent or strong winter–spring dust storms in the Mongolian Gobi Desert, particularly one centered at ∼4–3 thousand years before present (kyr BP). Variation in storm activity in the Mongolian Gobi Desert region may reflect changes in the strength and positions of the Aleutian Low and Siberian High. We suggest that periods of eastward displacement or increased intensity of the Aleutian Low correspond with times of increased extent of sea ice in the western Okhotsk Sea and eastern Bering Sea." @default.
• W2084705566 created "2016-06-24" @default.
• W2084705566 creator A5003783948 @default.
• W2084705566 creator A5027274795 @default.
• W2084705566 creator A5031438879 @default.
• W2084705566 creator A5046766013 @default.
• W2084705566 creator A5066486736 @default.
• W2084705566 creator A5075928644 @default.
• W2084705566 creator A5083926202 @default.
• W2084705566 creator A5085845664 @default.
• W2084705566 date "2014-08-01" @default.
• W2084705566 modified "2023-09-27" @default.
• W2084705566 title "Holocene sea surface temperature and sea ice extent in the Okhotsk and Bering Seas" @default.
• W2084705566 cites W1524215045 @default.
• W2084705566 cites W1542285314 @default.
• W2084705566 cites W1676028456 @default.
• W2084705566 cites W1821232912 @default.
• W2084705566 cites W1823070337 @default.
• W2084705566 cites W1909880476 @default.
• W2084705566 cites W1932053588 @default.
• W2084705566 cites W1958271493 @default.
• W2084705566 cites W1990899433 @default.
• W2084705566 cites W1991795942 @default.
• W2084705566 cites W1994620584 @default.
• W2084705566 cites W1998818093 @default.
• W2084705566 cites W2009712251 @default.
• W2084705566 cites W2010923517 @default.
• W2084705566 cites W2025452596 @default.
• W2084705566 cites W2028025026 @default.
• W2084705566 cites W2029550314 @default.
• W2084705566 cites W2032319289 @default.
• W2084705566 cites W2036611575 @default.
• W2084705566 cites W2037284018 @default.
• W2084705566 cites W2037580998 @default.
• W2084705566 cites W2038882749 @default.
• W2084705566 cites W2039691001 @default.
• W2084705566 cites W2043452910 @default.
• W2084705566 cites W2046432746 @default.
• W2084705566 cites W2051137249 @default.
• W2084705566 cites W2051882771 @default.
• W2084705566 cites W2053251742 @default.
• W2084705566 cites W2055240432 @default.
• W2084705566 cites W2057356026 @default.
• W2084705566 cites W2060342839 @default.
• W2084705566 cites W2064832016 @default.
• W2084705566 cites W2067814097 @default.
• W2084705566 cites W2068891510 @default.
• W2084705566 cites W2075250643 @default.
• W2084705566 cites W2077525884 @default.
• W2084705566 cites W2079447400 @default.
• W2084705566 cites W2082091575 @default.
• W2084705566 cites W2084369306 @default.
• W2084705566 cites W2084682724 @default.
• W2084705566 cites W2085892105 @default.
• W2084705566 cites W2090153272 @default.
• W2084705566 cites W2090969352 @default.
• W2084705566 cites W2091284813 @default.
• W2084705566 cites W2092375540 @default.
• W2084705566 cites W2092604802 @default.
• W2084705566 cites W2092889986 @default.
• W2084705566 cites W2093401535 @default.
• W2084705566 cites W2098193783 @default.
• W2084705566 cites W2098885374 @default.
• W2084705566 cites W2099137034 @default.
• W2084705566 cites W2099274609 @default.
• W2084705566 cites W2099966862 @default.
• W2084705566 cites W2102204600 @default.
• W2084705566 cites W2106585957 @default.
• W2084705566 cites W2108889829 @default.
• W2084705566 cites W2110989872 @default.
• W2084705566 cites W2111308404 @default.
• W2084705566 cites W2112962190 @default.
• W2084705566 cites W2113554481 @default.
• W2084705566 cites W2115280287 @default.
• W2084705566 cites W2117175737 @default.
• W2084705566 cites W2120915775 @default.
• W2084705566 cites W2126580316 @default.
• W2084705566 cites W2134542031 @default.
• W2084705566 cites W2139199775 @default.
• W2084705566 cites W2140477756 @default.
• W2084705566 cites W2142607986 @default.
• W2084705566 cites W2142711471 @default.
• W2084705566 cites W2146605700 @default.
• W2084705566 cites W2154276443 @default.
• W2084705566 cites W2166623877 @default.
• W2084705566 cites W2169632101 @default.
• W2084705566 cites W2176502348 @default.
• W2084705566 cites W2280624662 @default.
• W2084705566 cites W4213327538 @default.
• W2084705566 cites W4306293736 @default.
• W2084705566 doi "https://doi.org/10.1016/j.pocean.2014.04.017" @default.
• W2084705566 hasPublicationYear "2014" @default.
• W2084705566 type Work @default.
• W2084705566 sameAs 2084705566 @default.
• W2084705566 citedByCount "43" @default.
• W2084705566 countsByYear W20847055662014 @default.
• W2084705566 countsByYear W20847055662015 @default.
• W2084705566 countsByYear W20847055662016 @default.

• next