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- Lenggenhager, Sina; Croci‐Maspoli, Mischa; Brönnimann, Stefan
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Quarterly Journal of the Royal Meteorological Society, Vol. 145, Issue 719
https://doi.org/10.1002/qj.3449
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Evidence linking Arctic amplification to extreme weather in mid-latitudes: ARCTIC LINKS TO MID-LATITUDE WEATHER
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A New Rossby Wave–Breaking Interpretation of the North Atlantic Oscillation
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The relationship of winter season North Atlantic blocking frequencies to extreme cold or dry spells in the ERA-40
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A consistent poleward shift of the storm tracks in simulations of 21st century climate: POLEWARD SHIFT OF THE STORM TRACKS
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Recent Arctic amplification and extreme mid-latitude weather
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Dependence of Present and Future European Temperature Extremes on the Location of Atmospheric Blocking
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Blocking and its Response to Climate Change
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The Latitudinal Dependence of Atmospheric Jet Scales and Macroturbulent Energy Cascades
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Blocking variability: Arctic Amplification versus Arctic Oscillation: Blocking: −ao Versus Arctic Amplification
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The Sensitivity of the Jet Stream Response to Climate Change to Radiative Assumptions
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April 2019 |
A methodology for the comparison of blocking climatologies across indices, models and climate scenarios
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Robust Future Changes in Temperature Variability under Greenhouse Gas Forcing and the Relationship with Thermal Advection
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Relationship between eddy-driven jet latitude and width: JET LATITUDE AND JET WIDTH
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Influence of blocking on Northern European and Western Russian heatwaves in large climate model ensembles
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Weather-Layer Dynamics of Baroclinic Eddies and Multiple Jets in an Idealized General Circulation Model
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The Impact of Baroclinic Eddy Feedback on the Persistence of Jet Variability in the Two-Layer Model
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Response of the Midlatitude Jets, and of Their Variability, to Increased Greenhouse Gases in the CMIP5 Models
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Quantifying the relevance of atmospheric blocking for co-located temperature extremes in the Northern Hemisphere on (sub-)daily time scales: BLOCKING AND TEMPERATURE EXTREMES
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Planetary-scale baroclinic envelope Rossby solitons in a two-layer model and their interaction with synoptic-scale eddies
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