Marija Mokorić and Lovro Kalin

Slides:



Advertisements
Similar presentations
AGENZIA REGIONALE PER LA PROTEZIONE DELLAMBIENTE DELLA SARDEGNA ARPAS Andrea Motroni Climate, climate change and desertification.
Advertisements

Large Scale Patterns of Climatic Variations Amanda Rosenberger Photo :
The comparation of weather types in the years of extreme drought over Croatia Dunja Plačko-Vršnak, Krunoslav Mikec, Marija Mokorić Meteorological and Hydrological.
CO2 (ppm) Thousands of years ago Carbon dioxide concentrations over the last.
Class #7: Thursday, July 15 Global wind systems Chapter 10 1Class #7, Thursday, July 15, 2010.
Standardized Precipitation Index for Croatia Krešo Pandžić, Tanja Likso Meteorological and Hydrological Service, Grič 3, Zagreb
Explaining Changes in Extreme U.S. Climate Events Gerald A. Meehl Julie Arblaster, Claudia Tebaldi.
Summer 2010 Forecast. Outline Review seasonal predictors Focus on two predictors: ENSO Soil moisture Summer forecast Look back at winter forecast Questions.
Seasonal outlook of the East Asian Summer in 2015 Motoaki Takekawa Tokyo Climate Center Japan Meteorological Agency May th FOCRAII 1.
12th EMS Annual Meeting & 9th European Conference on Applied Climatology (ECAC), Łódź, September 2012 Rajmund Przybylak, Aleksandra Pospieszyńska.
Making Connections Chapter 12
U1LG3: Climates & Biomes Criteria for Success:
WEATHER, CLIMATE, and SEASON Arabejo, Mary Claire M. Sarabillo, Weena A. NatSci –A7 March 22, 2012.
Ocean Circulation Winds and Currents. The __________________ and the ___________________ interact The ocean and atmosphere transport heat from the ______________________________.
Global Climates. ► Weather: short-term condition of the atmosphere ► Climate: long-term conditions of the atmosphere, including averages and extremes.
The trend analysis demonstrated an overall increase in the values of air temperatures as well as an increase in the occurrence of extremely hot days, but.
Chapter 18 – Climate and Climate Change
The La Niña Influence on Central Alabama Rainfall Patterns.
THE GLOBAL CLIMATE WEATHER CLIMATE The condition of atmosphere at any particular time and place. It’s always changing The synthesis of weather, the average.
Long-term changes in frequencies of wind directions on the western coast of Estonia Jaak Jaagus Institute of Geography, University of Tartu Second International.
Warm-Up!!!!!!!!!!! What country has the coldest average temperature in the world? What country has the hottest average temperature in the world? Where.
Tamas Kovacs Hungarian Meteorological Service Climatology Division Seasonal forecast and an outlook for Winter 2013/14 in Hungary Tamas Kovacs - 10th Session.
C20C Workshop, ICTP Trieste 2004 The impact of stratospheric ozone depletion and CO 2 on tropical cyclone behaviour in the Australian region Syktus J.
MET 10 1 MET 10 Weather and Climate MET 10 Weather and Climate: Lecture 14 Global Climate Dr. Eugene Cordero Fall 2003 San Jose State University Reading:
BRITISH WEATHER. What is the British weather like? The climate is generally mild and temperate. The temperature is subject of two extremes: it is rarely.
THE FOUR SEASONS. A SEASON is one of the four periods of the year. Each season--spring, summer, autumn, and winter--lasts about three months and brings.
WMO-JMA Public Forum Workshop of the World Conference on Disaster Reduction: Reducing Risks of Weather, Climate and Water Extremes through Advanced Detecting,
Climate monitoring information on the Mediterranean Peter Bissolli Deutscher Wetterdienst (DWD, Germany), Dep. Climate Monitoring WMO RA VI Regional Climate.
INTRODUCTION Recent efforts within the National Weather Service’s Southern Region (NWS-SR) to refine criteria for excessive heat revealed high occurrences.
Global Climates. ► Weather: short-term condition of the atmosphere ► Climate: long-term conditions of the atmosphere, including averages and extremes.
“CLIMATE IS WHAT WE EXPECT, AND WEATHER IS WHAT WE GET” ~ MARK TWAIN.
What Causes Climate? Notes. Introduction A climate is the average, year-after- year weather conditions in an area. Two factors are important in describing.
ENVIRONMENTAL SCIENCE TEACHERS’ CONFERENCE ENVIRONMENTAL SCIENCE TEACHERS’ CONFERENCE, Borki Molo, Poland, 7-10 February 2007 Extreme Climatic and atmospheric.
The South American Monsoon System: Recent Evolution and Current Status Update prepared by Climate Prediction Center / NCEP 4 June 2012 For more information,
Ocean Circulation Winds and Currents. The atmosphere and the oceans interact The ocean and atmosphere transport heat from the equatorial regions to the.
Factors That Affect Climate. Identify five factors that affect climate and explain how each affects climate.
Climate: Climate: Factors that Affect Climate Page 631.
Climate.
World Geography Chapter 3
Acknowledgment: Trinh Tuan Long for TC movie and tracks Interannual variability of heavy rainfall over Central Vietnam Kim Nguyen, Jack Katzfey and John.
Effects of Latitude and Climate  Weather is the condition of the atmosphere at a specific place and time. 3.2 Terrestrial Biomes  One of the keys to.
Climate Change Observation, Inference & Prediction
Climate!.
CLIMATOLOGY OF CHINA AUTUMN.
5th International Conference on Earth Science & Climate Change
BFB Mid-latitude Cyclones
CLIMATE CHANGE IN TRINIDAD AND TOBAGO Willis Mills.
The Climate in Tunisia.
José J. Hernández Ayala Department of Geography University of Florida
Weather patterns and storms
Country Presentation SASCOF September 2016 Maldives
CLIMATE Key question #10 What is the difference between climate and weather? How do we pictorially represent climate over a year?
What Causes Climate? Notes.
Climate Factors.
Large Scale Patterns of Climatic Variations
Factors that Affect Climate
Weather vs. Climate? Weather: Atmospheric conditions (temperature, rainfall, etc…) at a specific point in time and specific place. Climate: Atmospheric.
What Causes Climate? Notes.
Southern Company Summer 2018 Outlook & Winter Review
Climates of the Earth Ch. 3: Climates of the Earth
Unit 3 Lesson 6 What Factors Affect Climate?
Earth & Sun.
What Causes Climate? Notes.
1 GFDL-NOAA, 2 Princeton University, 3 BSC, 4 Cerfacs, 5 UCAR
Large Scale Patterns of Climatic Variations
CLIMATE.
Changes in surface climate of the tropical Pacific
U1LG3: Climates & Biomes Criteria for Success:
What Causes Climate? Notes.
Southern Company Summer 2019 Outlook & Winter Review
Presentation transcript:

Analysis of atmospheric circulation changes over the Adriatic coast in warm period 1981-2010. Marija Mokorić and Lovro Kalin Meteorological and Hydrological Service of Croatia 12th EMS Annual Meeting & 9th European Conference on Applied Climatology, Łódź, Poland

outline introduction analysis conclusions and future work Croatia: summer months climate conditions recent changes analysis weather types (upper atmosphere) conclusions and future work 12th EMS Annual Meeting & 9th European Conference on Applied Climatology, Łódź, Poland

introduction In the last decade it was observed that the period of relative dry weather has been extended to July, and to the end of August and September more frequent months with less precipitation and higher air temperature, compared to climatological average longer firefighting season 12th EMS Annual Meeting & 9th European Conference on Applied Climatology, Łódź, Poland

introduction a large number of fires appeared in period 2001-2010 not only on the coast, but for the first time in the mountain region since 2005 the most dangerous fires appeared at the end of August and first part of September, when the extreme fires are not so common 12th EMS Annual Meeting & 9th European Conference on Applied Climatology, Łódź, Poland

weather types to find a possible explanation of such behaviour, an analysis of the upper atmosphere circulation was done for period 1981-2010 fires are connected with weather types and atmospheric circulation mean monthly circulation AT 500 hPa (~5.5 km) on the Northern hemisphere (Deutsche Wetterdienst) period 1981-2010 for June, July, August and September the weather pattern typing is done manually 12th EMS Annual Meeting & 9th European Conference on Applied Climatology, Łódź, Poland

weather types DRY WET eight main atmospheric circulation patterns Bischoff and Vargas (2003): upper cyclone CY upper through TR front side of upper through (south-west str.) SW west-stream W back side of upper through (north-west str.) NW upper atmospheric ridge R non-gradient field NG front side of the ridge FR DRY WET 12th EMS Annual Meeting & 9th European Conference on Applied Climatology, Łódź, Poland

back side of the trough (NW stream) source: Deutscher Wetterdienst 12th EMS Annual Meeting & 9th European Conference on Applied Climatology, Łódź, Poland

source: Deutscher Wetterdienst front side of the ridge source: Deutscher Wetterdienst 12th EMS Annual Meeting & 9th European Conference on Applied Climatology, Łódź, Poland

source: Deutscher Wetterdienst upper ridge source: Deutscher Wetterdienst 12th EMS Annual Meeting & 9th European Conference on Applied Climatology, Łódź, Poland

source: Deutscher Wetterdienst non-gradient field source: Deutscher Wetterdienst 12th EMS Annual Meeting & 9th European Conference on Applied Climatology, Łódź, Poland

source: Deutscher Wetterdienst west stream source: Deutscher Wetterdienst 12th EMS Annual Meeting & 9th European Conference on Applied Climatology, Łódź, Poland

front side of the trough (SW stream) source: Deutscher Wetterdienst 12th EMS Annual Meeting & 9th European Conference on Applied Climatology, Łódź, Poland

source: Deutscher Wetterdienst upper trough source: Deutscher Wetterdienst 12th EMS Annual Meeting & 9th European Conference on Applied Climatology, Łódź, Poland

source: Deutscher Wetterdienst upper cyclone source: Deutscher Wetterdienst 12th EMS Annual Meeting & 9th European Conference on Applied Climatology, Łódź, Poland

summer - autumn at the beggining of autumn, weather conditions change 12th EMS Annual Meeting & 9th European Conference on Applied Climatology, Łódź, Poland

in 2000’s occurence of ‘dry’ weather types (NG, NW) has increased June... 80’s TR NW W SW 90’s NG R 00’s FR in 2000’s occurence of ‘dry’ weather types (NG, NW) has increased 12th EMS Annual Meeting & 9th European Conference on Applied Climatology, Łódź, Poland

since 2005, occurence of ‘dry’ weather types (NG, NW) has increased September... 80’s W NG NW SW R TR 90’s 00’s since 2005, occurence of ‘dry’ weather types (NG, NW) has increased 12th EMS Annual Meeting & 9th European Conference on Applied Climatology, Łódź, Poland

conclusions in July and August no significant change is observed since 2005, in June and September occurence of ‘dry’ weather types (NG, R) has increased hot and dry season has expanded matches well with fire-fighter’s experience 12th EMS Annual Meeting & 9th European Conference on Applied Climatology, Łódź, Poland

future work go into more detailed analysis spatial (northern and southern Adriatic) temporal (order of weeks, days...) 12th EMS Annual Meeting & 9th European Conference on Applied Climatology, Łódź, Poland

references Bischoff S. A. and Vargas W. M. (2003): The 500 and 1000 hPa weather type circulations and their relationship with some extreme climatic conditions over southern South America. Internationa Journal of Climatology, 23, 541-556 Lončar, E. and Bajić, A. (1993): Weather types in Croatia (in Croatian). Croatian Meteorological Journal, 29, 31-45 Mokorić, M (1998): The Weather Types on Adriatic Coast of Croatia during the Season of Forest Fire Protection, Proceedings of III International Conference on Forest Fire Research, Coimbra-Luso, 1, 1305-1309; 12th EMS Annual Meeting & 9th European Conference on Applied Climatology, Łódź, Poland

Thank you for your attention! 12th EMS Annual Meeting & 9th European Conference on Applied Climatology, Łódź, Poland