Troposphere-Ionosphere-Magnetosphere Coupling Study TIMIS EoI 803 (as part of ICESTAR/IHY) Yuri Yampolski (2), Valery Korepanov (1), Gennadi Milinevsky.

Slides:



Advertisements
Similar presentations
Jan Cisak, PolandAGS 2002, Wellington, New Zealand Atmospheric Impacts on GPS observations in Antarctica.
Advertisements

Chapter 3 – Radio Phenomena
HOW DOES MY SIGNAL GET FROM HERE TO THERE? By Forest Cummings, W5LQU And Dave Russell, W2DMR.
Study of Pi2 pulsations observed from MAGDAS chain in Egypt E. Ghamry 1, 2, A. Mahrous 2, M.N. Yasin 3, A. Fathy 3 and K. Yumoto 4 1- National Research.
Gennadi Milinevsky National Antarctic Scientific Center of Ukraine, Kyiv National Taras Shevchenko University of Kyiv, Ukraine Ukraine.
23 rd ECRS The stratospheric polar vortex as a cause for the temporal variability of solar activity and galactic cosmic ray effects on the lower atmosphere.
Cosmic Ray Using for Monitoring and Forecasting Dangerous Solar Flare Events Lev I. Dorman (1, 2) 1. Israel Cosmic Ray & Space Weather Center and Emilio.
Wavelength The distance between one point on a wave and another point exactly like it.
Using a DPS as a Coherent Scatter HF Radar Lindsay Magnus Lee-Anne McKinnell Hermanus Magnetic Observatory Hermanus, South Africa.
THE AUSTRALIAN NATIONAL UNIVERSITY Infrasound Technology Workshop, November 2007, Tokyo, Japan OPTIMUM ARRAY DESIGN FOR THE DETECTION OF DISTANT.
– Ukrainian input in ILWS program O. FEDOROV Institute of Space Research, Kyiv, Ukraine V. KOREPANOV Lviv Centre of Institute of Space Research, Lviv,
Lecture-15 1 Lecture #15- Seismic Wave Overview. Lecture-15 2 Seismograms F Seismograms are records of Earth’s motion as a function of time.
DETECTION OF UPPER LEVEL TURBULENCE VIA GPS OCCULTATION METHODS Larry Cornman National Center for Atmospheric Research USA.
Reconstructing Active Region Thermodynamics Loraine Lundquist Joint MURI Meeting Dec. 5, 2002.
Satellite observation systems and reference systems (ae4-e01) Signal Propagation E. Schrama.
Naval Weapons Systems Energy Fundamentals Learning Objectives  Comprehend basic communication theory, electromagnetic (EM) wave theory  Comprehend.
TEC and its Uncertainty Ludger Scherliess Center for Atmospheric and Space Sciences Utah State University GEM Mini-Workshop San Francisco December 2014.
Characteristics of VLF Tweeks Nedra Tounsi & Hassen Ghalila Laboratoire de Spectroscopie Atomique Moléculaire et Applications 1 In this spectrogram recorded.
Transmission Media / Channels. Introduction Provides the connection between the transmitter and receiver. 1.Pair of wires – carry electric signal. 2.Optical.
V. M. Sorokin, V.M. Chmyrev, A. K. Yaschenko and M. Hayakawa Strong DC electric field formation in the ionosphere over typhoon and earthquake regions V.
Low-latitude Ionospheric Sensor Network (LISN) C. E. Valladares, Boston College V. Eccles, Space Environment Corporation E. Kudeki, University of Illinois.
Yuji Otake, Akito Araya and Kazuo Hidano
Antarctic Peninsula is a very suitable area for experimental investigations of troposphere-to-ionosphere energy transfer because this place characterized.
The UV range The UV range starts below 400 nm, i.e. deep violet. Usually UV radiation is divided into three main ranges. UV-A ( nm), UV-B (
1 Agenda Topic: Space Weather Modeling and the Whole Atmosphere Model (WAM) Presented By: Rodney Viereck(NWS/NCEP/SWPC) Contributors: Rashid Akmaev (SWPC)
Quasi-stationary planetary wave long-term changes in total ozone over Antarctica and Arctic A.Grytsai, O.Evtushevsky, O. Agapitov, A.Klekociuk, V.Lozitsky,
The Relations Between Solar Wind Variations and the North Atlantic Oscillation Rasheed Al-Nuaimi and Kais Al-Jumily Department of Atmospheric Sciences.
Electromagnetic and plasma disturbances caused by impact to the ionosphere Valery M. Sorokin Pushkov Institute of Terrestrial Magnetism, Ionosphere and.
29 August, 2011 Beijing, China Space science missions related to ILWS in China
1 Mars Micro-satellite Mission Japanese micro-satellite mission to Mars to study the plasma environment and the solar wind interaction with a weakly-magnetized.
UPenn NROTC Unit, dtd Fall 2004 Naval Weapons Systems Energy Fundamentals.
Jupiter Thomas Myers.
Introduction to Space Weather Jie Zhang CSI 662 / PHYS 660 Spring, 2012 Copyright © Ionosphere II: Radio Waves April 19, 2012.
Observation of global electromagnetic resonances by low-orbiting satellites Surkov V. V. National Research Nuclear University MEPhI.
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,
THE REACTION OF MID-LATITUDE IONOSPHERE ON STRONG IONOSPHERIC STORMS ON THE BASE OF THE EAST- SIBERIAN GROUND-BASED RADIO INSTRUMENT NETWORK DATA B.G.
Question 1 1) wavelength 2) frequency 3) period 4) amplitude 5) energy
Whistler Waves and Related Magnetospheric Phenomena
Chapter 6 The Atmosphere Preview Section 1 Characteristics of the AtmosphereCharacteristics of the Atmosphere.
5.1 Electromagnetic Radiation. Wave motion The transfer of energy without matter is called wave motion Two Types.
Comparison of the electron density profiles measured with the Incoherent Scatter Radar, Digisonde DPS-4 and Chirp-Ionosonde Ratovsky K.G., Shpynev* B.G.,
Key RO Advances Observation –Lower tropospheric penetration (open loop / demodulation) –Larger number of profiles (rising & setting) –Detailed precision.
Part 3  Transmission Media & EM Propagations.  Provides the connection between the transmitter and receiver. 1.Pair of wires – carry electric signal.
Chapter 22 Section 2 Handout
Forecasted 700 hPa Low (Blizzard of 2006) The RUC was saying “watch out.” This model is becoming a great short range model for East coast snowstorms (courtesy.
What is a geomagnetic storm? A very efficient exchange of energy from the solar wind into the space environment surrounding Earth; These storms result.
Layers of the Atmosphere How well can you understand your foldable?
Eeng360 1 Chapter 1 INTRODUCTION  Propagation of Electromagnetic Waves  Information Measure  Channel Capacity and Ideal Communication Systems Huseyin.
Radio Wave Propagation
By Saneeju m salu. Radio waves are one form of electromagnetic radiation RADIO WAVES.
These plots illustrate different dominant directions from Rothera and Halley. The vectors show individual wave velocities while the shaded yellow area.
Dynasonde measurements advance understanding of the thermosphere- ionosphere dynamics Nikolay Zabotin 1 with contributions from Oleg Godin 2, Catalin Negrea.
When Lower Atmosphere Waves Invade the Upper Atmosphere
CHARACTERISTICS OF TURBULENT PROCESS IN THE SOLAR PHOTOSPHERE
CEDAR Frontiers: Daytime Optical Aeronomy Duggirala Pallamraju and Supriya Chakrabarti Center for Space Physics, Boston University &
The Atmosphere.
Atmosphere-Ionosphere Wave Coupling as Revealed in Swarm Plasma Densities and Drifts Jeffrey M. Forbes Department of Aerospace Engineering Sciences, University.
Utilizing Scientific Advances in Operational Systems
ICESTAR: Solar-terrestrial and aeronomy research during the International Polar Year Kirsti Kauristie1, Allan Weatherwax2, Richard Harrison3, Richard.
The ionosphere is much more structured and variable than ever predicted. Solar Driven Model Since 2000, we have seen more, very clear evidence that the.
Lecture 4: Wave Propagation Concept
The UV range The UV range starts below 400 nm, i.e. deep violet. Usually UV radiation is divided into three main ranges. UV-A ( nm), UV-B (
Université Joseph Fourier Grenoble, France
Earth’s Ionosphere Lecture 13
788.11J Presentation “Atmospheric Observatory”
Exploring the ionosphere of Mars
REPEAT STATIONS MEASUREMENTS IN UKRAINE IN 2006
The Layered Atmosphere:
Propagation Effects on Communication Links
Ken Creager, Wendy McClausland and Steve Malone
Presentation transcript:

Troposphere-Ionosphere-Magnetosphere Coupling Study TIMIS EoI 803 (as part of ICESTAR/IHY) Yuri Yampolski (2), Valery Korepanov (1), Gennadi Milinevsky (3) (1) Lviv Center of Institute of Space Research, Ukraine (2) Institute of Radio Astronomy, Kharkiv, (3) National Taras Shevchenko University of Kyiv Research in the framework of SCAR ICESTAR Program

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

Magnetic field and pressure at Vernadsky Correlation Pressure-Magnetic Variations Response of magnetic variations to weather front

The main idea for TIMIS is the study powerful weather front “projection” to geospace heights. The West Antarctic Peninsula is one of the most active cyclonic regions of the Earth. The results, based on Vernadsky station data, show that the weather front is accompanied by excitement in troposphere the mid-scale atmospheric gravity waves (AGW). Hugo Island Palmer Vernadsky Rothera Arctowsky Palmer-Vernadsky 53 km Hugo Is.-Vernadsky 70 km Palmer- Hugo Is. 63 km Arctowsky-Vernadsky 440 km Rothera-Vernadsky 300 km Short base: Long base:

The AGW propagate to dynamo-area heights and modifies the transverse ionosphere conductivities and current systems that produce the magnetic field variations above the front passing and in conjugate region. Study this processes in the Antarctic Peninsula region will allow, first, reconstruct spatial structure of the weather front, secondly, restore spatial spectrum agitated AGW and, finally, restore the stimulated magnetic field variations. The project is based on the idea of the energy transport from the Earth surface to the upper ionosphere study using a network of the low power unmanned GPS-synchronized autonomous meteo-magnetic stations (AMMS).

The AMMS with total power consumption W have developed for this experiment in Ukraine. A network of observation sites spaced by km will be established in the West Antarctic Peninsula and near-shore islands. In addition to main goals of TIMIS the space distributed AMMS network will allow to investigate the large-scale long-period planetary wave in troposphere and their impact to upper atmosphere.

The Antarctic Peninsula AMMS network of high precision magnetometers will allow the study geomagnetic micropulsations, especially supported by geomagnetic variation measurements in the conjugate region. Other goal, which will be simultaneously achieved, is magnetovariational sounding with the AMMS network. This will allow the study of deep geoelectric structure of the region which very interesting from geological point of view.

Theoretical modeling of AGW – MHD modulation Cyclone in troposphere E-layer ionosphere

Idea: 1.The severe weather fronts are “projected” on ionosphere ~120 km height 2.The delay of magnetic field response minutes (corresponded vertical velocity m/s) Possible carrier? Atmosphere gravity waves AGW Distribution of sensitive magnetometers with pressure sensors along Antarctic Peninsula will give spatial and temporal coverage weather front movement and response in E-layer of ionosphere (and possible response in conjugate region?)

1. Three components magnetometer Magnetic field measurement range ±55000 nT Noise density at 1Hz less than 15 pT/√Hz Frequency band (DC-0.2) Hz 2. Atmospheric pressure sensor Mpa 3. Temperature sensor Temperature measurement range (- 40…+ 40) o C Temperature measurement error 0,1 o C 6. Flash memory capacity 6 month registration (one year in future) 7. Power consumption W AUTONOMOUS “METEO”MAGNETIC STATION (AMMS)

ANTARCTIC AUTONOMOUS METEOMAGNETIC STATION The four AMMS already constructed and tested for network ( km distance) installation in several points of Antarctic Peninsula PRECISION PRESSURE SENSOR

AMMS testing in 2005 in Antarctic Peninsula Berthelot Is Petermann Is Time for installation 2-5 hours

Hugo Island (US autonomous meteo-station) Vernadsky 70 km 53 km 63 km Possible sites for “small” network Palmer (Port Lockroy ?) Main need – logistic support

Current state-of- art (February 2007) 1.AMMS has been constructed 2.Till October 2007 two AMMS will be supplied by solar panels for 6 month (at least) continuous work 3.We have some financial support from National Antarctic Scientific Center 4.Main problem – logistics support to install AMMS with solar panels at Hugo Island (60 km from Palmer) 5.Planned (desirable) start for measurements - November We have pre-agree with Arctowsky and Rothera Research in the framework of SCAR ICESTAR Program