GLORIA — GEOMAR Library Ocean Research Information Access

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Stable isotope data of benthic foraminifera from OMEXII-9K (2018)

Hendry, Katharine R ; Gong, Xun ; Knorr, Gregor ; [et al.]

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Publication Date: 2023-02-12

Description: This data release contains stable isotope data from benthic foraminifera isolated from sediment core OMEXII-9K off the Iberian Margin, from 0 to 204cm, and an updated age model.

Keywords: Cibicidoides pachyderma, δ13C; Cibicidoides pachyderma, δ13C standard deviation; Cibicidoides pachyderma, δ18O; Cibicidoides pachyderma, δ18O standard deviation; Cibicidoides wuellerstorfi, δ13C; Cibicidoides wuellerstorfi, δ13C, standard deviation; Cibicidoides wuellerstorfi, δ18O; Cibicidoides wuellerstorfi, δ18O standard deviation; DEPTH, sediment/rock; OMEXII-9K_2; Tropical North Atlantic

Type: Dataset

Format: text/tab-separated-values, 140 data points

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Age determination of sediment core LV53-19-1 (2020)

Wu, Yonghua ; Shi, Xuefa ; Gong, Xun ; [et al.]

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Publication Date: 2023-06-27

Keywords: Age, 14C AMS; Age, 14C calibrated; Age, dated; Age, dated material; Age, dated standard error; AWI_Paleo; Biomarker; Calendar age; Calendar age, maximum/old; Calendar age, minimum/young; DEPTH, sediment/rock; Japan Sea; Laboratory code/label; Last Glacial; LV53-19-1; North Pacific; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; paleo-oceanography; PC; Piston corer; sea-level; SST; TEX86; UK'37; upper ocean

Type: Dataset

Format: text/tab-separated-values, 49 data points

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Poleward Shift of the Major Ocean Gyres Detected in a Warming Climate (2021)

Yang, Hu ; Lohmann, Gerrit ; Krebs-Kanzow, Uta ; [et al.]

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Publication Date: 2021-10-12

Description: Recent evidence shows that wind-driven ocean currents, like the western boundary currents, are strongly affected by global warming. However, due to insufficient observations both on temporal and spatial scales, the impact of climate change on large-scale ocean gyres is still not clear. Here, based on satellite observations of sea surface height and sea surface temperature, we find a consistent poleward shift of the major ocean gyres. Due to strong natural variability, most of the observed ocean gyre shifts are not statistically significant, implying that natural variations may contribute to the observed trends. However, climate model simulations forced with increasing greenhouse gases suggest that the observed shift is most likely to be a response of global warming. The displacement of ocean gyres, which is coupled with the poleward shift of extratropical atmospheric circulation, has broad impacts on ocean heat transport, regional sea level rise, and coastal ocean circulation.

Keywords: 551.46 ; ocean gyre ; climate change ; poleward shift ; global warming ; ocean circulation ; sea level rise

Language: English

Type: map

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