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Showing 1–17 of 17 results

Advanced filters: Author: Matthew D. Shupe Clear advanced filters

Author Correction: Annual cycle observations of aerosols capable of ice formation in central Arctic clouds

Jessie M. Creamean
Kevin Barry
Ola Persson
Amendments and CorrectionsOpen Access12 Oct 2022
Nature Communications

Volume: 13, P: 1
The Marginal Ice Zone as a dominant source region of atmospheric mercury during central Arctic summertime

Oceanic evasion, which mainly occurs in the Marginal Ice Zone, is the main cause of the summertime maximum of gaseous elemental mercury in the central Arctic Ocean

Fange Yue
Hélène Angot
Zhouqing Xie
ResearchOpen Access14 Aug 2023
Nature Communications

Volume: 14, P: 1-13
A central arctic extreme aerosol event triggered by a warm air-mass intrusion

Warm and moist air-mass intrusions into the Arctic are more frequent than the past decades. Here, the authors show that warm air mass intrusions from northern Eurasia inject record amounts of aerosols into the central Arctic Ocean strongly impacting atmospheric chemistry and cloud properties.

Lubna Dada
Hélène Angot
Julia Schmale
ResearchOpen Access08 Sept 2022
Nature Communications

Volume: 13, P: 1-15
Arctic warming by abundant fine sea salt aerosols from blowing snow

Fine sea salt aerosols produced by blowing snow in the Arctic impact cloud properties and warm the surface, according to observations from the MOSAiC expedition.

Xianda Gong
Jiaoshi Zhang
Jian Wang
ResearchOpen Access04 Sept 2023
Nature Geoscience

Volume: 16, P: 768-774
Humidity trends imply increased sensitivity to clouds in a warming Arctic

The cloud radiative effect (CRE) in the Arctic plays an important role in the amount of infrared radiation that reaches the surface. Here, the authors show that interplay between temperature and humidity controls CRE through competing influences in two semi-transparent wavelength ranges.

Christopher J. Cox
Von P. Walden
Matthew D. Shupe
ResearchOpen Access10 Dec 2015
Nature Communications

Volume: 6, P: 1-8
A tidal disruption event coincident with a high-energy neutrino

The tidal disruption event AT2019dsg is probably associated with a high-energy neutrino, suggesting that such events can contribute to the cosmic neutrino flux. The electromagnetic emission is explained in terms of a central engine, a photosphere and an extended synchrotron-emitting outflow.

Robert Stein
Sjoert van Velzen
Yuhan Yao
Research22 Feb 2021
Nature Astronomy

Volume: 5, P: 510-518
Annual cycle observations of aerosols capable of ice formation in central Arctic clouds

The Arctic is changing faster than anywhere else on Earth. Interactions between clouds and aerosols play a role in these changes. We report how the quantities and origins of aerosols that affect cloud ice formation change over a full sea ice cycle

Jessie M. Creamean
Kevin Barry
Ola Persson
ResearchOpen Access20 Jun 2022
Nature Communications

Volume: 13, P: 1-12
Measurements of aerosol microphysical and chemical properties in the central Arctic atmosphere during MOSAiC

Benjamin Heutte
Nora Bergner
Julia Schmale
ResearchOpen Access11 Oct 2023
Scientific Data

Volume: 10, P: 1-16
Widespread detection of chlorine oxyacids in the Arctic atmosphere

Observations are reported of HClO₃ and HClO₄ in the atmosphere and their widespread occurrence over the pan-Arctic during spring, providing further insights into atmospheric chlorine cycling in the polar environment.

Yee Jun Tham
Nina Sarnela
Alfonso Saiz-Lopez
ResearchOpen Access30 Mar 2023
Nature Communications

Volume: 14, P: 1-10
Optical follow-up of the neutron star–black hole mergers S200105ae and S200115j

The optical follow-up and analysis of two neutron star–black hole merger candidates with the Zwicky Transient Facility did not yield viable counterparts. However, state-of-the-art kilonova models constrain the ejecta properties of these mergers.

Shreya Anand
Michael W. Coughlin
Azamat F. Valeev
Research14 Sept 2020
Nature Astronomy

Volume: 5, P: 46-53
Year-round trace gas measurements in the central Arctic during the MOSAiC expedition

Hélène Angot
Byron Blomquist
Julia Schmale
ResearchOpen Access25 Nov 2022
Scientific Data

Volume: 9, P: 1-19
General relativistic orbital decay in a seven-minute-orbital-period eclipsing binary system

Observations of an eclipsing double-white-dwarf binary with an orbital period of 6.91 minutes that is decaying as predicted by general relativity are reported; once launched, the Laser Interferometer Space Antenna (LISA) should swiftly detect this binary.

Kevin B. Burdge
Michael W. Coughlin
Thomas A. Prince
Research24 Jul 2019
Nature

Volume: 571, P: 528-531
Role of air-mass transformations in exchange between the Arctic and mid-latitudes

Understanding the thermodynamics of air-mass transformations that occur in the atmosphere at the boundary between the Arctic and mid-latitudes is key to improving weather and climate predictions, according to a literature synthesis

Felix Pithan
Gunilla Svensson
Manfred Wendisch
Reviews29 Oct 2018
Nature Geoscience

Volume: 11, P: 805-812
Resilience of persistent Arctic mixed-phase clouds

Mixed-phase clouds, comprising both ice and supercooled liquid water, have a large impact on radiative fluxes in the Arctic. Interactions between numerous local feedbacks sustain these complex cloud systems, leading to the development of a resilient mixed-phase cloud system.

Hugh Morrison
Gijs de Boer
Kara Sulia
Reviews11 Dec 2011
Nature Geoscience

Volume: 5, P: 11-17
Continuous observations of the surface energy budget and meteorology over the Arctic sea ice during MOSAiC

Christopher J. Cox
Michael R. Gallagher
Taneil Uttal
ResearchOpen Access04 Aug 2023
Scientific Data

Volume: 10, P: 1-27
Profile observations of the Arctic atmospheric boundary layer with the BELUGA tethered balloon during MOSAiC

Christian Pilz
Michael Lonardi
Manfred Wendisch
ResearchOpen Access10 Aug 2023
Scientific Data

Volume: 10, P: 1-12
Effects of Monoamine Oxidase Inhibition on the Reinforcing Properties of Low-Dose Nicotine

Tracy T Smith
Laura E Rupprecht
Alan F Sved
Research09 Mar 2016
Neuropsychopharmacology

Volume: 41, P: 2335-2343