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Dr Antje Weisheimer (she)

Principal NCAS Research Fellow

Research theme

  • Climate physics

Sub department

  • Atmospheric, Oceanic and Planetary Physics

Research groups

  • Predictability of weather and climate
Antje.Weisheimer@physics.ox.ac.uk
Telephone: 01865 (2)82441
Robert Hooke Building, room S43
ECMWF
NCAS
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Warming Stripes for Oxford from 1814-2019

Warming Stripes for Oxford from 1814-2019.

Stochastic Parameterization: Towards a new view of Weather and Climate Models

(2015)

Authors:

Judith Berner, Ulrich Achatz, Lauriane Batte, Lisa Bengtsson, Alvaro De La Camara, Daan Crommelin, Hannah Christensen, Matteo Colangeli, Stamen Dolaptchiev, Christian LE Franzke, Petra Friederichs, Peter Imkeller, Heikki Jarvinen, Stephan Juricke, Vassili Kitsios, Franois Lott, Valerio Lucarini, Salil Mahajan, Timothy N Palmer, Cecile Penland, Jin-Song Von Storch, Mirjana Sakradzija, Michael Weniger, Antje Weisheimer, Paul D Williams, Jun-Ichi Yano
More details from the publisher

Oceanic stochastic parametrizations in a seasonal forecast system

(2015)

Authors:

M Andrejczuk, FC Cooper, S Juricke, TN Palmer, A Weisheimer, L Zanna
More details from the publisher

Impact of Initial Conditions versus External Forcing in Decadal Climate Predictions: A Sensitivity Experiment*

Journal of Climate American Meteorological Society 28:11 (2015) 4454-4470

Authors:

Susanna Corti, Tim Palmer, Magdalena Balmaseda, Antje Weisheimer, Sybren Drijfhout, Nick Dunstone, Wilco Hazeleger, Jürgen Kröger, Holger Pohlmann, Doug Smith, Jin-Song von Storch, Bert Wouters
More details from the publisher

Impact of hindcast length on estimates of seasonal climate predictability

Geophysical Research Letters 42:5 (2015) 1554-1559

Authors:

W Shi, N Schaller, D Macleod, TN Palmer, A Weisheimer

Abstract:

It has recently been argued that single-model seasonal forecast ensembles are overdispersive, implying that the real world is more predictable than indicated by estimates of so-called perfect model predictability, particularly over the North Atlantic. However, such estimates are based on relatively short forecast data sets comprising just 20 years of seasonal predictions. Here we study longer 40 year seasonal forecast data sets from multimodel seasonal forecast ensemble projects and show that sampling uncertainty due to the length of the hindcast periods is large. The skill of forecasting the North Atlantic Oscillation during winter varies within the 40 year data sets with high levels of skill found for some subperiods. It is demonstrated that while 20 year estimates of seasonal reliability can show evidence of overdispersive behavior, the 40 year estimates are more stable and show no evidence of overdispersion. Instead, the predominant feature on these longer time scales is underdispersion, particularly in the tropics.
More details from the publisher

Impact of hindcast length on estimates of seasonal climate predictability

Geophysical Research Letters American Geophysical Union (AGU) 42:5 (2015) 1554-1559

Authors:

W Shi, N Schaller, D MacLeod, TN Palmer, A Weisheimer

Abstract:

It has recently been argued that single-model seasonal forecast ensembles are overdispersive, implying that the real world is more predictable than indicated by estimates of so-called perfect model predictability, particularly over the North Atlantic. However, such estimates are based on relatively short forecast data sets comprising just 20 years of seasonal predictions. Here we study longer 40 year seasonal forecast data sets from multimodel seasonal forecast ensemble projects and show that sampling uncertainty due to the length of the hindcast periods is large. The skill of forecasting the North Atlantic Oscillation during winter varies within the 40 year data sets with high levels of skill found for some subperiods. It is demonstrated that while 20 year estimates of seasonal reliability can show evidence of overdispersive behavior, the 40 year estimates are more stable and show no evidence of overdispersion. Instead, the predominant feature on these longer time scales is underdispersion, particularly in the tropics. KEY POINTS: Predictions can appear overdispersive due to hindcast length sampling errorLonger hindcasts are more robust and underdispersive, especially in the tropicsTwenty hindcasts are an inadequate sample size to assess seasonal forecast skill.
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