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Future increases in Arctic precipitation linked to local evaporation and sea-ice retreat

Nature (London), 2014-05, Vol.509 (7501), p.479-482

2014

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Added Value of Large Ensemble Simulations for Assessing Extreme River Discharge in a 2 °C Warmer World

Geophysical research letters, 2019-02, Vol.46 (4), p.2093-2102

2019

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The simultaneous occurrence of surge and discharge extremes for the Rhine delta

Natural hazards and earth system sciences, 2013-08, Vol.13 (8), p.2017-2029

2013

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Strong future increases in Arctic precipitation variability linked to poleward moisture transport

Science advances, 2020-02, Vol.6 (7), p.eaax6869-eaax6869

2020

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The ocean-atmosphere response to wind-induced thermocline changes in the tropical South Western Indian Ocean

Climate dynamics, 2015-08, Vol.45 (3-4), p.989-1007

2015

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Signals of anthropogenic influence on European warming as seen in the trend patterns of daily temperature variance

International journal of climatology, 2005-01, Vol.25 (1), p.1-16

2005

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Attractor learning in synchronized chaotic systems in the presence of unresolved scales

Chaos (Woodbury, N.Y.), 2017-12, Vol.27 (12)

2017

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Future continental summer warming constrained by the present-day seasonal cycle of surface hydrology

Scientific reports, 2020-03, Vol.10 (1), p.4721, Article 4721

2020

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Robust assessment of future changes in extreme precipitation over the Rhine basin using a GCM

Hydrology and earth system sciences, 2011-04, Vol.15 (4), p.1157-1166

2011

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ECBILT: a dynamic alternative to mixed boundary conditions in ocean models

Tellus. Series A, Dynamic meteorology and oceanography, 1998-05, Vol.50 (3), p.348-367

1998

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Preferred regime transition routes and evidence for an unstable periodic orbit in a baroclinic model

Journal of the atmospheric sciences, 2004-09, Vol.61 (18), p.2267-2282

2004

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Complete synchronization of chaotic atmospheric models by connecting only a subset of state space

Nonlinear processes in geophysics, 2012-11, Vol.19 (6), p.611-621

2012

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Shifts of means are not a proxy for changes in extreme winter temperatures in climate projections

Climate dynamics, 2005-07, Vol.25 (1), p.51-63

2005

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Potential causes of abrupt climate events: A numerical study with a three-dimensional climate model

Geophysical research letters, 2002-09, Vol.29 (18), p.7-1-7-4

2002

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The Influence of Ocean Convection Patterns on High-Latitude Climate Projections

Journal of climate, 2004-11, Vol.17 (22), p.4316-4329

2004

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Large sea-ice volume anomalies simulated in a coupled climate model

Climate dynamics, 2003-03, Vol.20 (5), p.523-536

2003

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A mechanism of decadal variability of the sea-ice volume in the Northern Hemisphere

Climate dynamics, 2002-05, Vol.19 (1), p.61-83

2002

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Intrinsic limits to predictability of abrupt regional climate change in IPCC SRES scenarios

Geophysical research letters, 2002-08, Vol.29 (16), p.14-1-14-4

2002

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An efficient description of the dynamics of barotropic flow

Journal of the atmospheric sciences, 1995-04, Vol.52 (7), p.915-936

SELTEN, F. M

1995

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Meteorological conditions leading to extreme low variable renewable energy production and extreme high energy shortfall

Renewable & sustainable energy reviews, 2019-09, Vol.111, p.261-275

2019

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On the Mechanism of the Antarctic Circumpolar Wave

Journal of climate, 2000-05, Vol.13 (9), p.1461-1480

2000

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Solar-induced versus internal variability in a coupled climate model

Geophysical research letters, 1999-01, Vol.26 (2), p.205-208

1999

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Rapid transitions and ultra-low frequency behaviour in a 40 kyr integration with a coupled climate model of intermediate complexity

Climate dynamics, 2001-04, Vol.17 (7), p.559-570

2001

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A multi-model ensemble method that combines imperfect models through learning

Earth system dynamics, 2011-01, Vol.2 (1), p.161-177

2011

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The Role of the Ocean in Midlatitude, Interannual-to-Decadal-Timescale Climate Variability of a Coupled Model

Journal of climate, 2001-09, Vol.14 (17), p.3617-3630

2001

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Future increases in Arctic precipitation linked to local evaporation and sea-ice retreat

Added Value of Large Ensemble Simulations for Assessing Extreme River Discharge in a 2 °C Warmer World

The simultaneous occurrence of surge and discharge extremes for the Rhine delta

Strong future increases in Arctic precipitation variability linked to poleward moisture transport

The ocean-atmosphere response to wind-induced thermocline changes in the tropical South Western Indian Ocean

Signals of anthropogenic influence on European warming as seen in the trend patterns of daily temperature variance

Attractor learning in synchronized chaotic systems in the presence of unresolved scales

Future continental summer warming constrained by the present-day seasonal cycle of surface hydrology

Robust assessment of future changes in extreme precipitation over the Rhine basin using a GCM

ECBILT: a dynamic alternative to mixed boundary conditions in ocean models

Preferred regime transition routes and evidence for an unstable periodic orbit in a baroclinic model

Complete synchronization of chaotic atmospheric models by connecting only a subset of state space

Shifts of means are not a proxy for changes in extreme winter temperatures in climate projections

Potential causes of abrupt climate events: A numerical study with a three-dimensional climate model

The Influence of Ocean Convection Patterns on High-Latitude Climate Projections

Large sea-ice volume anomalies simulated in a coupled climate model

A mechanism of decadal variability of the sea-ice volume in the Northern Hemisphere

Intrinsic limits to predictability of abrupt regional climate change in IPCC SRES scenarios

An efficient description of the dynamics of barotropic flow

Meteorological conditions leading to extreme low variable renewable energy production and extreme high energy shortfall

On the Mechanism of the Antarctic Circumpolar Wave

Solar-induced versus internal variability in a coupled climate model

Rapid transitions and ultra-low frequency behaviour in a 40 kyr integration with a coupled climate model of intermediate complexity

A multi-model ensemble method that combines imperfect models through learning

The Role of the Ocean in Midlatitude, Interannual-to-Decadal-Timescale Climate Variability of a Coupled Model

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