Discuss 7 deficiencies/impediments in our understanding. 1
|
|
|
- Brianna Ross
- 10 years ago
- Views:
Transcription
1 Do We Really Understand Solar-Wind/Magnetosphere Coupling? Joe Borovsky Space Science Institute --- University of Michigan!We have major unsolved issues about A. what controls dayside reconnection B. the magnitude of and physics of the viscous interaction.!we have lack of understanding of post-reconnection coupling physics.!we have a problem using data correlations to confirm physical principles. Discuss 7 deficiencies/impediments in our understanding. 1
2 1 What Controls the Dayside Reconnection Rate: E sw or 0.1v A B? (1) Since the reconnection rate v in B has the dimension of an electric field, it has been argued that E recon = E sw = v sw B z. The solar-wind electric field evolved to v swx B y sin z (θ clock /2). (2) The Petschek 0.1v A B yields derivations R(n sw,v sw,m A,θ clock ) R quick = n sw 1/2 v sw 2 M A /[ M A ] 1/4 sin 2 (θ/2) Both (1) and (2) do well in correlations with geomagnetic activity. Is one correct? Is one wrong? 2
3 2a Correlation Game: How well can solar-wind variables describe the variance of geomagnetic indices? Correlations: Physics Versus Math Physics improvement of correlation coefficient: Choose solar-wind variables that more accurately describe the coupling mechanism of the solar wind to the magnetosphere. Mathematical improvement of correlation coefficient: Choose solar-wind variables that better describe the variance of the solar wind, with a better chance of describing magnetospheric variance. When the variables are noisy, how can you tell better physics from better math? 3
4 2b Correlations: Cause and Effect In the solar wind, all variables are correlated or anti-correlated. And all variables are noisy (imperfect). (1) A solar-wind variable can be acting as a proxy for another solarwind variable. (2) A solar-wind variable may be acting to suppress the noise on another solar-wind variable. (3) A solar-wind variable may be acting to supply information about the type of solar-wind plasma. Sorting out cause and effect in correlations is... difficult. 4
5 3 What Is the Nature of the Viscous Interaction? (1) What is the magnitude of the viscous interaction? (viscous interaction versus reconnection behind the cusps) (2) What physical mechanisms are acting? Kelvin-Helmholtz rollups? Plasma-wave diffusion? Other? (3) What variables in the solar-wind control the viscous interaction? 5
6 4 What Is the Physics of the Turbulence Effect? AE, AU, -AL, Kp, -Dst, and PCI are positively correlated with δb/b of the upstream solar wind. These correlations hold when the reconnection driver functions are binned. These correlations hold when the fluctuations are purely northward. Is there a physical mechanism that couples solarwind turbulence to the magnetosphere? What type of solar-wind fluctuations are important? 6
7 5 The Feedback of Magnetospheric Mass Density on the Dayside Reconnection Rate Magnetospheric plasma can mass-load dayside reconnection: predicted, simulated, and confirmed by spacecraft measurements. Criterion from the Cassak-Shay equation: ρ mag ρ sh B mag /B s. Storm levels of driving bring a magnetospheric response via: 1 plasmaspheric drainage plume 2 oxygen-rich ion plasma sheet 3 warm plasma cloak. 1) We don t have surveys of the mass density ρ of the ion plasma sheet in the dayside magnetosphere. 2) We don t know the properties of the warm plasma cloak or its global evolution pattern. We can t quantify the amount of mass loading of dayside reconnection by the magnetosphere. 7
8 6 What is the Physics of Mass Coupling between the Solar Wind and the Magnetosphere? 1) We don t know the physical mechanisms that transport plasma from the magnetosheath into the magnetosphere. 2) We don t know how the plasma is processed upon entry. 3) Are there multiple pathways for plasma entry: LLBL versus mantle? 4) Can we quantitatively predict the mass transport. 8
9 7 The Physics of Post-Reconnection Coupling of the Solar Wind to the Magnetosphere-Ionosphere System After dayside reconnection, magnetospheric magnetic field lines connect directly into the moving magnetosheath plasma. 1) How important is the solar-wind driving of antisunward convection in the polar-cap ionosphere? 2) When do Region-I type currents close in the magnetosheath and bow shock? 3) How does polar-cap-potential saturation work? Several mechanisms, no consensus. 9
10 Summary Our physics understanding of solar-wind/ magnetosphere coupling is in very poor shape. (1) Control of dayside reconnection (2) Interpretation of correlations (3) The viscous interaction (4) The turbulence effect (5) Mass loading of dayside reconnection (6) Plasma entry (7) Post-reconnection coupling physics 10
11 Acknowledgements Over the years: Joachim Birn Mick Denton Richard Denton Herb Funsten Michael Hesse Masha Kuznetsova Benoit Lavraud Michelle Thomsen John Steinberg 11
Solar Wind Control of Density and Temperature in the Near-Earth Plasma Sheet: WIND-GEOTAIL Collaboration. Abstract
1 Geophys. Res. Letters, 24, 935-938, 1997. Solar Wind Control of Density and Temperature in the Near-Earth Plasma Sheet: WIND-GEOTAIL Collaboration T. Terasawa 1, M. Fujimoto 2, T. Mukai 3, I. Shinohara
The Solar Wind Interaction with the Earth s Magnetosphere: A Tutorial. C. T. Russell
The Solar Wind Interaction with the Earth s Magnetosphere: A Tutorial C. T. Russell Department of Earth and Space Sciences and Institute of Geophysics and Space Physics University of California Los Angeles
Kinetic effects in the turbulent solar wind: capturing ion physics with a Vlasov code
Kinetic effects in the turbulent solar wind: capturing ion physics with a Vlasov code Francesco Valentini [email protected] S. Servidio, D. Perrone, O. Pezzi, B. Maruca, F. Califano, W.
Keywords: Geomagnetic storms Dst index Space Weather Recovery phase.
MAGNETOSPHERE BEHAVIOUR DURING THE RECOVERY PHASE OF GEOMAGNETIC STORMS JESÚS AGUADO, CONSUELO CID, YOLANDA CERRATO, ELENA SAIZ Departamento de Física. Universidad de Alcalá, E-28871 Alcalá de Henares,
Space Weather: An Introduction C. L. Waters. Centre for Space Physics University of Newcastle, Australia
Space Weather: An Introduction C. L. Waters Centre for Space Physics University of Newcastle, Australia 1 Outline Space weather: Conditions on the Sun and in the solar wind, magnetosphere, ionosphere and
Coronal Heating Problem
Mani Chandra Arnab Dhabal Raziman T V PHY690C Course Project Indian Institute of Technology Kanpur Outline 1 2 3 Source of the energy Mechanism of energy dissipation Proposed mechanisms Regions of the
Unusual declining phase of solar cycle 23: Weak semi-annual variations of auroral hemispheric power and geomagnetic activity
Click Here for Full Article GEOPHYSICAL RESEARCH LETTERS, VOL. 36, L22102, doi:10.1029/2009gl040825, 2009 Unusual declining phase of solar cycle 23: Weak semi-annual variations of auroral hemispheric power
Temperature anisotropy in the solar wind
Introduction Observations Simulations Summary in the solar wind Petr Hellinger Institute of Atmospheric Physics & Astronomical Institute AS CR, Prague, Czech Republic Kinetic Instabilities, Plasma Turbulence
Magnetohydrodynamics. Basic MHD
Magnetohydrodynamics Conservative form of MHD equations Covection and diffusion Frozen-in field lines Magnetohydrostatic equilibrium Magnetic field-aligned currents Alfvén waves Quasi-neutral hybrid approach
A Beginner s Guide to Space Weather and GPS Professor Paul M. Kintner, Jr. with acknowledgements to
A Beginner s Guide to Space Weather and GPS Professor Paul M. Kintner, Jr. with acknowledgements to M. Psiaki, T. Humphreys, A. Cerruti, B. Ledvina, A. Mannucci, and E. R. de Paula I. Introduction This
EMİNE CEREN KALAFATOĞLU EYİGÜLER
EMİNE CEREN KALAFATOĞLU EYİGÜLER SPACE ENVIRONMENT UZB411E 2015-2016 FALL ROOM: 322 / THIRD FLOOR UPPER ATMOSPHERE AND SPACE WEATHER LAB OFFICE HOURS: EVERY TUESDAY AND WEDNESDAY BETWEEN 15-17 FOR OTHER
Space Weather Research and Forecasting in CRL, Japan
Space Weather Research and Forecasting in CRL, Japan Maki Akioka Hiraiso Solar Observatory Communications Research Laboratory Contact [email protected] 1 Contents of Presentation 1.Space Weather Observation
Kolmogorov versus Iroshnikov-Kraichnan spectra: Consequences for ion heating in
Kolmogorov versus Iroshnikov-Kraichnan spectra: Consequences for ion heating in the solar wind C. S. Ng 1, A. Bhattacharjee 2, D. Munsi 2, P. A. Isenberg 2, and C. W. Smith 2 1 Geophysical Institute, University
Department of Aeronautics and Astronautics School of Engineering Massachusetts Institute of Technology. Graduate Program (S.M., Ph.D., Sc.D.
Department of Aeronautics and Astronautics School of Engineering Massachusetts Institute of Technology Graduate Program (S.M., Ph.D., Sc.D.) Field: Space Propulsion Date: October 15, 2013 1. Introduction
Basic Equations, Boundary Conditions and Dimensionless Parameters
Chapter 2 Basic Equations, Boundary Conditions and Dimensionless Parameters In the foregoing chapter, many basic concepts related to the present investigation and the associated literature survey were
Wave-particle and wave-wave interactions in the Solar Wind: simulations and observations
Wave-particle and wave-wave interactions in the Solar Wind: simulations and observations Lorenzo Matteini University of Florence, Italy In collaboration with Petr Hellinger, Simone Landi, and Marco Velli
The Next Generation Science Standards (NGSS) Correlation to. EarthComm, Second Edition. Project-Based Space and Earth System Science
The Next Generation Science Standards (NGSS) Achieve, Inc. on behalf of the twenty-six states and partners that collaborated on the NGSS Copyright 2013 Achieve, Inc. All rights reserved. Correlation to,
SPACE WEATHER INTERPRETING THE WIND. Petra Vanlommel & Luciano Rodriguez
SPACE WEATHER INTERPRETING THE WIND Petra Vanlommel & Luciano Rodriguez THE SUN LOSES ENERGY Radiation Mass Particles THE SUN LOSES ENERGY PHYSICAL REPHRASING Total Solar Irradiance Solar Wind Fast Particles
Diagnostics. Electric probes. Instituto de Plasmas e Fusão Nuclear Instituto Superior Técnico Lisbon, Portugal http://www.ipfn.ist.utl.
C. Silva Lisboa, Jan. 2014 IST Diagnostics Electric probes Instituto de Plasmas e Fusão Nuclear Instituto Superior Técnico Lisbon, Portugal http://www.ipfn.ist.utl.pt Langmuir probes Simplest diagnostic
Towards an Enhanced Telluric Compensation Methodology
Towards an Enhanced Telluric Compensation Methodology Chijioke Ukiwe & Shamus M c Donnell Hunter M c Donnell Pipelines Services Inc. Presented at AUCSC 2011 by Gord Parker, C.E.T., CP2 Edmonton, Alberta,
Going up: Out of the atmosphere and into space
Belgian Institute for Space Aeronomy (BIRA-IASB) Institut d Aéronomie Spatiale de Belgique (IASB) Belgisch Instituut voor Ruimte-Aeronomie (BIRA) ELGISCH INSTITUUT VOOR RUIMTE-AERONOMIE INSTITUT D AERONOMIE
SIO 229 Gravity and Geomagnetism: Class Description and Goals
SIO 229 Gravity and Geomagnetism: Class Description and Goals This graduate class provides an introduction to gravity and geomagnetism at a level suitable for advanced non-specialists in geophysics. Topics
INTRODUCTION TO SOLAR WEATHER & HF PROPAGATION. Lewis Thompson W5IFQ September 27, 2011
INTRODUCTION TO SOLAR WEATHER & HF PROPAGATION Lewis Thompson W5IFQ September 27, 2011 PRESENTATION Ionospheric propagation NVIS Long-Range Frequency Selection (Critical Frequency & MUF) Propagation modeling
4-1-3 Space Weather Forecast Using Real-time Data
4-1-3 Space Weather Forecast Using Real-time Data In recent years, advances in telecommunications technology have made it possible to collect space-based and ground-based observation data needed for space
The solar wind (in 90 minutes) Mathew Owens
The solar wind (in 90 minutes) Mathew Owens 5 th Sept 2013 STFC Advanced Summer School [email protected] Overview There s simply too much to cover in 90 minutes Hope to touch on: Formation of the
Interaction of Energy and Matter Gravity Measurement: Using Doppler Shifts to Measure Mass Concentration TEACHER GUIDE
Interaction of Energy and Matter Gravity Measurement: Using Doppler Shifts to Measure Mass Concentration TEACHER GUIDE EMR and the Dawn Mission Electromagnetic radiation (EMR) will play a major role in
Solar Storms and Northern lights - how to predict Space Weather and the Aurora
Solar Storms and Northern lights - how to predict Space Weather and the Aurora Pål Brekke Norwegian Space Centre/UNIS Pål Brekke torsdag 12. mars 15 Fleet of satellites watching the Sun Stereo SDO SOHO
Intended Procurements in the Space Weather (SWE) Segment. SSA Industry Day 11 June 2013, ESOC
Intended Procurements in the Space Weather (SWE) Segment SSA Industry Day 11 June 2013, ESOC Juha-Pekka Luntama SSA Space Weather Segment Manager ESA Unclassified Releasable to the Public SSA/SWE Precursor
NUMERICAL ANALYSIS OF THE EFFECTS OF WIND ON BUILDING STRUCTURES
Vol. XX 2012 No. 4 28 34 J. ŠIMIČEK O. HUBOVÁ NUMERICAL ANALYSIS OF THE EFFECTS OF WIND ON BUILDING STRUCTURES Jozef ŠIMIČEK email: [email protected] Research field: Statics and Dynamics Fluids mechanics
Graduate Certificate Program in Energy Conversion & Transport Offered by the Department of Mechanical and Aerospace Engineering
Graduate Certificate Program in Energy Conversion & Transport Offered by the Department of Mechanical and Aerospace Engineering Intended Audience: Main Campus Students Distance (online students) Both Purpose:
The ratio of inertial to viscous forces is commonly used to scale fluid flow, and is called the Reynolds number, given as:
12.001 LAB 3C: STOKES FLOW DUE: WEDNESDAY, MARCH 9 Lab Overview and Background The viscosity of a fluid describes its resistance to deformation. Water has a very low viscosity; the force of gravity causes
Solar Activity and Earth's Climate
Rasmus E. Benestad Solar Activity and Earth's Climate Second Edition Published in association with Springer Praxis ids Publishing Publisl PRAXI Chichester, UK Contents Preface to the second edition Preface
Solar Wind: Theory. Parker s solar wind theory
Solar Wind: Theory The supersonic outflow of electrically charged particles, mainly electrons and protons from the solar CORONA, is called the SOLAR WIND. The solar wind was described theoretically by
Dimensional Analysis
Dimensional Analysis An Important Example from Fluid Mechanics: Viscous Shear Forces V d t / / / / / / / / / / / / / / / / / / / / / / / / / / / / / / / / / Ƭ = F/A = μ V/d More generally, the viscous
ME6130 An introduction to CFD 1-1
ME6130 An introduction to CFD 1-1 What is CFD? Computational fluid dynamics (CFD) is the science of predicting fluid flow, heat and mass transfer, chemical reactions, and related phenomena by solving numerically
Solar Wind Heating by MHD Turbulence
Solar Wind Heating by MHD Turbulence C. S. Ng, A. Bhattacharjee, and D. Munsi Space Science Center University of New Hampshire Acknowledgment: P. A. Isenberg Work partially supported by NSF, NASA CMSO
Measurement and Metrics Fundamentals. SE 350 Software Process & Product Quality
Measurement and Metrics Fundamentals Lecture Objectives Provide some basic concepts of metrics Quality attribute metrics and measurements Reliability, validity, error Correlation and causation Discuss
What is the purpose of this document? What is in the document? How do I send Feedback?
This document is designed to help North Carolina educators teach the Common Core (Standard Course of Study). NCDPI staff are continually updating and improving these tools to better serve teachers. Statistics
Coordinate generators
SPENVIS Upgrades Coordinate generators Merge orbit generator and grid generator: Simplification of model implementation Simplification of model presentation and navigation Orbit generator: Add NORAD Two
Fluid-Induced Material Transport: A Volume Averaged Approach to Modelling in SPH
Fluid-Induced Material Transport: A Volume Averaged Approach to Modelling in SPH Vinay Kumar SPH Workshop, 30.06. 01.07.2014, Karlsruhe www.baw.de Outline Motivation Model concept Groundwater model SPH
Grade 12 Consumer Mathematics Standards Test. Written Test Student Booklet
Grade 12 Consumer Mathematics Standards Test Written Test Student Booklet January 2011 Manitoba Education Cataloguing in Publication Data Grade 12 Consumer Mathematics Standards Test : Written Test Student
CROSS-CORRELATION BETWEEN STOCK PRICES IN FINANCIAL MARKETS. 1. Introduction
CROSS-CORRELATION BETWEEN STOCK PRICES IN FINANCIAL MARKETS R. N. MANTEGNA Istituto Nazionale per la Fisica della Materia, Unità di Palermo and Dipartimento di Energetica ed Applicazioni di Fisica, Università
Kinetic processes and wave-particle interactions in the solar wind
Kinetic processes and wave-particle interactions in the solar wind Eckart Marsch Institute for Experimental and Applied Physics (IEAP), Christian Albrechts University at Kiel, 24118 Kiel, Germany Seminar
Natural Convection. Buoyancy force
Natural Convection In natural convection, the fluid motion occurs by natural means such as buoyancy. Since the fluid velocity associated with natural convection is relatively low, the heat transfer coefficient
Lecture 14. Introduction to the Sun
Lecture 14 Introduction to the Sun ALMA discovers planets forming in a protoplanetary disc. Open Q: what physics do we learn about the Sun? 1. Energy - nuclear energy - magnetic energy 2. Radiation - continuum
Diffusion and Fluid Flow
Diffusion and Fluid Flow What determines the diffusion coefficient? What determines fluid flow? 1. Diffusion: Diffusion refers to the transport of substance against a concentration gradient. ΔS>0 Mass
The Theory of Magnetic Reconnection: Past, Present, and Future
The Theory of Magnetic Reconnection: Past, Present, and Future Paul Cassak University of Delaware & West Virginia University 2008 AGU Joint Assembly May 28, 2008 SOHO (ESA & NASA) Magnetic Reconnection
Correlation of GEO Communications Satellite Anomalies and Space Weather Phenomena: Improved Satellite Performance and Risk Mitigation
Correlation of GEO Communications Satellite Anomalies and Space Weather Phenomena: Improved Satellite Performance and Risk Mitigation Whitney Q. Lohmeyer 1 and Kerri Cahoy 2 MIT, Cambridge, MA, 02139 and
Coupling Forced Convection in Air Gaps with Heat and Moisture Transfer inside Constructions
Coupling Forced Convection in Air Gaps with Heat and Moisture Transfer inside Constructions M. Bianchi Janetti 1, F. Ochs 1 and R. Pfluger 1 1 University of Innsbruck, Unit for Energy Efficient Buildings,
EASA Safety Information Bulletin
EASA Safety Information Bulletin SIB No.: 2012-09 Issued: 23 May 2012 Subject: Effects of Space Weather on Aviation Ref. Publication: 1. EU OPS 1.390 Cosmic Radiation; 2. SIB 2012-10 Single Event Effects
SPACE WEATHER SUPPORT FOR COMMUNICATIONS. Overview
SPACE WEATHER SUPPORT FOR COMMUNICATIONS Overview Ionospheric variability (space weather) significantly impacts ground and space-based communications. In essence, the electrically charged particles of
Dynamic Process Modeling. Process Dynamics and Control
Dynamic Process Modeling Process Dynamics and Control 1 Description of process dynamics Classes of models What do we need for control? Modeling for control Mechanical Systems Modeling Electrical circuits
Space Weather Prediction Research and Services for China Manned Space Mission
Space Weather Prediction Research and Services for China Manned Space Mission Siqing Liu National Space Science Center, CAS Center for Space Science and Applied Research, CAS Outline I. General information
CSSAR Space Science Cooperation
CSSAR Space Science Cooperation WANG Shuzhi Center for Space Science and Applied Research Chinese Academy of Science(CSSAR) Table of Contents Brief History of CSSAR International Cooperation CAS Strategic
NOAA Space Weather Prediction Testbed and TESTMEX - NASA
NOAA Space Weather Prediction Testbed: Overview and Updates Rodney Viereck Director, Space Weather Prediction Testbed, NOAA Space Weather Prediction Center Outline: Overview The Transition Process Accomplishments
Open channel flow Basic principle
Open channel flow Basic principle INTRODUCTION Flow in rivers, irrigation canals, drainage ditches and aqueducts are some examples for open channel flow. These flows occur with a free surface and the pressure
ME 305 Fluid Mechanics I. Part 8 Viscous Flow in Pipes and Ducts
ME 305 Fluid Mechanics I Part 8 Viscous Flow in Pipes and Ducts These presentations are prepared by Dr. Cüneyt Sert Mechanical Engineering Department Middle East Technical University Ankara, Turkey [email protected]
Climate Models: Uncertainties due to Clouds. Joel Norris Assistant Professor of Climate and Atmospheric Sciences Scripps Institution of Oceanography
Climate Models: Uncertainties due to Clouds Joel Norris Assistant Professor of Climate and Atmospheric Sciences Scripps Institution of Oceanography Global mean radiative forcing of the climate system for
U.S. DEPARTMENT OF COMMERCE
Space Weather Space Weather Storms from the Sun Storms from the Sun U.S. DEPARTMENT OF COMMERCE National Oceanic and Atmospheric Administration National Weather Service U.S. Department of Commerce National
The Effect of Space Weather Phenomena on Precise GNSS Applications
FUGRO SATELLITE POSITIONING Doc. Ref.: A12321850TCBRC1 The Effect of Space Weather Phenomena on Precise GNSS Applications December 2014 PUBLIC Table of contents The Effect of Space Weather Phenomena on
Asymmetric Magnetic Reconnection in the Solar Atmosphere
Asymmetric Magnetic Reconnection in the Solar Atmosphere Nick Murphy Harvard-Smithsonian Center for Astrophysics March 13, 2015 Outline Basic physics of magnetic reconnection Magnetic reconnection in different
Space Weather: Forecasting & Impacts on Critical Infrastructure
Space Weather: Forecasting & Impacts on Critical Infrastructure Dr. Genene Fisher Senior Advisor for Space Weather National Weather Service AMS Washington Forum 12 April 2012 Outline Solar Activity Update
Supporting document to NORSOK Standard C-004, Edition 2, May 2013, Section 5.4 Hot air flow
1 of 9 Supporting document to NORSOK Standard C-004, Edition 2, May 2013, Section 5.4 Hot air flow A method utilizing Computational Fluid Dynamics (CFD) codes for determination of acceptable risk level
Analysis of Bayesian Dynamic Linear Models
Analysis of Bayesian Dynamic Linear Models Emily M. Casleton December 17, 2010 1 Introduction The main purpose of this project is to explore the Bayesian analysis of Dynamic Linear Models (DLMs). The main
Theory of moist convection in statistical equilibrium
Theory of moist convection in statistical equilibrium By analogy with Maxwell-Boltzmann statistics Bob Plant Department of Meteorology, University of Reading, UK With thanks to: George Craig, Brenda Cohen,
Loop Bandwidth and Clock Data Recovery (CDR) in Oscilloscope Measurements. Application Note 1304-6
Loop Bandwidth and Clock Data Recovery (CDR) in Oscilloscope Measurements Application Note 1304-6 Abstract Time domain measurements are only as accurate as the trigger signal used to acquire them. Often
Diagnostics. Electric probes. Instituto de Plasmas e Fusão Nuclear Instituto Superior Técnico Lisbon, Portugal http://www.ipfn.ist.utl.
Diagnostics Electric probes Instituto de Plasmas e Fusão Nuclear Instituto Superior Técnico Lisbon, Portugal http://www.ipfn.ist.utl.pt Langmuir probes Simplest diagnostic (1920) conductor immerse into
Problem Statement In order to satisfy production and storage requirements, small and medium-scale industrial
Problem Statement In order to satisfy production and storage requirements, small and medium-scale industrial facilities commonly occupy spaces with ceilings ranging between twenty and thirty feet in height.
Met Office Space Weather Operations and R&D
Met Office Space Weather Operations and R&D David Jackson Mark Gibbs, Suzy Bingham, Francois Bocquet, Edmund Henley, Sophie Murray WMO / ISES Meeting, August 9-10 2014, Moscow, Russia Met Office Motivation?
Predicting the Performance of a First Year Graduate Student
Predicting the Performance of a First Year Graduate Student Luís Francisco Aguiar Universidade do Minho - NIPE Abstract In this paper, I analyse, statistically, if GRE scores are a good predictor of the
Bulk properties of the slow and fast solar wind and interplanetary coronal mass ejections measured by Ulysses: Three polar orbits of observations
Click Here for Full Article JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 114,, doi:10.1029/2008ja013631, 2009 Bulk properties of the slow and fast solar wind and interplanetary coronal mass ejections measured
Brillig Systems Making Projects Successful
Metrics for Successful Automation Project Management Most automation engineers spend their days controlling manufacturing processes, but spend little or no time controlling their project schedule and budget.
CFD SIMULATION OF SDHW STORAGE TANK WITH AND WITHOUT HEATER
International Journal of Advancements in Research & Technology, Volume 1, Issue2, July-2012 1 CFD SIMULATION OF SDHW STORAGE TANK WITH AND WITHOUT HEATER ABSTRACT (1) Mr. Mainak Bhaumik M.E. (Thermal Engg.)
Space Weather Measurements. Mary Kicza Assistant Administrator NOAA Satellite & Info. Service (NESDIS) Space Weather Enterprise Forum
Continuity of Critical Space Weather Measurements Mary Kicza Assistant Administrator NOAA Satellite & Info. Service (NESDIS) Space Weather Enterprise Forum May 19, 2009 NOAA Space Weather Requirements
Analysis of Multi-Spacecraft Magnetic Field Data
COSPAR Capacity Building Beijing, 5 May 2004 Joachim Vogt Analysis of Multi-Spacecraft Magnetic Field Data 1 Introduction, single-spacecraft vs. multi-spacecraft 2 Single-spacecraft data, minimum variance
Rating Systems for Fixed Odds Football Match Prediction
Football-Data 2003 1 Rating Systems for Fixed Odds Football Match Prediction What is a Rating System? A rating system provides a quantitative measure of the superiority of one football team over their
Meeting the Grand Challenge of Protecting an Astronaut s Health: Electrostatic Active Space Radiation Shielding for Deep Space Missions
Meeting the Grand Challenge of Protecting an Astronaut s Health: Electrostatic Active Space Radiation Shielding for Deep Space Missions Ram Tripathi NASA Langley Research Center NIAC 2012 Spring Symposium,
How To Understand Space Weather
GOES Data and Products in the Space Weather Prediction Center and National Geophysical Data Center Mary Shouldis Satellite Data Product Development Team Lead NGDC/University of Colorado/CIRES Putting Science
Fluid Dynamics and the Navier-Stokes Equation
Fluid Dynamics and the Navier-Stokes Equation CMSC498A: Spring 12 Semester By: Steven Dobek 5/17/2012 Introduction I began this project through a desire to simulate smoke and fire through the use of programming
Experimental investigation of golf driver club head drag reduction through the use of aerodynamic features on the driver crown
Available online at www.sciencedirect.com Procedia Engineering 00 (2013) 000 000 www.elsevier.com/locate/procedia The 2014 conference of the International Sports Engineering Association Experimental investigation
Experiment #1, Analyze Data using Excel, Calculator and Graphs.
Physics 182 - Fall 2014 - Experiment #1 1 Experiment #1, Analyze Data using Excel, Calculator and Graphs. 1 Purpose (5 Points, Including Title. Points apply to your lab report.) Before we start measuring
Secondary Ion Mass Spectrometry
Secondary Ion Mass Spectrometry A PRACTICAL HANDBOOK FOR DEPTH PROFILING AND BULK IMPURITY ANALYSIS R. G. Wilson Hughes Research Laboratories Malibu, California F. A. Stevie AT&T Bell Laboratories Allentown,
Analyzing Structural Equation Models With Missing Data
Analyzing Structural Equation Models With Missing Data Craig Enders* Arizona State University [email protected] based on Enders, C. K. (006). Analyzing structural equation models with missing data. In G.
