Publications

1897 to 1908 of 14119 results

1. Ocean sustainability: act before it’s too late [Correspondence]

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2. Does tectonic deformation control episodic continental arc magmatism? Evidence from granitic magnetic fabrics (AMS)

   This paper applies magnetic fabric analyses to plutons of the East Pacific continental arc. Continental arc magmatism is strongly episodic, with voluminous granitic magma addition occurring during discrete high-flux events […]

   Read more of: Does tectonic deformation control episodic continental arc magmatism? Evidence from granitic magnetic fabrics (AMS)

3. Emerging Technologies and Approaches for In Situ, Autonomous Observing in the Arctic

   Understanding and predicting Arctic change and its impacts on global climate requires broad, sustained observations of the atmosphere-ice-ocean system, yet technological and logistical challenges severely restrict the temporal and spatial […]

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4. Deep carbon export peaks are driven by different biological pathways during the extended Scotia Sea (Southern Ocean) bloom

   Estimating the amount of organic carbon leaving the upper water column and becoming sequestered in the deep ocean is a major challenge in our understanding the oceanic C cycle. This […]

   Read more of: Deep carbon export peaks are driven by different biological pathways during the extended Scotia Sea (Southern Ocean) bloom

5. Life, diatoms and everything: a tribute to Leanne Armand [Guest Editorial]

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6. Multiple carbon cycle mechanisms associated with the glaciation of Marine Isotope Stage 4

   Here we use high-precision carbon isotope data (δ13C-CO2) to show atmospheric CO2 during Marine Isotope Stage 4 (MIS 4, ~70.5-59 ka) was controlled by a succession of millennial-scale processes. Enriched […]

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7. Decadal Scale Variability of Larsen Ice Shelf Melt Captured by Antarctic Peninsula Ice Core

   In this study, we used the stable water isotope record (δ18O) from an ice core drilled in Palmer Land, southern Antarctic Peninsula (AP). Utilizing δ18O we identified two climate regimes […]

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8. Global phylogeography of hyperdiverse lanternfishes indicates sympatric speciation in the deep sea

   Lanternfishes (Myctophidae) are one of the most species-rich families of mid-water fishes. They inhabit the mesopelagic zone, where physical barriers to dispersal and gene flow are permeable. Thus, modes of […]

   Read more of: Global phylogeography of hyperdiverse lanternfishes indicates sympatric speciation in the deep sea

9. The importance of ion composition for radiation belt modeling

   The banded structure of Electromagnetic Ion Cyclotron (EMIC) wave spectra and their resonant interactions with radiation belt electrons depend on the cold ion composition. However, there is a great deal […]

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10. The influence of tides on the marine carbonate chemistry of a coastal polynya in the south-eastern Weddell Sea

    Tides significantly affect polar coastlines by modulating ice shelf melt and modifying shelf water properties through transport and mixing. However, the effect of tides on the marine carbonate chemistry in […]

    Read more of: The influence of tides on the marine carbonate chemistry of a coastal polynya in the south-eastern Weddell Sea

11. The Ocean Boundary Layer beneath Larsen C Ice Shelf: Insights from Large-Eddy Simulations with a Near-Wall Model

    The melt rate of Antarctic ice shelves is of key importance for rising sea levels and future climate scenarios. Recent observations beneath Larsen C Ice Shelf revealed an ocean boundary […]

    Read more of: The Ocean Boundary Layer beneath Larsen C Ice Shelf: Insights from Large-Eddy Simulations with a Near-Wall Model

12. Warming-induced monsoon precipitation phase change intensifies glacier mass loss in the southeastern Tibetan Plateau

    Glaciers are key components of the mountain water towers of Asia and are vital for downstream domestic, agricultural, and industrial uses. The glacier mass loss rate over the southeastern Tibetan […]

    Read more of: Warming-induced monsoon precipitation phase change intensifies glacier mass loss in the southeastern Tibetan Plateau