Climate change and the response of phenology of Great Tit, Collared Flycatcher, Summer Oak and herbivorous caterpillars during 1961 – 2007 in the Czech.

Slides:



Advertisements
Similar presentations
AgroCLIM software tool for effective calculation of agrometeorological indices ADAGIO & COST 734 Miroslav Trnka, Petr Hlavinka, Jan Balek, Josef Eitzinger,
Advertisements

NatureWatch program Plantwatch Canada: an example to integrate research activities in school.
LEPIDOPTERA LARVAE AS AN INDICATOR OF MULTI-TROPHIC LEVEL RESPONSES TO CHANGING SEASONALITY IN THE ARCTIC K. M. Daly, 1 H. Steltzer, 1 L. Gough, 2 M. Rich,
Phenology: Step Together Step ELF Activity: Biosphere 4A
PERUN: THE SYSTEM FOR SEASONAL CROP YIELD FORECASTING BASED ON THE CROP MODEL AND WEATHER GENERATOR Martin Dubrovský (1), Zdeněk Žalud (2), Mirek Trnka.
MAPPING ANIMAL FITNESS ONTO SEASONAL CLIMATE CHANGE F. Stephen Dobson Department of Biological Sciences College of Science & Mathematics.
The central theme of this project is to attempt to quantify the effect of riparian cover on stream water temperature at small spatial scales, with a view.
Dave Sauchyn, Ph.D., P.Geo. C-CIARN Prairies Prairie Adaptation Research Collaborative Senate Committee on Agriculture and Forestry Ottawa, December, 2002.
Results – climatic variables Temperature:  Local average air temperatures over have significantly increased during March, April and May in Fermoy.
North American snowfall variation from a unique gridded data set Daria Kluver Department of Geography University of Delaware.
Figures from : Thompson, D.W.J., M.P. Baldwin, and J.M. Wallace, 2001: Stratospheric connection to Northern Hemisphere wintertime weather: implications.
Early flowering of plants in the Northern Great Plains linked to increasing spring temperatures over 100 years Kelsey L. Dunnell & Steven E. Travers, Department.
Long Term Streamflow Forecast Validation Western Washington Watersheds Water Year 2004 If only we’d seen this one coming... Pascal Storck 3TIER Environmental.
Appendix K Phase 2 HGB Mid Course Review Average Minimum and Maximum Temperatures from at 9 Weather Stations in East Texas and West Louisiana.
Alan F. Hamlet Dennis P. Lettenmaier Center for Science in the Earth System Climate Impacts Group and Department of Civil and Environmental Engineering.
CORPUS CHRISTI CATHOLIC COLLEGE – GEOGRAPHY DEPARTMENT 1 How to draw a climate graph By the end of today’s lesson you will:  know how to draw a climate.
Presentation to Pre-Sessional Consultations on the IPCC TAR Milan, Italy November 2003 BRIAN CHALLENGER ANTIGUA AND BARBUDA.
The National Climate Assessment: Overview Glynis C. Lough, Ph.D. National Climate Assessment US Global Change Research Program National Coordination Office.
Plant material: 8-year-old saplings of European beech (Fagus sylvatica L.) and Norway spruce (Picea abies (L.) Karsten) were exposed for three growing.
12th EMS Annual Meeting & 9th European Conference on Applied Climatology (ECAC), Łódź, September 2012 Rajmund Przybylak, Aleksandra Pospieszyńska.
Interannual and Regional Variability of Southern Ocean Snow on Sea Ice Thorsten Markus and Donald J. Cavalieri Goal: To investigate the regional and interannual.
StateDivision Mean Winter Temperature CT 1 - Northwest26.9 +/ Central29.5 +/ Coastal31.9 +/ MA 1 - Western24.9.
Phenology: Step Together Step ELF Activity: Biosphere 4A
Expected Change of the Key Agrometeorological Parameters in Central Europe by 2050 Trnka M. 1,3, Štěpánek P. 2, Dubrovský M. 3, Semerádová D. 1,3, Eitzinger.
National Climatic Data Center NCDC "State of the climate" search/2008/ann/bams/.pdf and.ppt.
Climate Change Tendencies in Georgia under Global Warming Conditions Mariam Elizbarashvili 1 Marika Tatishvili 2 Ramaz Meskhia 2 Nato Kutaladze 3 1. Ivane.
Projection of uncertainties of the climate change scenarios into the estimates of future agrometeorological conditions and crop yields? M. Trnka (1,2),
Introduction Oithona similis is the most abundant copepod in the Gulf of Alaska, and is a dominant in many ecosystems from the poles to the sub-tropics.
3202 / 3200 / 3260 Climate Graphs WORLD GEOGRAPHY 3202 / 3200 / 3260 Climate Graphs Mr. Oliver H. Penney.
DATA ANALYSIS PROJECT SIMONE PHILLIPS 24 APRIL 2014 EAS 4480.
Quality control of daily data on example of Central European series of air temperature, relative humidity and precipitation P. Štěpánek (1), P. Zahradníček.
Validation of NARCCAP climate products for forest resource applications in the southeast United States. Willis Shem 1, Thomas Mote 2, Marshall Shepherd.
The climate and climate variability of the wind power resource in the Great Lakes region of the United States Sharon Zhong 1 *, Xiuping Li 1, Xindi Bian.
Ice Cover in New York City Drinking Water Reservoirs: Modeling Simulations and Observations NIHAR R. SAMAL, Institute for Sustainable Cities, City University.
The length of apricot phenophases is most significantly influenced by average and maximum temperature. Further statistical analyses show that minimum temperature.
Monthly Air Temperature Homogenization over France An example in department Vendée Anne – Marie WIECZOREK METEO – FRANCE.
APPLICATION OF THE WEATHER GENERATOR IN PROBABILISTIC CROP YIELD FORECASTING Martin Dubrovský (1), Zdeněk Žalud (2), Mirek Trnka (2), Jan Haberle (3) Petr.
Martine Rebetez Summer 2003 maximum and minimum daily temperatures over a 3300 m altitudinal range Martine Rebetez.
Investigations of long and short term changes in Total Ozone at the Sonnblick Observatory (3106 m, Austria) S. Simic, P. Weihs and G. Rengarajan and W.
Chitu, E. Topor, E. Paltineanu, C. R. Dumitru, I. M. Sumedrea, D. Chitu, V. Ionita, A. D. Filipescu, L. Research Institute for Fruit Growing Pitesti -
Spring Budburst Study A Research project Model Secondary School for the Deaf Indiana School for the Deaf Spring 2007.
Herbivore Trophic Dynamics: Potential Influences of Climate Warming Brad Griffith USGS, Alaska Cooperative Fish and Wildlife Research Unit University of.
Research & Systematic Observations (IX) Vulnerability Assessment, Impacts and Adaptation Measures (VII) Research & Systematic Observations (IX) Vulnerability.
Experience regarding detecting inhomogeneities in temperature time series using MASH Lita Lizuma, Valentina Protopopova and Agrita Briede 6TH Homogenization.
ESTIMATING THE CROP YIELD POTENTIAL OF THE CZECH REPUBLIC IN PRESENT AND CHANGED CLIMATES Martin Dubrovsky (1) Mirek Trnka (2), Zdenek Zalud (2), Daniela.
Chapter 04 Author: Lee Hannah. FIGURE 4.1 Accelerating Ice Break up and Delayed Ice Formation. Ice break up and formation is shown for major rivers and.
Correlation Between Precipitation and Temperature by Solaleh Khezri.
Indicators for Climate Change over Mauritius Mr. P Booneeady Pr. SDDV Rughooputh.
The evaluation of phenological phases of plants in a flood-plain forest of southern Moravia in 1961 – 2007 Lenka Bartošová (1), Zdeněk Bauer (1), Miroslav.
GLOBAL WARMING IMPACTS. Fig_06_01 Departures from March temperatures (NASA)
IMPLICATIONS OF CLIMATE CHANGE FOR NORTH AMERICAN WOOD WARBLERS (PARULIDAE) Paul K. Strode INTRODUCTION Recent investigations of long-term ecological data.
Changes in the Melt Season and the Declining Arctic Sea Ice
Topic 10 - Ecosystems.
The Pattern of Change in U.S. Streamflow
Ecological responses to climate change
Huyck Preserve Phenology Project
~100 yrs of global temperature trends predictions
Climate Graphs What do they tell us?.
Climate Graphs What do they tell us?.
Using Remote Sensing to Monitor Plant Phenology Response to Rain Events in the Santa Catalina Mountains Katheryn Landau Arizona Remote Sensing Center Mentors:
STATISTICAL AGENCY UNDER PRESIDENT OF THE REPUBLIC OF TAJIKISTAN
Trends in Iowa Precipitation: Observed and Projected Future Trends
Land surface phenology versus traditional observations
Extension Climate Science Team
An Analysis of Possibilities of Forecasting the AVISO Agrometeorological Model Input   Münster P. Chuchma F.
3Institute of Geography, Masaryk University, Brno, Czech Republic
Introduction to Phenology
EMS Annual Meeting 2017, Dublin
What is winter? A reckoning for seasonally snow-covered, social-ecological systems B33M-2848 Alexandra R. Contosta1, Nora J. Casson2, Sarah.
Presentation transcript:

Climate change and the response of phenology of Great Tit, Collared Flycatcher, Summer Oak and herbivorous caterpillars during 1961 – 2007 in the Czech Republic Lenka Bartošová (1), Miroslav Trnka (1), Zdeněk Bauer (1), Petr Štěpánek (2), Jana Bauerová (1), Martin Možný (3), Zdeněk Žalud (1) (1) Institute for Agrosystems and Bioclimatology, Mendel University of Agriculture and Forestry Brno, Czech Republic, (2) Department of Climatology and Meteorology, Czech Hydrometeorological Institute Brno, Czech Republic (3) Agrometeorological observatory in Doksany, Czech Hydrometeorological Institute, Doksany, Czech Republic phenological input data t-test, Kendall Rank Correlation test for significance in trends coherency analyses – at 95% and 99% confidence levels for pheno and meteo series Pearson and Spearman correlation coefficient for pairs of pheno stages meteorological parameters INTRODUCTION On this poster we present phenology of Great Tit, Collared Flycatcher, Summer Oak and herbivorous caterpillars within flood plain forest ecosystem during 1961 and Phenophases of species mentioned above have shifted during last 47 years to the earlier time and therefore the study focuses on the mutual influence of shifts in phenology of individual species in this simplified trophic chain and its overall stabillity. AIMS - to find out how shifting of phenophases affect trophic chain of observed species - to analyse if happen mistiming of individual phenophases - to clarify how temperature in particular period correlate with development of phenophases STUDY AREA - 4 research plots of biogeocenoses group Ulmi- fraxineta carpini pairs of Great Tit, 3437 pairs of Collared Flycatcher - 2 species of caterpillars: Winter Moth (Operophtera brumata) and Tortrix Moth (Tortrix viridana) - bud break and full foliage of Summer Oak METHODOLOGY Onset of phenophases of a) Summer Oak where the dashed line is bud bursting and continuous line is full foliage; b) Great Tit, for both bird populations the dashed line is FLD (first laying date) and solid line is MLD (mean laying date); c) peak of caterpillar, where the dashed line is start and solid line is end of excrement fall- down; d)Collared Flycatcher RESULTS 1. shifting of phenophases4. onset of phenophases Onset of phenological stages during individual decades of the record. The white bar indicates range of mean and ± st. dev. with mean value being depicted by vertical line. The extend of black bars indicate minimum and maximum values in the individual periods. 2. coherency analysis Coherency analysis between accumulated maximum temperatures above 8°C and Summer Oak bud burst, Great Tit MLD, start of caterpillar peak season and Collared Flycatcher MLD. The sum of maximum temperatures was accumulated for period of Summer Oak: January 1 – April 25, Great Tit: January 1 – April 10, caterpillar: January 1 – April 30, Collared Flycatcher: March 1 – May coherency analysis II Coherency analysis of selected pairs of phenophases at selected location. 1) Summer Oak bud burst – beginning of caterpillar season; 2) Summer Oak full foliage – end of caterpillar season; 3) Summer oak bud burst – Great Tit MLD; 4) beginning of caterpillar season – Great Tit MLD, 5) end of caterpillar season – Great Tit MLD; 6) beginning of caterpillar season – Collared Flycatcher MLD; 7) end of caterpillar season – Collared Flycatcher MLD; 8) Great Tit MLD – Collared Flycatcher MLD. CONCLUSION - results for sum of maximum daily temperatures above 8°C and for onset of phenological stages of all the species studied exceeded the 95% and 99% confidence levels for frequencies above 20 years - the mutual timing of the phenological stages in simplified trophic chain do not be affected by shifting of phenophases. Phenophases are separating or overlaying in some years but there is no disruption of the food chain. There has been a consistent shift towards earlier onset of individual phenophases over the last 47 years - Summer Oak bud bursting has shifted on average by 7.9 days and full foliage by 8.9 days, MLD has advanced on average by 7.8 days for the Great Tit and by 8.7 days for Collared Flycatcher and the activity of caterpillars has advanced by 8.7 days Acknowledgements: The study was supported by the project Grant Agency of the Czech Republic (no. 521/08/1682), Research plan No. MSM “Biological and technological aspects of sustainability of controlled ecosystems and their adaptability to climate change” and KONTAKT OC 187 (linked to COST 734).