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Mike Blackburn
NCAS-Climate, University of Reading
 





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The Record Wet Autumn of 2000 in Western Europe

Mike Blackburn and Brian Hoskins

The Autumn (Fall) season of 2000 saw record rainfall and widespread flooding in western Europe. It was the wettest Autumn in England and Wales since records began in 1766, and several regions from France to Norway received double their average rainfall.

This exceptional weather was linked to a persistent large-scale pattern of unusual conditions stretching across the Atlantic and northern Europe, the "Scandinavia pattern", with low pressure near the UK and a strong Scandinavian ridge. A regression analysis has shown that wet UK Autumns during the preceding 40 years were also associated with this pattern.

Using a simplified numerical model of the global atmosphere, our research suggests that the pattern was triggered by unusually dry weather over the tropical west Atlantic and South America in Autumn 2000. Experiments using this (barotropic) model have shown that anomalous upper-level convergence and sinking of air in this region in Autumn would give rise to a Rossby wavetrain remarkably similar to the observed pattern over Europe.


The "Scandinavia pattern" of the Autumn flow had been identified previously as one of a number of patterns of northern hemisphere variability by Barnston and Livezey (1987, Mon. Wea. Rev., 115, 1083-1126), but had not been associated with wet Autumns in western Europe. The pattern was originally named "Eurasian Type-1" by Barnston and Livezey but it has subsequently been renamed the "Scandinavia pattern" in an extended version of their analysis at NOAA's Climate Prediction Centre (CPC). It is CPC's index of the strength of the pattern that we have used in this study.

Variations in the winter climate of western Europe have been linked to a different pattern, the North Atlantic Oscillation (NAO), in recent years. Since the 1960s the positive phase of NAO, with strengthened westerly flow into Europe, has become more prevalent in winter. In Autumn 2000, however, the phase of NAO varied from month to month so that, in the seasonal average, the observed flow did not project strongly onto the NAO pattern. In contrast, the period of wet Autumn weather coincided with persistence of the Scandinavia pattern, from its onset in mid September until its decay in mid December. In the subsequent winter months, which have also been wetter than average in the UK, the wet periods have coincided with further occurrences of the Scandinavia pattern.


This work is being submitted for publication.

Copy of a less specialist paper submitted 10/2001 (pdf).

Poster accompanying a talk at the Royal Meteorological Society Conference 09/2001 (A4 size pdf) (A0 size pdf).

Copy of an article in the UGAMP Newsletter No 24, 03/2001 (pdf).


DEFRA webpage on Autumn 2000 flooding.
DEFRA report on causes of the Autumn 2000 flooding.

Environment Agency flood reports index.
"Lessons Learned" Environment Agency report on the Autumn 2000 flooding.


European Flooding during Summer 2002

Mike Blackburn, Brian Hoskins, Pete Inness & Julia Slingo

UGAMP Newsletter article containing preliminary results of a study into the European flooding and the Indian monsoon failure during Summer 2002 (PDF).

Article on the European flooding and monsoon drought of Summer 2002, from the latest edition of NERC's Planet Earth publication (PDF).

A0 poster on Summer 2002 A0 poster: postscript : pdf

A4 poster: postscript : pdf

PDF version of a slide for the FREE meeting on Summer 2002.

Powerpoint presentation on 2002 European Floods, Indian Monsoon and ENSO (9.7Mbytes).

Monsoon online


Boscastle Flood, 16 August 2004

UK Met Office:
Boscastle flood rainfall observations and statistics.

NCAS news feature

Cambourne sounding for 12UTC on 16th August.
The atmosphere was close to moist-neutrality and was moist in depth. There was little directional wind shear up to the tropopause, with the wind almost parallel to the north Cornish coast.

Provisional data for precipitation averaged over England and Wales from the Met Office place 2004 as the 6th wettest August since records began in 1766. Monthly precipitation in 2004 was 151.8mm, compared with the long term average of 82.7mm and the 1961-1990 average of 77mm.
Plot of the historical data for August.

June/July 2007 UK Floods

During much of June and July 2007 the Atlantic jet-stream was displaced equatorward of its normal position (comparison). At the same time, a quasi-stationary wave pattern persisted from the north Pacific over north America and the Atlantic to Europe, with an upper-air trough close to the UK.
This large-scale environment led to weather systems tracking further south than normal towards the UK, and to in-situ developments associated with the upper-air potential vorticity (PV) anomaly over the UK.

Animation of the dynamical tropopause potential temperature, which includes the periods of intense rainfall on 25 June and 20 July. In each case there was a cold air anomaly over the UK, almost cut off, associated with a PV maximum in the upper troposphere (the period 29/06 - 05/07 is missing).

Walker Institute press release and meteorological context
CEH report
Met Office rainfall   May   June   July   JJA
June 25 - Yorkshire Floods
BBC Weather Centre summary

July 20 - Central/Southern England Floods
BBC Weather Centre summary
Hertmonceux sounding for 00UTC on 20 July.
Hertmonceux sounding for 12UTC on 20 July.
Ahead of the system at 00Z, the atmosphere was close to moist-neutrality, almost saturated through the depth of the troposphere, with total column water vapour ~30kg/m2. The sounding is unstable to a relatively small amount of lifting. By 12Z drier air aloft has reached Hestmonceux.


Special Issue of the Royal Meteorological Society's journal Weather on the 2007 Summer floods, including a paper by Blackburn, Methven and Roberts on the Large-scale context for the UK floods in summer 2007.

UK Flooding-related links

DEFRA Flood Management information.

Environment Agency Flooding information.

Foresight: UK Government Foresight project on Flooding & Coastal Defence.

CEH water research theme.

FREE, Flood Risk from Extreme Events is a NERC directed programme.

FRMRC, Flood Risk Management Research Consortium is an EPSRC-led programme.


Current research on Extreme Seasons

We are currently investigating persistent Atlantic weather regimes associated with extreme seasonal precipitation in the UK and parts of continental Europe during during Summer 2007 and Autumn 2000. This is a PhD project from October 2007 to September 2010, funding Ricardo Fonseca.


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National Centre for Atmospheric Science
Mike Blackburn   27 June 2013
NCAS-Climate
Department of Meteorology
University of Reading
PO Box 243, Reading RG6 6BB, UK

University of Reading