Publications associées à Protéine antigel

Characteristics and sources of fluorescent aerosols in the central Arctic Ocean

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The Arctic is sensitive to cloud radiative forcing. Due to the limited number of aerosols present throughout much of the year, cloud formation is susceptible to the presence of cloud condensation nuclei and ice nucleating particles (INPs). Primary biologic ...

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Physicochemical characterization and source apportionment of Arctic ice-nucleating particles observed in Ny-Alesund in autumn 2019

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Ice-nucleating particles (INPs) initiate primary ice formation in Arctic mixed-phase clouds (MPCs), altering cloud radiative properties and modulating precipitation. For atmospheric INPs, the complexity of their spatiotemporal variations, heterogeneous sou ...

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Aerosol‐cloud interactions play an important role in the Arctic climate but remain poorly understood. Ice nucleating particles (INPs) contribute to the formation of ice crystals at temperatures above ‐38 °C in mixed phase clouds, which are predominant in t ...

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Snowfall microphysics: a dual-frequency and Doppler spectral radar perspective

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Snowfall is an essential component of the hydrological cycle, as it is involved in most precipitation on Earth, either directly as snow falling to the ground or indirectly as rain melted from snow. At the same time, the ice phase of clouds and precipitatio ...

EPFL2023

Fluorescent aerosols in the Arctic: Seasonality and sources

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Aerosol-cloud interactions play an important role in regulating the Arctic climate. However, cloud formation processes in the Arctic remain poorly understood and information on aerosol properties in this environment are insufficient, especially during pola ...

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Mixed-phase clouds in polar regions play a crucial role in surface ice melting. To accurately predict their radiative impact in climate models, an accurate representation of their microphysical structure is required. However, cloud ice content is generally ...

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Arctic clouds are among the largest sources of uncertainty in predictions of Arctic weather and climate. This is mainly due to errors in the representation of the cloud thermodynamic phase and the associated radiative impacts, which largely depends on the ...

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Protéine antigel

Investigating the intra-molecular and inter-molecular effects of post-translational modifications on intrinsically disordered protein regions and structured protein regions

Characteristics and sources of fluorescent aerosols in the central Arctic Ocean

Physicochemical characterization and source apportionment of Arctic ice-nucleating particles observed in Ny-Alesund in autumn 2019

Sources and seasonality of fluorescent aerosols in the Arctic

Snowfall microphysics: a dual-frequency and Doppler spectral radar perspective

Fluorescent aerosols in the Arctic: Seasonality and sources

Highly Active Ice‐Nucleating Particles at the Summer North Pole

Ice Multiplication in Polar Mixed-Phase Clouds

Secondary ice production in NorESM2 climate model: quantifying the impact on Arctic clouds

Secondary Ice Formation Processes in climate models

Graph Chatbot

Chattez avec Graph Search

Physicochemical characterization and source apportionment of Arctic ice-nucleating particles observed in Ny-Alesund in autumn 2019

Sources and seasonality of fluorescent aerosols in the Arctic

Secondary Ice Formation Processes in climate models

Investigating the intra-molecular and inter-molecular effects of post-translational modifications on intrinsically disordered protein regions and structured protein regions

Highly Active Ice‐Nucleating Particles at the Summer North Pole

Characteristics and sources of fluorescent aerosols in the central Arctic Ocean

Ice Multiplication in Polar Mixed-Phase Clouds

Fluorescent aerosols in the Arctic: Seasonality and sources

Snowfall microphysics: a dual-frequency and Doppler spectral radar perspective

Secondary ice production in NorESM2 climate model: quantifying the impact on Arctic clouds