Zobrazeno 1 - 10
of 58
pro vyhledávání: '"L. Papritz"'
Publikováno v:
Weather and Climate Dynamics, Vol 5, Pp 463-489 (2024)
When foehn winds surmount the Alps from the south, they often abruptly and vigorously descend into the leeside valleys on the Alpine north side. Scientists have long been intrigued by the underlying cause of this pronounced descent. While mountain gr
Externí odkaz:
https://doaj.org/article/2def5ce0cee84857ba95755124451cb4
Publikováno v:
Weather and Climate Dynamics, Vol 5, Pp 323-343 (2024)
Extreme heatwaves are one of the most impactful natural hazards, posing risks to human health, infrastructure, and ecosystems. Recent theoretical and observational studies have suggested that the vertical temperature structure during heatwaves limits
Externí odkaz:
https://doaj.org/article/38c0ada3b7e04c3d96f1d2633dc379b7
Publikováno v:
Weather and Climate Dynamics, Vol 5, Pp 181-209 (2024)
The development of atmospheric blocks over the North Atlantic–European region can lead to extreme weather events like heat waves or cold air outbreaks. Despite their potential severe impact on surface weather, the correct prediction of blocking lif
Externí odkaz:
https://doaj.org/article/0f5e1a4bb8ef4f74a1d3d1b39fb2cdd3
Publikováno v:
Weather and Climate Dynamics, Vol 4, Pp 943-961 (2023)
Despite the general warming trend, wintertime cold-air outbreaks in Europe have remained nearly as extreme and as common as decades ago. In this study, we identify six principal 850 hPa cold anomaly types over Europe in 1979–2020 using self-organiz
Externí odkaz:
https://doaj.org/article/8abc7d35892446a1bb971f3a3706898d
Publikováno v:
Weather and Climate Dynamics, Vol 3, Pp 1113-1138 (2022)
It has long been recognized that a rich variety of Alpine south-foehn flavours exist that are related to varying flow conditions above crest level, the presence and intensity of orographic precipitation on the Alpine south side, and the Po Valley str
Externí odkaz:
https://doaj.org/article/f9d7fec2237f4c869fa809031b68e1d8
Publikováno v:
Weather and Climate Dynamics, Vol 3, Pp 601-623 (2022)
The future evolution of storm tracks, their intensity, shape, and location, is an important driver of regional precipitation changes, cyclone-associated weather extremes, and regional climate patterns. For the North Atlantic storm track, Coupled Mode
Externí odkaz:
https://doaj.org/article/6750e2657cd74d1fb1cfdef9f313bc4a
Publikováno v:
Weather and Climate Dynamics, Vol 3, Pp 1-20 (2022)
A substantial portion of the moisture transport into the Arctic occurs in episodic, high-amplitude events with strong impacts on the Arctic's climate system components such as sea ice. This study focuses on the origin of such moist-air intrusions dur
Externí odkaz:
https://doaj.org/article/5fd03a25ff03424fb5da65d486464de3
Publikováno v:
Weather and Climate Dynamics, Vol 3, Pp 21-44 (2022)
Atmospheric blocking can influence Arctic weather by diverting the mean westerly flow and steering cyclones polewards, bringing warm, moist air to high latitudes. Recent studies have shown that diabatic heating processes in the ascending warm conveyo
Externí odkaz:
https://doaj.org/article/112cbfffe0224ac2ba3ae039057a7416
Publikováno v:
Weather and Climate Dynamics, Vol 3, Pp 89-111 (2022)
The Arctic atmosphere is strongly affected by anthropogenic warming leading to long-term trends in surface temperature and sea ice extent. In addition, it exhibits strong variability on timescales from days to seasons. While recent research elucidate
Externí odkaz:
https://doaj.org/article/19caf0f13152417fadce769147beda14
Autor:
H. Afargan-Gerstman, I. Polkova, L. Papritz, P. Ruggieri, M. P. King, P. J. Athanasiadis, J. Baehr, D. I. V. Domeisen
Publikováno v:
Weather and Climate Dynamics, Vol 1, Pp 541-553 (2020)
Marine cold air outbreaks (MCAOs) in the northeastern North Atlantic occur due to the advection of extremely cold air over an ice-free ocean. MCAOs are associated with a range of severe weather phenomena, such as polar lows, strong surface winds and
Externí odkaz:
https://doaj.org/article/ef2581e252ae4f95ab2c49815b0ae224