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Heini Wernli

Researcher at ETH Zurich

Publications -  306
Citations -  17718

Heini Wernli is an academic researcher from ETH Zurich. The author has contributed to research in topics: Extratropical cyclone & Precipitation. The author has an hindex of 67, co-authored 257 publications receiving 14867 citations. Previous affiliations of Heini Wernli include École Polytechnique Fédérale de Lausanne & University of Mainz.

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Heavy precipitation events where there’s no rain: Saharan rainfall climatology and its relationship with cyclones

TL;DR: In this article , the authors used high-resolution satellite precipitation estimates (IMERG) and meteorological reanalysis (ERA5) to identify thousands of heavy precipitation events (HPEs) that occurred over the Sahara in the past 21 years, and identify the governing atmospheric conditions on HPE-days, with a focus on surface cyclones.
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Influences of sources and weather dynamics on atmospheric deposition of Se species and other trace elements

TL;DR: In this article , the authors applied different chemical measurements to aerosol samples taken at a weekly resolution over 5 years (2015-2019), as well as precipitation and cloud water samples taken during a field campaign of two months in 2019 at Pic du Midi Observatory (French Pyrenees; 2877 m a.s.
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Warm conveyor belts in present-day and future climate simulations. Part I: Climatology and impacts

TL;DR: In this paper , the authors investigated how warm conveyor belts (WCB) will change in a future climate and found that WCB inflow regions in the North Pacific are systematically shifted northward in winter, which is in agreement with the northward shift of the storm track in this region.
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Aerosol-cloud interactions over the central Arctic Ocean

TL;DR: In this article , a detailed in-situ observations of aerosols and clouds performed on board the Swedish icebreaker Oden were performed over the central Arctic Ocean in 2018. And they showed that Aitken-mode particles, i.e. particles below 70 nm diameter, contribute significantly to cloud-forming particles (here termed cloud residuals), especially towards autumn with the start of the freeze-up of the sea ice.