0000000000172213

AUTHOR

Amos Winter

showing 5 related works from this author

Persistent link between Caribbean precipitation and Atlantic Ocean circulation during the Last Glacial revealed by a speleothem record from Puerto Ri…

2020

The sensitivity of tropical Atlantic precipitation patterns to the mean position of the Intertropical Convergence Zone (ITCZ) at different time scales is well‐known. However, recent research suggests a more complex behavior of the northern hemispheric tropical rain belt related to the ITCZ in the western tropical Atlantic. Here we present a precisely dated speleothem multi‐proxy record from a well‐monitored cave in Puerto Rico, covering the period between 46.2 and 15.3 ka. The stable isotope and trace element records document a pronounced response of regional rainfall to abrupt climatic excursions in the North Atlantic across the Last Glacial such as Heinrich stadials and Dansgaard/Oeschger…

551.7Atmospheric Sciencegeographygeography.geographical_feature_categoryStable isotope ratio550.28Last GlacialspeleothemsOcean currentPaleontologySpeleothemstable isotopesprecipitation reconstructionOceanographyOceanographyHeinrich stadialsPrecipitationGlacial periodGeologyDansgaard/Oeschger cycles
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Human adaptation strategies to abrupt climate change in Puerto Rico ca. 3.5 ka

2015

The connection between climatic change and social response is complex because change articulates a number of inter-related factors. Human decisions are filtered by social buffers – including social memory, risk perception, and cultural priorities – and the rate and scale of climate change is usually much larger than the scale of human decision-making. In this article, we provide information on climate change based on precisely dated speleothems with the response evident in archaeological sites that have radiocarbon date ranges within the same time frame. A stalagmite recovered from within the catchment area for aquifer recharge of the Pre-Arawak site of Angostura in Barceloneta, Puerto Ric…

ArcheologyGlobal and Planetary ChangeEcologySocial responseEcologyPaleoclimatologyAbrupt climate changePaleontologyClimate changeAdaptation strategiesGeologyEarth-Surface ProcessesThe Holocene
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Monitoring of Cueva Larga, Puerto Rico—A First Step to Decode Speleothem Climate Records

2017

This study presents results of an ongoing cave monitoring program at Cueva Larga, Puerto Rico. The monitoring includes monthly analyses of stable isotope ratios of rain and drip water, and trace element ratios of drip water and cave air parameters. Drip sites are above growing speleothems offering the unique chance to calibrate geochemical variations in speleothems in order to reconstruct past climate conditions. Seasonal rainfall patterns above Cueva Larga show characteristic stable isotope values. The wet season is characterized by more negative δ18O and δD values and a maritime deuterium excess (+10‰). The dry season has more positive δ18O and δD values and elevated deuterium excess (>15…

Wet seasonHydrologygeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesStable isotope ratioδ18OSpeleothem010502 geochemistry & geophysicsKarst01 natural sciencesMonitoring programCaveDry seasonPhysical geography0105 earth and related environmental sciences
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Hurricane Impact on Seepage Water in Larga Cave, Puerto Rico

2018

Atmospheric Sciencegeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesEcologyPaleontologySoil ScienceForestryAquatic Science010502 geochemistry & geophysics01 natural sciencesPaleotempestologyOceanographyCavePaleoclimatologyEnvironmental scienceTropical cyclone0105 earth and related environmental sciencesWater Science and TechnologyJournal of Geophysical Research: Biogeosciences
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Last glacial millennial-scale hydro-climate and temperature changes in Puerto Rico constrained by speleothem fluid inclusion δ<sup>18&a…

2021

Abstract. We present speleothem fluid inclusion δ18Of and δ2Hf values from Larga Cave, Puerto Rico, that covers the interval between 46.2 to 15.3 ka before present on millennial scale, including the Last Glacial Maximum (LGM) and several stadial and interstadial cycles. The dataset can be divided in two main clusters of stable isotope compositions of the fluid inclusion water with respect to the global meteoric water line which coincide with strong variations in the water content of the stalagmite. In particular, this clustering is found to be climate related, where the first cluster comprises samples from cold and dry periods, such as Heinrich and Greenland stadials, as well as parts of th…

geographygeography.geographical_feature_categoryCaveGlobal meteoric water lineMeteoric waterSpeleothemLast Glacial MaximumStalagmiteStadialGlacial periodAtmospheric sciencesGeology
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