Gennadi Milinevsky National Antarctic Scientific Center of Ukraine, Kyiv National Taras Shevchenko University of Kyiv, Ukraine Ukraine.

Slides:



Advertisements
Similar presentations
Weather Review.
Advertisements

The toxicant XRF-analysis of gentoo penguin feather of Petermann Island colony, Antarctic Peninsula Andreev A.A. (1), Andreev A.V.(1), Shnyukov S.E. (1),
It all begins with the sun……
Troposphere-Ionosphere-Magnetosphere Coupling Study TIMIS EoI 803 (as part of ICESTAR/IHY) Yuri Yampolski (2), Valery Korepanov (1), Gennadi Milinevsky.
Climate change in the Antarctic. Turner et al, Significant warming of the Antarctic Winter Troposphere. Science, vol 311, pp Radiosonde.
SC.D CS The student knows that the water cycle is influenced by temperature, pressure, and the topography of the land. Content Limits: Items will.
Chapter 17: The Atmosphere
3. Climate Change 3.1 Observations 3.2 Theory of Climate Change 3.3 Climate Change Prediction 3.4 The IPCC Process.
NATS 101 Lecture 3 Climate and Weather. Climate and Weather “Climate is what you expect. Weather is what you get.” -Robert A. Heinlein.
1 NATS 101 Lecture 3 Climate and Weather. 2 Review and Missed Items Pressure and Height-Exponential Relationship Temperature Profiles and Atmospheric.
Focus on High Latitudes State of the Antarctic & Southern Ocean Climate System Authors: P. A. Mayewski, M. P. Meredith, C. P. Summerhayes, J. Turner, A.
Global Patterns & Relative Humidity
The Atmosphere Shreya Patel.
Antarctic Peninsula is a very suitable area for experimental investigations of troposphere-to-ionosphere energy transfer because this place characterized.
The Earths Weather. Layers of the Atmosphere  The atmosphere is divided into five layers. It is thickest near the surface and thins out with height until.
1. Meteorology Chapter 1 Introduction to the Atmosphere Meteorology \ Dr. Mazin sherzad.
 Atmosphere is a layer of gasses surrounding the earth  The atmosphere is made up of oxygen, nitrogen, argon carbon dioxide, some of helium, hydrogen,
 Weather Weather is over a short period of time Constantly changing, current condition of the atmosphere  Climate Climate is over a long period of.
6.4.8: Explain how convection affects weather patterns and climate.
EARTH’S CLIMATE. Latitude – distance north or south of equator Elevation – height above sea level Topography – features on land Water Bodies – lakes and.
Chapter 18 – Climate and Climate Change
Chapter 22 The Atmosphere
Chapter 3 The Changing Weather. Chapter 3 Terms Condensation Condensation Orographic Condensation Orographic Condensation Convectional Condensation Convectional.
Air, Weather, and Climate
Questions for Today:  What is Weather and Climate?  What are four major factors that determine Global Air Circulation?  How do Ocean Currents affect.
Russian proposals to Scientific program of Hydrometeorological observatory in framework of meteorological and radiation measurements (prepared by A. Makshtas)
Quasi-stationary planetary wave long-term changes in total ozone over Antarctica and Arctic A.Grytsai, O.Evtushevsky, O. Agapitov, A.Klekociuk, V.Lozitsky,
Polar Prediction The Scientific Challenges - Antarctica John Turner British Antarctic Survey Cambridge, UK.
Weather Review. Air Masses Air Mass – A large body of air through which temperature and moisture are the same. Types 1. Continental – formed over land.
Acoustic-gravity wave monitoring for global atmospheric studies Elisabeth Blanc 1 Alexis Le Pichon 1 Lars Ceranna 2 Thomas Farges 1 2- BGR / B3.11, Hannover,
 What is your view on climate change? Write down either: What you believe about climate change What you have heard someone say about climate change 
Atmosphere. Composition of the Earth’s Atmosphere The is a mixture of gases with some suspended solids and liquids. The atmosphere is a mixture of gases.
Autonomous Polar Atmospheric Observations John J. Cassano University of Colorado.
Environmental Science Chapter 7 Notes #1. Atmosphere Thin Layer of gases that surrounds the Earth Extends from the surface to 100’s of km’s above “Air”
Unit 4 Vocabulary The Atmosphere. 1. Storm surge – abnormal rise of the sea along a shore as a result of strong winds 2. local winds – winds causes by.
The Earth and Its Atmosphere
METEOROLOGICAL DATA COLLECTION NETWORK OF IMD. Meteorological instrument Observer Meteorological Observation (In situ & Remote sensing)
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Central Case: Charging toward cleaner air in London London has had bad.
CHARACTERISTICS OF THE ATMOSPHERE. Composition of Atmosphere  Made up mostly of Nitrogen (N)  Oxygen makes up a little more than 20%
Meteorology. The Atmosphere Compare the terms weather and climate. Weather refers to the state of the atmosphere at any given time and place. Climate.
1. The atmosphere 2 © Zanichelli editore 2015 Characteristics of the atmosphere 3 © Zanichelli editore 2015.
Climate and Global Change Notes 17-1 Earth’s Radiation & Energy Budget Resulting Seasonal and Daily Temperature Variations Vertical Temperature Variation.
Presentation by: Alex Hezik – Atmosphere, Weather, and Climate Layers of the Atmosphere troposphere: moderates flow of energy to Earth; where weather.
Chapter 1. Overview of the Earth’s Atmosphere  The atmosphere is a delicate life giving blanket of air surrounding the Earth.  Without the atmosphere.
ATMOSPHERE OBJECTIVE 1 1.What are the structural components of the
1 Air, Weather, and Climate. 2 2 Earth’s Atmosphere  Compared to the size of the Earth (12000 km), the atmosphere is a thin shell (120 km)  Composed.
How Convection Currents Affect Weather and Climate.
Chapter 2 Climate. Weather: the combination of temperature, humidity, precipitation, wind, cloudiness, and other atmospheric condition occurring at a.
Antarctic climate cooling and terrestrial ecosystem response 환경계획학과 환경관리전공 김지연.
Earth’s atmosphere Earth’s atmosphere is a thin layer of gases. It is unique in its composition and temperature so life can exist on Earth.
When Lower Atmosphere Waves Invade the Upper Atmosphere
Weather Jeopardy.
The Earth’s Atmosphere
The Atmosphere.
Chapter 15: Atmosphere.
The Atmosphere: Structure and Temperature
The Atmosphere Layers and aerosols.
Antarctica and climate change
The Atmosphere of Earth
Factors that Affect Climate
Earth’s Atmosphere.
Weather, Climate & Society ATMO 336 Climate vs. Weather
Atmosphere
WEATHER & CLIMATE Atmosphere Composition: - 78% Nitrogen - 21% Oxygen
OC3570 Operational Meteorology
NATS 101 Lecture 3 Climate and Weather
NATS 101 Lecture 3 Climate and Weather
Chapter 5 Ecosystems and the Physical Environment
NATS 101 Lecture 3 Climate and Weather
Air, Weather, and Climate
Presentation transcript:

Gennadi Milinevsky National Antarctic Scientific Center of Ukraine, Kyiv National Taras Shevchenko University of Kyiv, Ukraine Ukraine Antarctic research at Vernadsky station: results and prospects This work was partly supported by grant INTAS

Where and what research Ukraine provides in Antarctica? Task 1. Climate change at Antarctic Peninsula Task 2. Antarctic ozone hole Task 3. Sun-Earth energy transfer, space weather Other research (GPS, GIS, Biology, Medicine) Priorities of research Structure:

Task 1: Climate change at Antarctic Peninsula

Annual mean temperature in raised up to 2.5  С Warming in Antarctic Peninsula region Faraday/Vernadsky temperature,

- temperature - pressure - wind speed and direction - precipitation - humidity - snow level Meteorology and climate Modular Automatic Meteo Station – MAWS:

Sea water temperature anomaly +4.2  C

Antarctic Peninsula climate changes – impact on ecosystem Met Records Minimum temperature  C 1958 Maximum temperature  C 1985 Maximum gust 78 knots 1991 Deschampcia Antarctica

UV-A and UV-B measurements

The tide gauge for sea level measurements – climate warming

Sea water and salinity measurements at Barchans Islands hydrology site

Galindez Island aerial photograph, December 1956 (BAS, R.Thomas, 1963 ) Ice caps dynamics in Antarctic Peninsula climate change conditions

Galindez ice cap boundaries: Dec 1956 and Jan 2004 Since 1956 the Galindez ice cap area has decreased significantly

West part of Galindez ice cap changes м м м 3

Argentina Islands ice caps: prognosis for the future If the temperature trend left constant that the ice cap could be discharging within century This process could be increased due to unique water temperature anomaly observed last years (up to + 4°C)

Task 2: Antarctic Ozone Hole

Ozone measurements season

Longitude asymmetry in is rising Planetary wave in ozone layer

Displacement to East from  55°W to  0° Consequence: redistribution of UV radiation at sea level This changes may influence on regional climate and ecosystem During 30 years the asymmetry in ozone max and min positions enhanced

Task 3: Sun-Earth and troposphere-ionosphere energy transfer, space weather processes of energy distribution from the Earth surface to ionosphere height

Need to understand how solar energy affect the atmosphere and climate Solar effects are focused in polar regions

Ionosonde ISP-42 - radar for impulse ionosphere soundings Height: km Frequency: MHz Ionosphere soundings

Vernadsky Boston area Geomagnetic conjugate regions: Vernadsky – USA East Coast Channel for energy transfer from S-hemisphere to N-hemisphere

Magnetometer LEMI-008 Measurement range Resolution Range I nT 10 nT Range II nT 0.1 nT Bandwidth DC 1 Hz Time of sampling 1s, 2s, 5s, 10 s, 60 s Extremely low noise level – less than 5 pT at 1 Hz

The geomagnetic micropulsations Pc3 observed simultaneously at Vernadsky and Boston area

Troposphere Weather – Space Weather Drake Passage and Antarctic Peninsula –place for cyclones ~ 50 powerful cyclones annually Energy propagation from surface to ionosphereCyclon April 1, 1998

Magnetic field and pressure at Vernadsky Correlation AG waves

Idea: 1.The severe weather fronts is “projected” on ionosphere 120 km height 2.The delay of magnetic field response minutes (corresponded velocity m / s) 3.«Projection» of weather fronts to North hemisphere! Possible carrier? Atmosphere gravity waves AGW: Severe troposphere weather front “pull” the AGW

Search of planetary wave propagation to ionosphere heights: E-layer (120 km)

LEMI-112a induction magnetometer -ELF receiver: two orthogonal search-coil magnetometers -frequency band 0, Hz -low noise level – less than 0,03 pT/ at 10 Hz.

F2 layer height long-term changes : + - Faraday data, х – Vernadsky data Greenhouse effect cooling in mesosphere (90 km), “drop down” of ionosphere layers

in Vernadsky region and adjacent territory of Antarctic Peninsula Other research: Geodesy survey, GIS - GPS – gravimetric measurements

Permanent dual-frequency GPS receiver antenna installation at Vernadsky, Antarctica, April tectonics - total electron content - troposphere humidity

Biology, human biology and medicine HUMAN ADAPTATION

The toxicant XRF-analysis of gentoo penguin feather of Petermann Island colony, Antarctic Peninsula

“clean” hair “dirty” hair Ni, Cu, Pb, Se, Hg Cleaning of human body during winter XRF-analysis of the metals in the winterers hair

After winter the Cs amount in body essentially decreased Ukrainian winterers have usually increased amount of R/A Cs in body

Conclusion: Priorities of research Climate variability study ( ice cap ) Ozone hole (Oz and UV measurements) Upper atmosphere – Space Weather GIS of the Vernadsky region Creation of UA National Antarctic Database Providing the environmental monitoring Geodetic network – neotectonics Research equipment development