Recent Advances in Atmospheric, Solar-Terrestrial Physics and Space
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Sun-Earth System Interaction Studies Over Vietnam: an International Cooperative Project
Ann. Geophys., 24, 3313–3327, 2006 www.ann-geophys.net/24/3313/2006/ Annales © European Geosciences Union 2006 Geophysicae Sun-Earth System Interaction studies over Vietnam: an international cooperative project C. Amory-Mazaudier1, M. Le Huy2, Y. Cohen3, V. Doumbia4,*, A. Bourdillon5, R. Fleury6, B. Fontaine7, C. Ha Duyen2, A. Kobea4, P. Laroche8, P. Lassudrie-Duchesne6, H. Le Viet2, T. Le Truong2, H. Luu Viet2, M. Menvielle1, T. Nguyen Chien2, A. Nguyen Xuan2, F. Ouattara9, M. Petitdidier1, H. Pham Thi Thu2, T. Pham Xuan2, N. Philippon**, L. Tran Thi2, H. Vu Thien10, and P. Vila1 1CETP/CNRS, 4 Avenue de Neptune, 94107 Saint-Maur-des-Fosses,´ France 2Institute of Geophysics, Vietnamese Academy of Science and Technology , 18 Hoang Quoc Viet, Cau Giay, Hano¨ı, Vietnam 3IPGP, 4 Avenue de Neptune, 94107 Saint-Maur-des-Fosses,´ France 4Laboratoire de Physique de l’Atmosphere,` Universite´ d’Abidjan Cocody 22 B.P. 582, Abidjan 22, Coteˆ d’Ivoire 5Institut d’Electronique et de Tel´ ecommunications,´ Universite´ de Rennes Batˆ 11D, Campus Beaulieu, 35042 Rennes, cedex,´ France 6ENST, Universite´ de Bretagne Occidentale, CS 83818, 29288 Brest, cedex´ 3, France 7CRC , Faculte´ des Sciences, 6 Boulevard Gabriel, F 21004 Dijon cedex´ 04, France 8Unite´ de Recherche Environnement Atmospherique,´ ONERA, 92332 Chatillon, cedex,´ France 9University of Koudougou, Burkina Faso 10Laboratoire signaux et systemes,` CNAM, 292 Rue saint Martin, 75141 Paris cedex´ 03, France *V. Doumbia previously signed V. Doumouya **affiliation unknown Received: 15 June 2006 – Revised: 19 October 2006 – Accepted: 8 November 2006 – Published: 21 December 2006 Abstract. During many past decades, scientists from var- the E, F1 and F2 ionospheric layers follow the variation of ious countries have studied separately the atmospheric mo- the sunspot cycle. -
Study of the Geoeffectiveness of Coronal Mass Ejections
Study of the geoeffectiveness of coronal mass ejections Katarzyna Bronarska Jagiellonian University Faculty of Physics, Astronomy and Applied Computer Science Astronomical Observatory PhD thesis written under the supervision of dr hab. Grzegorz Michaªek September 2018 Acknowledgements Pragn¦ wyrazi¢ gª¦bok¡ wdzi¦czno±¢ moim rodzicom oraz m¦»owi, bez których »aden z moich sukcesów nie byªby mo»liwy. Chc¦ równie» podzi¦kowa¢ mojemu promotorowi, doktorowi hab. Grzogorzowi Michaªkowi, za ci¡gªe wsparcie i nieocenion¡ pomoc. I would like to express my deepest gratitude to my parents and my husband, without whom none of my successes would be possible. I would like to thank my superior, dr hab. Grzegorz Michaªek for continuous support and invaluable help. Abstract This dissertation is an attempt to investigate geoeectiveness of CMEs. The study was focused on two important aspects regarding the prediction of space weather. Firstly, it was presented relationship between energetic phenomena on the Sun and CMEs producing solar energetic particles. Scientic considerations demonstrated that very narrow CMEs can generate low energy particles (energies below 1 MeV) in the Earth's vicinity without other activity on the Sun. It was also shown that SEP events associated with active regions from eastern longitudes have to be complex to produce SEP events at Earth. On the other hand, SEP particles originating from mid-longitudes (30<latitude<70) on the west side of solar disk can be also associated with the least complex active regions. Secondly, two phenomena aecting CMEs detection in coronagraphs have been dened. During the study the detection eciency of LASCO coronagraphs was evaluated. It was shown that the detection eciency of the LASCO coronagraphs with typical data availability is sucient to record all potentially geoeective CMEs. -
Continuous Magnetic Reconnection at the Earth's Magnetopause
Why Study Magnetic Reconnection? Fundamental Process • Sun: Solar flares, Flare loops, CMEs • Interplanetary Space • Planetary Magnetosphere: solar wind plasma entry, causes Aurora Ultimate goal of the project – observe magnetic reconnection by satellite in situ through predictions of reconnection site in model Regions of the Geosphere • Solar wind: made up of plasma particles (pressure causes field distortion) • Bow shock: shock wave preceding Earth’s magnetic field • Magnetosheath: region of shocked plasma (higher density) • Magnetopause: Boundary between solar wind/geosphere • Cusp region: region with open field lines and direct solar wind access to upper atmosphere Magnetic Reconnection • Two antiparallel magnetized plasmas, separated by current sheet • Occurs in a very small area (Diffusion Region) At the Earth’s Magnetopause: • IMF reconnects with Earth’s magnetic field across the magnetopause • Southward IMF reconnects near equator • Forms open field lines, which convect backwards to cusp Instrument Overview Polar –TIMAS Wind - SWE instrument • Outside • Measures 3D velocity geospheric distributions influence • Focused on H+ data • Provides solar wind data Magnetic Reconnection Observed in the Cusp Magnetopause Fast Particle Magnetospheric Slow Particle • Color spectrogram Cusp • Measures energy and intensity (flux) of protons from solar wind Solar Wind in cusp with respect to time and latitude • Latitude changes due to convection Color spectrogram produced by IDL program written by mentor Methodology to Determine Where Reconnection -
Extraformational Sediment Recycling on Mars Kenneth S
Research Paper GEOSPHERE Extraformational sediment recycling on Mars Kenneth S. Edgett1, Steven G. Banham2, Kristen A. Bennett3, Lauren A. Edgar3, Christopher S. Edwards4, Alberto G. Fairén5,6, Christopher M. Fedo7, Deirdra M. Fey1, James B. Garvin8, John P. Grotzinger9, Sanjeev Gupta2, Marie J. Henderson10, Christopher H. House11, Nicolas Mangold12, GEOSPHERE, v. 16, no. 6 Scott M. McLennan13, Horton E. Newsom14, Scott K. Rowland15, Kirsten L. Siebach16, Lucy Thompson17, Scott J. VanBommel18, Roger C. Wiens19, 20 20 https://doi.org/10.1130/GES02244.1 Rebecca M.E. Williams , and R. Aileen Yingst 1Malin Space Science Systems, P.O. Box 910148, San Diego, California 92191-0148, USA 2Department of Earth Science and Engineering, Imperial College London, South Kensington, London SW7 2AZ, UK 19 figures; 1 set of supplemental files 3U.S. Geological Survey, Astrogeology Science Center, 2255 N. Gemini Drive, Flagstaff, Arizona 86001, USA 4Department of Astronomy and Planetary Science, Northern Arizona University, P.O. Box 6010, Flagstaff, Arizona 86011, USA CORRESPONDENCE: [email protected] 5Department of Planetology and Habitability, Centro de Astrobiología (CSIC-INTA), M-108, km 4, 28850 Madrid, Spain 6Department of Astronomy, Cornell University, Ithaca, New York 14853, USA 7 CITATION: Edgett, K.S., Banham, S.G., Bennett, K.A., Department of Earth and Planetary Sciences, The University of Tennessee, 1621 Cumberland Avenue, 602 Strong Hall, Knoxville, Tennessee 37996-1410, USA 8 Edgar, L.A., Edwards, C.S., Fairén, A.G., Fedo, C.M., National Aeronautics -
Directed Reading Packet
Directed Reading Packet Geosphere Unit Name:_______________________________ Teacher: _________________ Period: ____ Section 1.2: A View of Earth This section explains the physical structure of Earth. Reading Strategy Predicting Before you read, predict the meaning of the vocabulary terms. After you read, revise your definition if your prediction was incorrect. For more information on this Reading Strategy, see the Reading and Study Skills in the Skills and Reference Handbook at the end of your textbook. Vocabulary Term Before You Read After You Read hydrosphere a. b. atmosphere c. d. geosphere e. f. biosphere g. h. core i. j. mantle k. l. crust m. n. Earth’s Major Spheres 1. Earth can be thought of as consisting of four major spheres: the , , , and . Match each term to its description. Term Description 2. hydrosphere a. all life-forms on Earth 3. atmosphere b. composed of the core, mantle, and crust 4. geosphere c. dense, heavy inner sphere of Earth 5. biosphere d. thin outside layer of Earth’s surface 6. core e. the water portion of Earth 7. mantle f. the gaseous envelope around Earth 8. crust g. located between the crust and core of Earth 9. What does each letter in the diagram below represent? A. B. C. D. E. F. G. H. I. J. Plate Tectonics 10. Is the following sentence true or false? Forces such as weathering and erosion that work to wear away high points and flatten out Earth’s surface are called constructive forces. 11. Circle the letter of each type of constructive force. a. gravity b. -
Session B-1: Model Building in Planetary Science and the NGSS
Model Building in Planetary Science and the NGSS Dr. Eric Hawker IMSA Science Faculty March 4th , 2016 Planetary Science • Planets are complicated dynamic systems. • There are many planetary attributes that interact with each other. • The dynamic changes that planets go through are driven by energy. Model Building • Usually these are not physical models! • A set of concepts that describe a system. • NGSS Science and Engineering Practices: Developing and Using Models: Modeling in 9–12 builds on K–8 experiences and progresses to using, synthesizing, and developing models to predict and show relationships among variables between systems and their components in the natural and designed world(s). • Develop a model based on evidence to illustrate the relationships between systems or between components of a system. (HS-ESS2-1), (HS-ESS2-3),(HS-ESS2-6) • Use a model to provide mechanistic accounts of phenomena. (HS- ESS2-4) Model Building • HS-ESS2-1. Develop a model to illustrate how Earth’s internal and surface processes operate at different spatial and temporal scales to form continental and ocean-floor features. • HS-ESS2-3. Develop a model based on evidence of Earth’s interior to describe the cycling of matter by thermal convection. • HS-ESS2-6. Develop a quantitative model to describe the cycling of carbon among the hydrosphere, atmosphere, geosphere, and biosphere. Heat from Planetary Formation • The initial solar nebula of dust and gas that the Solar System formed from had a lot of gravitational potential energy. • This gravitational potential energy was turned into thermal energy (heat) during planetary formation. Atacama Large Millimeter Array image of HL Tauri Radioactivity • When the planets formed, radioactive isotopes such as uranium, thorium, and potassium were trapped deep underground. -
Geosphere Process Report for the Safety Assessment SR-Site Assessment Safety the for Report Process Geosphere Technical Report TR-10-48
Geosphere process report for the safety assessment SR-Site Technical Report TR-10-48 Geosphere process report for the safety assessment SR-Site Svensk Kärnbränslehantering AB November 2010 Svensk Kärnbränslehantering AB Swedish Nuclear Fuel and Waste Management Co Box 250, SE-101 24 Stockholm Phone +46 8 459 84 00 TR-10-48 CM Gruppen AB, Bromma, 2010 CM Gruppen ISSN 1404-0344 SKB TR-10-48 Geosphere process report for the safety assessment SR-Site Svensk Kärnbränslehantering AB November 2010 A pdf version of this document can be downloaded from www.skb.se 2011-10. Preface This document compiles information on processes in the geosphere relevant for long-term safety of a KBS-3 repository. It supports the safety assessment SR-Site, which will support the licence application for a final repository in Sweden. The work of compiling this report has been led by Kristina Skagius, Kemakta Konsult AB. She has also been the main editor of the report. The following persons have had the main responsibilities for specific subject areas: Harald Hökmark, Clay Technology AB (thermal and mechanical processes), Jan-Olof Selroos, SKB (hydrogeological and transport processes), and Ignasi Puigdomenech and Birgitta Kalinowski, SKB (geochemical processes). In addition, a number of experts have contributed to specific parts of the report as listed in Section 1.3. The report has been reviewed by Jordi Bruno, Amphos, Spain; John Cosgrove, Imperial College, UK; Thomas Doe, Golder Associates Inc, USA; Alan Hooper, Alan Hooper Consulting Limited, UK; John Hudson, Rock Engineering Consultants, UK; Ivars Neretnieks, Royal Institute of Technology, Sweden; Mike Thorne, Mike Thorne and Associates Ltd, UK; and Per-Eric Ahlström, SKB. -
Theory, Modeling, and Integrated Studies in the Arase (ERG) Project
Seki et al. Earth, Planets and Space (2018) 70:17 https://doi.org/10.1186/s40623-018-0785-9 FULL PAPER Open Access Theory, modeling, and integrated studies in the Arase (ERG) project Kanako Seki1* , Yoshizumi Miyoshi2, Yusuke Ebihara3, Yuto Katoh4, Takanobu Amano1, Shinji Saito5, Masafumi Shoji2, Aoi Nakamizo6, Kunihiro Keika1, Tomoaki Hori2, Shin’ya Nakano7, Shigeto Watanabe8, Kei Kamiya5, Naoko Takahashi1, Yoshiharu Omura3, Masahito Nose9, Mei‑Ching Fok10, Takashi Tanaka11, Akimasa Ieda2 and Akimasa Yoshikawa11 Abstract Understanding of underlying mechanisms of drastic variations of the near-Earth space (geospace) is one of the current focuses of the magnetospheric physics. The science target of the geospace research project Exploration of energiza‑ tion and Radiation in Geospace (ERG) is to understand the geospace variations with a focus on the relativistic electron acceleration and loss processes. In order to achieve the goal, the ERG project consists of the three parts: the Arase (ERG) satellite, ground-based observations, and theory/modeling/integrated studies. The role of theory/modeling/integrated studies part is to promote relevant theoretical and simulation studies as well as integrated data analysis to combine diferent kinds of observations and modeling. Here we provide technical reports on simulation and empirical models related to the ERG project together with their roles in the integrated studies of dynamic geospace variations. The simu‑ lation and empirical models covered include the radial difusion model of the radiation belt electrons, GEMSIS-RB and RBW models, CIMI model with global MHD simulation REPPU, GEMSIS-RC model, plasmasphere thermosphere model, self-consistent wave–particle interaction simulations (electron hybrid code and ion hybrid code), the ionospheric electric potential (GEMSIS-POT) model, and SuperDARN electric feld models with data assimilation. -
Development of a Local Empirical Model of Ionospheric Total Electron
www.nature.com/scientificreports OPEN Development of a local empirical model of ionospheric total electron content (TEC) and its application for studying solar‑ionospheric efects Pantea Davoudifar1,2*, Keihanak Rowshan Tabari1, Amir Abbas Eslami Shafgh1, Ali Ajabshirizadeh3, Zahra Bagheri4, Fakhredin Akbarian Tork Abad2 & Milad Shayan1 Regular and irregular variations in total electron content(TEC) are one of the most signifcant observables in ionosphericstudies. During the solar cycle 24, the variability of ionosphere isstudied using global positioning system derived TEC at amid‑latitude station, Tehran (35.70N, 51.33E). Based on solar radiofux and seasonal and local time‑dependent features of TEC values, asemi‑ empirical model is developed to represent its monthly/hourlymean values. Observed values of TEC and the results of oursemi‑empirical model then are compared with estimated values of astandard plasmasphere–ionosphere model. The outcome of this modelis an expected mean TEC value considering the monthly/hourly regularefects of solar origin. Thus, it is possible to use it formonitoring irregular efects induced by solar events. As a result,the connection of TEC variations with solar activities are studiedfor the case of coronal mass ejections accompanying extremesolar fares. TEC response to solar fares of class X is wellreproduced by this model. Our resulting values show that the mostpowerful fares (i.e. class X) induce a variation of more than 20percent in daily TEC extent. In the Earth’s ionosphere, the variability of space weather is easily refected in TEC. As the total number of electrons is measured along a vertical column of one square meter cross-section (1 TEC Unit (TECU) = 1 × 1016 electrons m−2 ) from the height of a GPS satellite (∼ 20, 000 km ) to the receiver, thus TEC char- acterizes variations in both ionosphere and plasmasphere 1. -
Space Weather Effects Studies in Azerbaijan: Potential Impacts on Geosphere, Biosphere and Periodic Comets
SENS 2007 Third Scientific Conference with International Participation SPACE, ECOLOGY, NANOTECHNOLOGY, SAFETY 27–29 June 2007, Varna, Bulgaria SPACE WEATHER EFFECTS STUDIES IN AZERBAIJAN: POTENTIAL IMPACTS ON GEOSPHERE, BIOSPHERE AND PERIODIC COMETS Elchin Babayev, Arif Hashimov, Ayyub Guliyev, Famil Mustafa, Peter Shustarev, Abbas Asgarov Azerbaijan National Academy of Sciences 10, Istiglaliyyat Street, Baku, AZ-1001, the Republic of Azerbaijan е-mail: [email protected] Key words: space weather, power failures, sudden cardiac death, traffic accidents, periodic comets Abstract. For getting more and better knowledge about the physical links between major space weather sources (solar, geomagnetic and cosmic ray activities) and short- and long-term effects on technical-engineering systems and biosphere, particularly, human life and health state in middle latitudes, we are conducting complex (theoretical, experimental and statistical) space weather studies in the Azerbaijan National Academy of Sciences. Part of main and recently obtained results of these collaborative investigations of potential space weather effects on functioning of power supply systems, sudden cardiac death mortality as well as an influence of changes of heliogeophysical conditions on dynamics of traffic accidents is briefly provided in this review paper. An influence of solar activity on changes of brightness curves of periodic comets 29P/Schwassmann-Wachmann and 1P/Halley is investigated on the basis of data with about 1300 and 5900 estimations of brightness and using improved by authors calculations for visual magnitude of comets. 1. Introduction According to the US National Space Weather Programme (1995), space weather refers to the “conditions on the Sun and in the solar wind, magnetosphere, ionosphere, and thermosphere that can influence the performance and reliability of space-borne and ground-based technological systems and can endanger human life or health”. -
Changing Climate a Guide for Teaching Climate Change in Grades 3 to 8 the Climate System 1 and Greenhouse Effect by Lindsey Mohan and Jenny D
ENVIRONMENTAL LITERACY TEACHER GUIDE SERIES Changing Climate A Guide for Teaching Climate Change in Grades 3 to 8 The Climate System 1 and Greenhouse Effect by Lindsey Mohan and Jenny D Ingber “Climate is what you increased risk of drought, wildfires, and of this natural phenomenon is now expect, weather is plant and animal extinctions. causing a range of changes throughout In order to make well-informed Earth’s system. what you get.” decisions that will enable humans and In this chapter we consider the Robert A. Heinlein other organisms to continue to thrive on differences between climate and Earth into the future, today’s students weather, look at the climate system in arth’s global climate is changing, need to have at least a basic scientific more detail, discuss what it means for bringing numerous changes to the understanding of our planet’s climate climate to change, and take a closer E planet and the organisms that live system and the role that humans are look at the Greenhouse Effect and what on it. Validated records from instruments playing in changing it. students know about this important around the world show that our global The climate system encompasses a phenomenon. temperature increased by around one complex set of processes that affect degree Celsius (almost two degrees conditions around the world. One of Our Experience Fahrenheit) during the second half of the most important features of the of Climate the 20th century. Consequences of this climate system—the Greenhouse Weather and climate are a part of observed warming include substantial Effect—is necessary for life on Earth. -
Locations of Chorus Emissions Observed by the Polar Plasma Wave Instrument K
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 115, A00F12, doi:10.1029/2009JA014579, 2010 Click Here for Full Article Locations of chorus emissions observed by the Polar Plasma Wave Instrument K. Sigsbee,1 J. D. Menietti,1 O. Santolík,2,3 and J. S. Pickett1 Received 18 June 2009; revised 20 November 2009; accepted 17 December 2009; published 8 June 2010. [1] We performed a statistical study of the locations of chorus emissions observed by the Polar spacecraft’s Plasma Wave Instrument (PWI) from March 1996 to September 1997, near the minimum of solar cycles 22/23. We examined how the occurrence of chorus emissions in the Polar PWI data set depends upon magnetic local time, magnetic latitude, L shell, and L*. The Polar PWI observed chorus most often over a range of magnetic local times extending from about 2100 MLT around to the dawn flank and into the dayside magnetosphere near 1500 MLT. Chorus was least likely to be observed near the dusk flank. On the dayside, near noon, the region in which Polar observed chorus extended to larger radial distances and higher latitudes than at other local times. Away from noon, the regions in which chorus occurred were more restricted in both radial and latitudinal extent. We found that for high‐latitude chorus near local noon, L* provides a more reasonable mapping to the equatorial plane than the standard L shell. Chorus was observed slightly more often when the magnitude of the solar wind magnetic field BSW was greater than 5 nT than it was for smaller interplanetary magnetic field strengths.