Jet-stream images For BBC programme Five Miles High Mike Blackburn, Brian Hoskins University of Reading August 2007 Colours on the maps show wind speed.

Slides:



Advertisements
Similar presentations
Unit 9 It's warm 清丰县第一实验小学 唐利娟.
Advertisements

Last week, we looked at rain, wind and clouds
Adaptation to heat waves occurrence in France S. Planton*, M. Gillet**, M. Déqué*, and J. Manach* *Météo-France, CNRM ** « Observatoire National sur les.
CLIMATE.
ECMWF Training Course 2009 – NWP-PR
1 How does relief affect temperature? 2 Hurricanes are associated with which type of pressure?
© University of Reading TAC-3 Conference June 2012 The dependence of contrail formation on weather pattern and altitude.
The European flooding of summer 2002 and its global connections Mike Blackburn, Brian Hoskins, Pete Inness, Julia Slingo Centre for Global Atmospheric.
Atmospheric Teleconnections and Climate Change
The European flooding of summer 2002 and its global connections Mike Blackburn, Brian Hoskins, Pete Inness, Julia Slingo Centre for Global Atmospheric.
Large-scale context for the UK floods in Summer 2007 Submitted to Weather, 14 May 2008 Mike Blackburn 1 John Methven 2 and Nigel Roberts 3 (1) National.
1 NCAS SMA presentation 14/15 September 2004 The August 2002 European floods: atmospheric teleconnections and mechanisms Mike Blackburn (1), Brian Hoskins.
August-September 2012 Slides for Met Office Seasonal Forecast Discussion 20 September 2012 Mike Blackburn National Centre for Atmospheric Science, University.
Blocking and regime transitions Tim Woollings With thanks to: Brian Hoskins, Abdel Hannachi, Christian Franzke, Joaquim Pinto, Joao Santos, Olivia Martius,
AGENZIA REGIONALE PER LA PROTEZIONE DELLAMBIENTE DELLA SARDEGNA ARPAS Andrea Motroni Climate, climate change and desertification.
Russian Summer Heat Wave 2010: Climatological Background and Intraseasonal Evolution Igor Zveryaev, Yulia Zyulyaeva Sergey Gulev, Klaus Peter Koltermann.
Recurring Weather.
Global Precipitation Precipitation averages just about 1 meter per year over Earth but, like wealth, varies widely from place to place and from time to.
“Traditional” terminology
Through a PowerPoint presentation participants will have a broad understanding of the Nevada fire situation during August, 2006 thereby beginning the.
Flash Flood Climatology for the Goodland County Warning Area 13 th High Plains Conference August 27, 2009.
Global Average Barometric Pressure: January
The Island Akiba. Factors Contributing to Climate Location Ocean Currents Unique Physical Features Wind patterns.
Summer Weather and Bushfire Threats in SE Australia Tony Langdon VK3JED for the VoIP Weather Net November
Important Maps of Europe
Mid-latitude Climates
The Climate in Britain. Weather vs. Climate Weather refers to the short term conditions of the atmosphere on a local scale. Climate refers to the long.
The Potential for Skill across the range of the Seamless-Weather Climate Prediction Problem Brian Hoskins Grantham Institute for Climate Change, Imperial.
Blocking and Rossby Wave-breaking
Review of Northern Winter 2010/11
Upper-level Mesoscale Disturbances on the Periphery of Closed Anticyclones Thomas J. Galarneau, Jr. and Lance F. Bosart University at Albany, State University.
Overview Northern hemisphere extra-tropics El Niño Seasonal Climate – Winter Mike Blackburn Seasonal Climate Discussion, 14 April 2010.
ACCENT/GLOREAM 2006, October, Paris Photo-oxidants formation and transport over Europe during the heat wave period in July 2006 Joanna Struzewska.
AIR MASSES A large body of air (thousands of miles) Changes in weather are caused by movements of air masses As an air mass moves away, temp & humidity.
Factors which influence climate Today’s Aim - 1.To learn the different factors that affect climate. Keywords Latitude, Equator, Sea Breeze, Prevailing.
Level 5 What are the reasons for British Weather and Climate? We will learn about:- Low Pressure (Depression) weather High pressure (Anticyclone) weather.
Air Masses and Fonts Chapter 8 Section 3.
Convectively Coupled Kelvin Waves Multi-Scale Study Over Africa in 2011 Matthew Janiga.
Climate in Ireland. Ireland has an oceanic climate which is mainly determined by the Atlantic Ocean which lies to the west coast of the island. Due to.
Japan 2012 Summer 2012 Central Europe – spring 2013 Greenland – summer 2012 Black Sea A Smörgåsbord of Wacky Weather… Europe Texas March 2012 in Burlington,
Understanding jet streams. What are jet streams? Jet streams are narrow, fast- moving air currents (winds). They are found at high altitude, at the boundary.
Why does it rain so much in the UK? Add in as many answers as possible.
The La Niña Influence on Central Alabama Rainfall Patterns.
Seasonal Cycle, Monsoons and Tropical Convergence Zones Vernon E. Kousky NOAA/ Climate Prediction Center February 2013.
Introduction #2 C Global Patterns. The first two slide shows in this introduction illustrated the importance of the sun’s solar energy and how it effects.
Factors That Affect Climate. Latitude Ocean currents Winds and Air masses Elevation Relief Near Water.
Materials Adapted from The University of Georgia
Anticyclones The calm and still ones. Characteristics of anticyclones  You know the routine – pens and the whiteboard  Just think opposite of depressions.
1 Last week, we looked at rain, wind and clouds This week we are going to look at weather in different parts of the UK.
Air Masses and Fronts METR April Air Mass: a large volume of air that has remained over a surface for a long enough period of time to be.
Avinashmatta.blogspot.com Monsoons. What are monsoons The word "monsoon" is derived from the Arabic word "mausim" which means season. Ancient traders.
March 8, 2013 Steve Baxter Monthly Climate Review February 2013.
II. Climate Regions A. Wind and Water – 1. Because Europe is farther north than the United States, you might think it has a colder climate. a) In fact,
Air Masses and Fronts.
Weather National 5 supported study
Oliver Elison Timm ATM 306 Fall 2016
UK Climate is Temperature – Cool, Wet Winters and Warm, Wet Summers
World Climate Zones.
MID-LATITUDE WEATHER SYSTEMS: PART IV: SURFACE-UPPER AIR LINKAGE
Overview of East Asian Summer Monsoon etc
Is air moving away or towards each of these pressure centers?
ATMS790: Graduate Seminar, Yuta Tomii
Precipitation Climatology of Costa Rica and its Variability
Air Masses and Fronts.
500 hPa height , surface pressure
Season & Weather Unit 5 The four seasons.
U.S. Air Masses.
S4 – Weather Unit Image copyright Joseph Kerski.
Four Seasons! By izabelle.
Presentation transcript:

jet-stream images For BBC programme Five Miles High Mike Blackburn, Brian Hoskins University of Reading August 2007 Colours on the maps show wind speed Arrows show the wind direction all values are in metres per second Slightly more than double (x2.2) to get miles per hour

Climatological jet-streams Northern Winter DJFSouthern Summer DJF

Climatological jet-streams Northern Summer JJASouthern Winter JJA

Extreme seasons Northern Winter (Climatology)Northern Winter 1963 Not very clear – next slide better – Atlantic sector

Extreme seasons Northern Winter (Climatology)Northern Winter 1963 Note colour scale ms -1 Persistent blocking anticyclone, diverting the jetstream Leads to cold winters in western Europe (more continental)

Extreme seasons Northern Summer (Climatology)Northern Summer 1976 Note colour scale ms -1 Persistent blocking anticyclone, diverting the jetstream Leads to hot summers in western Europe (more continental)

Extreme seasons Northern Summer (Climatology)Northern Summer 2007 Note colour scale ms -1 Very wet in UK and surrounding countries Major UK rainfall events: June 13-15; June 25, July 20 Persistent waves on the jet-stream, with a trough of low pressure near the UK

Summer 2007 animation Northern Summer day averages Wind speed at 250 hPa This is an animation in.gif format