• Impact of Martian Crustal Magnetic Field on the Ion Escape 

  Dubinin, E.; Fraenz, M.; Pätzold, M.; Woch, J.; McFadden, J.; Fan, K.; Wei, Y.; Tsareva, O.; Zelenyi, L. (Journal of Geophysical Research: Space Physics, 2020)

  Based on the Mars Atmosphere and Volatile EvolutioN (MAVEN) observations, we have analyzed the role of the crustal magnetic field on ion loss driven by the direct interaction of the solar wind with the Mars ionosphere. ...

• Forms of meteorological knowledge 1750–1850 in German countries and beyond 

  Richter, Linda (Wiley Interdisciplinary Reviews: Climate Change, 2020)

  The complexity of atmospherical processes has always yielded a multitude of ways of knowing about the weather. What has been lacking in the historiography of meteorology so far is a way to formulate differences between ...

• Quantifying the Effects of EMIC Wave Scattering and Magnetopause Shadowing in the Outer Electron Radiation Belt by Means of Data Assimilation 

  Cervantes, S.; Shprits, Y. Y.; Aseev, N. A.; Allison, H. J. (Journal of Geophysical Research: Space Physics, 2020)

  In this study we investigate two distinct loss mechanisms responsible for the rapid dropouts of radiation belt electrons by assimilating data from Van Allen Probes A and B and Geostationary Operational Environmental ...

• Sensitivity study of the planetary boundary layer and microphysical schemes to the initialization of convection over the Arabian Peninsula 

  Schwitalla, Thomas; Branch, Oliver; Wulfmeyer, Volker (Quarterly Journal of the Royal Meteorological Society, 2019)

  In this study, we present a five-member Weather Research and Forecasting (WRF) physics ensemble over the Arabian Peninsula on the convection-permitting (CP) scale and investigate the ability to simulate convection and ...

• Analysis of the Thermodynamic Phase Transition of Tracked Convective Clouds Based on Geostationary Satellite Observations 

  Coopman, Q.; Hoose, C.; Stengel, M. (Journal of Geophysical Research: Atmospheres, 2020)

  Clouds are liquid at temperature greater than 0°C and ice at temperature below −38°C. Between these two thresholds, the temperature of the cloud thermodynamic phase transition from liquid to ice is difficult to predict and ...

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