Published September 2018 | Version v1
Journal article

Blocking and its Response to Climate Change

  • 1. University of Oxford, Department of Physics, Atmospheric, Oceanic and Planetary Physics (United Kingdom)
  • 2. Consejo Superior de Investigaciones Científicas - Universidad Complutense de Madrid (CSIC-UCM), Instituto de Geociencias (IGEO) (Spain)
  • 3. University of Reading, Department of Meteorology (United Kingdom)
  • 4. Seoul National University, School of Earth and Environmental Sciences (Korea, Republic of)
  • 5. University of Bern, Institute of Geography, Oeschger Centre for Climate Change Research (Switzerland)
  • 6. University of Reading, National Centre for Atmospheric Science (United Kingdom)
  • 7. Center for International Climate Research (CICERO) (Norway)
  • 8. University of Missouri, Atmospheric Science Program, School of Natural Resources (United States)
  • 9. ETH Zürich, Institute for Atmospheric and Climate Science (Switzerland)

Description

Purpose of Review

Atmospheric blocking events represent some of the most high-impact weather patterns in the mid-latitudes, yet they have often been a cause for concern in future climate projections. There has been low confidence in predicted future changes in blocking, despite relatively good agreement between climate models on a decline in blocking. This is due to the lack of a comprehensive theory of blocking and a pervasive underestimation of blocking occurrence by models. This paper reviews the state of knowledge regarding blocking under climate change, with the aim of providing an overview for those working in related fields.

Recent Findings

Several avenues have been identified by which blocking can be improved in numerical models, though a fully reliable simulation remains elusive (at least, beyond a few days lead time). Models are therefore starting to provide some useful information on how blocking and its impacts may change in the future, although deeper understanding of the processes at play will be needed to increase confidence in model projections. There are still major uncertainties regarding the processes most important to the onset, maintenance and decay of blocking and advances in our understanding of atmospheric dynamics, for example in the role of diabatic processes, continue to inform the modelling and prediction efforts.

Summary

The term 'blocking' covers a diverse array of synoptic patterns, and hence a bewildering range of indices has been developed to identify events. Results are hence not considered fully trustworthy until they have been found using several different methods. Examples of such robust results are the underestimation of blocking by models, and an overall decline in future occurrence, albeit with a complex regional and seasonal variation. In contrast, hemispheric trends in blocking over the recent historical period are not supported by different methods, and natural variability will likely dominate regional variations over the next few decades.

Additional details

Identifiers

Publishing Information

Journal Title
Current Climate Change Reports
Journal Volume
4
Journal Issue
3
Journal Page Range
p. 287-300
ISSN
2198-6061

INIS

Country of Publication
Germany
Country of Input or Organization
International Atomic Energy Agency (IAEA)
INIS RN
51016350
Subject category
S54: ENVIRONMENTAL SCIENCES;
Descriptors DEI
CLIMATE MODELS; CLIMATES; CLIMATIC CHANGE; SEASONAL VARIATIONS; SIMULATION; STORMS; WEATHER
Descriptors DEC
MATHEMATICAL MODELS; VARIATIONS

Optional Information

Copyright
Copyright (c) 2018 The Author(s)