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  • 1
    Publication Date: 2024-04-20
    Keywords: 130-806; 138-846; 138-849; 167-1014; 167-1018; 181-1123; 181-1125; 184-1143; 184-1148; 198-1208; 198-1209; 198-1210; 202-1239; 202-1241; 321-U1338; 89-586_Site; 90-593_Site; 90-594_Site; Benthic foraminifera; Binary Object; Carbon and oxygen stable isotopes; COMPCORE; Composite Core; Deep Sea Drilling Project; DSDP; Equatorial East Pacific; Exp321; File content; Glomar Challenger; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Leg130; Leg138; Leg167; Leg181; Leg184; Leg198; Leg202; Leg89; Leg90; North Pacific Ocean; Ocean Drilling Program; ODP; Pacific Equatorial Age Transect II / Juan de Fuca; South China Sea; South Pacific; South Pacific/CONT RISE; South Pacific/Tasman Sea/PLATEAU; South Pacific Ocean; Stable isotope
    Type: Dataset
    Format: text/tab-separated-values, 4 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2024-04-18
    Keywords: 198-1209A; 198-1209B; AGE; Benthic foraminifera; Carbon and oxygen stable isotopes; Cibicidoides wuellerstorfi, δ13C; Cibicidoides wuellerstorfi, δ18O; Depth, composite; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Joides Resolution; Leg198; North Pacific Ocean; Ocean Drilling Program; ODP; Sample code/label; Stable isotope; δ18O, adjusted/corrected
    Type: Dataset
    Format: text/tab-separated-values, 415 data points
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  • 3
    Publication Date: 2024-04-18
    Keywords: 198-1210A; 198-1210B; AGE; Benthic foraminifera; Carbon and oxygen stable isotopes; Cibicidoides wuellerstorfi, δ13C; Cibicidoides wuellerstorfi, δ18O; Depth, composite; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Joides Resolution; Leg198; North Pacific Ocean; Ocean Drilling Program; ODP; Sample code/label; Stable isotope; δ18O, adjusted/corrected
    Type: Dataset
    Format: text/tab-separated-values, 324 data points
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  • 4
    Publication Date: 2024-04-20
    Description: Benthic foraminifera stable isotopes values from Shatsky Rise 1209 and 1210. A synthesis of benthic foraminifera d13C values from the mid-Pliocene warm period and early Pliocene and OC3 products pre-Industrial water column d13C and Late Holocene core top benthic foraminifera d13C.
    Keywords: Benthic foraminifera; Carbon and oxygen stable isotopes; Deep Sea Drilling Project; DSDP; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Ocean Drilling Program; ODP; Stable isotope
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 5
    Publication Date: 2024-04-25
    Description: Modelling output from a Late Pliocene and Early Pliocene geochemically enabled CESM 1.2.2.1. The CESM 1.2.2.1 code used to run the climate simulations is available from https://svn-ccsm-models.cgd.ucar.edu/cesm1/release_tags/cesm1_2_2_1. The code modifications made to CESM 1.2.2.1 to include carbon isotopes following ref. 38 are available from https://github.com/nburls/FordEtAl2022_CISOmods. Figures with coastal outlines (for example, Figs. 1 and 2 and Extended Data Figs. 1 and 2) were created in Matlab with the M_maps package71.
    Keywords: Binary Object; Binary Object (File Size); File content; Model; Modelling; Pliocene; Preindustrial
    Type: Dataset
    Format: text/tab-separated-values, 12 data points
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  • 6
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    AMS (American Meteorological Society)
    In:  Journal of Climate, 27 (21). pp. 8135-8150.
    Publication Date: 2020-08-04
    Description: Sea surface temperature (SST) anomalies in the eastern equatorial Atlantic are connected to modulations in the strength of the South Atlantic subtropical high-pressure system, referred to as the South Atlantic Anticyclone (SAA). Using ocean and atmosphere reanalysis products we show here that the strength of the SAA from February to May impacts the timing of the cold tongue onset and the intensity of its development in the eastern equatorial Atlantic (EEA) via anomalous tropical wind power. This modulation of the timing and amplitude of the seasonal cold tongue development manifests as anomalous SST events peaking between June and August. The timing and impact of this connection is not completely symmetric for warm and cold events. For cold events, an anomalously strong SAA in February and March leads to positive wind power anomalies from February to June resulting in an early cold tongue onset and subsequent cold SST anomalies in June and July. For warm events the anomalously weak SAA persists until May, generating negative wind power anomalies that lead to a late cold tongue onset as well as a suppression of the cold tongue development and associated warm SST anomalies. Mechanisms by which SAA induced wind power variations south of the equator influence EEA SST are discussed, including ocean adjustment via Rossby and Kelvin wave propagation, meridional advection, and local intraseasonal wind variations
    Type: Article , PeerReviewed
    Format: text
    Format: text
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  • 7
    Publication Date: 2024-02-07
    Description: Interannual sea surface temperature (SST) variations in the tropical Atlantic Ocean lead to anomalous atmospheric circulation and precipitation patterns with important ecological and socioeconomic consequences for the semiarid regions of sub-Saharan Africa and northeast Brazil. This interannual SST variability is characterized by three modes: an Atlantic meridional mode featuring an anomalous cross-equatorial SST gradient that peaks in boreal spring; an Atlantic zonal mode (Atlantic Nino mode) with SST anomalies in the eastern equatorial Atlantic cold tongue region that peaks in boreal summer; and a second zonal mode of variability with eastern equatorial SST anomalies peaking in boreal winter. Here we investigate the extent to which there is any seasonality in the relationship between equatorial warm water recharge and the development of eastern equatorial Atlantic SST anomalies. Seasonally stratified cross-correlation analysis between eastern equatorial Atlantic SST anomalies and equatorial heat content anomalies (evaluated using warm water volume and sea surface height) indicate that while equatorial heat content changes do occasionally play a role in the development of boreal summer Atlantic zonal mode events, they contribute more consistently to Atlantic Nino II, boreal winter events. Event and composite analysis of ocean adjustment with a shallow water model suggest that the warm water volume anomalies originate mainly from the off-equatorial northwestern Atlantic, in agreement with previous studies linking them to anomalous wind stress curl associated with the Atlantic meridional mode.
    Type: Article , PeerReviewed
    Format: text
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  • 8
    Publication Date: 2017-11-26
    Description: An essential element of modern ocean circulation and climate is the Atlantic meridional overturning circulation(AMOC), which includes deep-water formation in the subarctic North Atlantic. However, a comparable overturningcirculation is absent in the Pacific, the world’s largest ocean, where relatively fresh surface waters inhibit North Pacificdeep convection. We present complementary measurement and modeling evidence that the warm, ~400–ppmv(parts per million by volume) CO2world of the Pliocene supported subarctic North Pacific deep-water formationand a Pacific meridional overturning circulation (PMOC) cell. In Pliocene subarctic North Pacific sediments, we reportorbitally paced maxima in calcium carbonate accumulation rate, with accompanying pigment and total organiccarbon measurements supporting deep-ocean ventilation-driven preservation as their cause. Together with highaccumulation rates of biogenic opal, these findings require vigorous bidirectional communication between surfacewaters and interior waters down to ~3 km in the western subarctic North Pacific, implying deep convection. Redox-sensitive trace metal data provide further evidence of higher Pliocene deep-ocean ventilation before the 2.73-Ma(million years) transition. This observational analysis is supported by climate modeling results, demonstratingthat atmospheric moisture transport changes, in response to the reduced meridional sea surface temperaturegradients of the Pliocene, were capable of eroding the halocline, leading to deep-water formation in the westernsubarctic Pacific and a strong PMOC. This second Northern Hemisphere overturning cell has important implica-tions for heat transport, the ocean/atmosphere cycle of carbon, and potentially the equilibrium response of thePacific to global warming.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
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  • 9
    Publication Date: 2022-01-10
    Description: The mid-Pliocene (∼3 Ma) is one of the most recent warm periods with high CO2 concentrations in the atmosphere and resulting high temperatures, and it is often cited as an analog for near-term future climate change. Here, we apply a moisture budget analysis to investigate the response of the large-scale hydrological cycle at low latitudes within a 13-model ensemble from the Pliocene Model Intercomparison Project Phase 2 (PlioMIP2). The results show that increased atmospheric moisture content within the mid-Pliocene ensemble (due to the thermodynamic effect) results in wetter conditions over the deep tropics, i.e., the Pacific intertropical convergence zone (ITCZ) and the Maritime Continent, and drier conditions over the subtropics. Note that the dynamic effect plays a more important role than the thermodynamic effect in regional precipitation minus evaporation (PmE) changes (i.e., northward ITCZ shift and wetter northern Indian Ocean). The thermodynamic effect is offset to some extent by a dynamic effect involving a northward shift of the Hadley circulation that dries the deep tropics and moistens the subtropics in the Northern Hemisphere (i.e., the subtropical Pacific). From the perspective of Earth's energy budget, the enhanced southward cross-equatorial atmospheric transport (0.22 PW), induced by the hemispheric asymmetries of the atmospheric energy, favors an approximately 1∘ northward shift of the ITCZ. The shift of the ITCZ reorganizes atmospheric circulation, favoring a northward shift of the Hadley circulation. In addition, the Walker circulation consistently shifts westward within PlioMIP2 models, leading to wetter conditions over the northern Indian Ocean. The PlioMIP2 ensemble highlights that an imbalance of interhemispheric atmospheric energy during the mid-Pliocene could have led to changes in the dynamic effect, offsetting the thermodynamic effect and, hence, altering mid-Pliocene hydroclimate.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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