Using Solar Active Region Latitude Analysis to Monitor Solar Cycle Progress
|
|
- Cecil Carroll
- 6 years ago
- Views:
Transcription
1 Using Solar Active Region Latitude Analysis to Monitor Solar Cycle Progress Published by RyeBrook Space Science Services 216 Abstract: This paper seeks to answer the question does solar active region latitude analysis (SARLA) have value as a means of tracking solar cycle progress? Whilst the SARLA data show the expected migration of solar active regions toward the solar equator as cycle 24 progresses toward maximum the effect is rather subtler than expected, and only becomes dramatically obvious when the data are presented in a certain manner. This research demonstrates that a single point of reference in the data gives little or no indication of solar cycle progression, and that SARLA is only useful as a retrospective tool for identifying solar cycle change-over. A coincidental finding of the research is a north-south hemisphere asymmetry of active region distribution that results in extended periods during the five-year data sample, when solar activity was completely absent from one hemisphere or the other. Whether this is scientifically significant or not is uncertain, and a further, more extended study is required in order to answer this question. Background: Since the 11-year solar activity cycle was first recognised in 1843, records have shown a repeating pattern in which solar active regions occur closer to the solar equator as the solar cycle progresses. This is evident in the well-known Butterfly Diagram (Figure1) that plots active region latitudes over the last 13 years. Some time after solar maximum, active regions abruptly migrate away from the solar equator, and thus we are able to assess when one cycle has ended, and the next has begun. In this paper, the author has taken data for active region latitudes for the five years leading up to the accepted maximum of solar cycle 24 a weak maximum and has arranged these data in spread sheet form for analysis. The intention of this process has been both to confirm the value of solar active region latitude analysis (SARLA) as a means of tracking solar cycle progress, and also to look for any other patterns that might be hidden in the data. This project was begun while the author was Director of the Land s End Solar Observatory (2-214). RyeBrook Space Science Services acquired ownership of LESO in 214, and subsequently disbanded the observatory in early 215. This paper is therefore presented as the intellectual property of RyeBrook Space.
2 Figure 1: The Butterfly Diagram. Source NASA Methodology: The capture of data for this study was time-consuming and laborious. For each day in the five-year sample period, there were four data-points. These were: the northerly extent and southerly extent of solar active regions in the northern solar hemisphere, and the northerly and southerly extent of solar active regions in the southern solar hemisphere. These extents had to be manually identified and extrapolated from the daily lists of latitude co-ordinates for all active regions. The resulting datasets comprised some 7,3 data-points. Because this large number of data is too cumbersome to use for analysis, and in order to smooth any errors, the average monthly values for the four extents of solar activity were calculated, reducing the number of data-points to just 24. These values, rounded to one decimal place were used to plot graphs for each year of the study, and a graph for all five years. A benefit of manually capturing all of these data was that any patterns hidden in the data became very apparent to the author. In the case of an apparent north-south hemisphere asymmetry of active region distribution, it was noted that there were a significant number of periods where solar activity was absent from one hemisphere or the other for several days at a time, and it was only by manually capturing all of the data that this became obvious. The need to analyse this phenomenon to ascertain its scientific significance, necessitated manipulation of the data to show a comparison between spotless days in the northern hemisphere, and those in the southern hemisphere during the five-year sample period. This meant changing the values of southern hemisphere episode to negatives in order to show both sets of data on the same graph in a meaningful way. When viewing this graph it is important to remember that values for northern and southern hemisphere are both actually positive.
3 Results: Solar Active Region Latitude Analysis 211 Monthly Averages January February March June August November December Figure 2: RyeBrook Space 215 There is a marked trend toward the solar equator in the southerly extent of active regions in the northern hemisphere. The northern extent of active regions in the northern hemisphere does not appear to shadow the southern extent, with the overall effect of a widening of the band of activity in the northern hemisphere. The extent of active regions in the southern hemisphere shows no particular trend, though there is an apparent widening of the band of activity toward the end of the year. There were occasions when solar activity was absent in the southern hemisphere for several days at a time. Solar Active Region Latitude Analysis 212 Monthly Averages January February March June August November December
4 Figure 3: RyeBrook Space 215 There is a marked trend toward the solar equator in the northerly extent of active regions in the northern hemisphere, as well as in the northerly extent of active regions in the southern hemisphere. The southern extent of active regions in both hemispheres does not seem to show any marked trend, with the exception of a last-minute convergence of the southern extent in the southern hemisphere, There were a significant number of occasions when solar activity was absent in the southern hemisphere for several days. This occurs much less frequently in the northern hemisphere, though more so than in the previous year. Solar Active Region Latitude Analysis 213 Monthly Averages January February March June August November December Figure 4: RyeBrook Space 215 There is a subtle general trend toward the solar equator in both hemispheres. This is most noticeable in the northern extent of the southern hemisphere active regions, Once again there were short periods when solar active regions were absent from the southern hemisphere, but more noticeably there were a significant number of periods where there was an absence of activity in the northern hemisphere. This seems to represent a change in the dynamics.
5 Solar Active Region Latitude Analysis 214 Monthly Averages January February March June August November December Figure 5: RyeBrook Space 215 There appears to be a levelling-out of active region latitudes during 214, with a significant widening of the band of activity toward the end of the year. Some short periods of an absence of activity in the northern hemisphere were noted, though less than in the previous year, and there were no periods of absence of activity in the southern hemisphere. Solar Active Region Latitude Analysis 215 Monthly Averages January February March June August November December Figure 6: RyeBrook Space 215 There is a much less marked trend in the data for 215, and there is certainly no dramatic convergence or divergence in the activity latitudes that would suggest an obvious solar maximum.
6 It is interesting to note though, that in the middle of January 215, active region 2262 came so close to the solar equator that it actually wandered between the northern and southern hemispheres for a few days. Once again it was noticed that there were periods of several days at a time during the year, when solar activity was completely absent from one hemisphere or another. It is therefore likely that these occurrences are of scientific significance, and should be studied in more detail. 211 to 215 Combined SARLA Monthly Averages Jan- 11 Jan- 12 Jan- 13 Jan- 14 Jan Figure 7: RyeBrook Space 216 Though there is a general trend in the five years data of a convergence of solar active regions toward the solar equator there is disappointingly no dramatic marker for the point of solar maximum. There is a more marked trend during 211 than later years, and the southerly extent of active regions in the northern hemisphere as well as the northerly extent of solar activity in the southern hemisphere, show the most marked convergence toward the equator. This at times results in a widening of the band of activity though it is noted that this widening closes again toward the end of the sample period. From Figure 1, it is apparent that convergence of the northerly extent of solar active regions in the northern hemisphere, and the southerly extent of active regions in the southern hemisphere, continues for some time after the point of solar maximum. Periods of Sun-spotless Days: The significance of periods of several days at a time where solar activity was completely absent from one hemisphere or the other is uncertain. In order to try to understand any scientific significance, spotless days by hemisphere were plotted for each month of the entire sample period to produce a graph. Values for the southern hemisphere were made negative
7 in order that they may be plotted in a meaningful way on the graph, but it must be remembered that these are in fact positive values. 5-5 Jan- 11 Jan- 12 Jan- 13 Jan- 14 Jan- 15 Spotless days northern hemisphere Spotless days southern hemisphere Figure 8: RyeBrook Space 216 A brief analysis of the resulting graph reveals a rough oscillation between spotless days in the northern hemisphere, and those in the southern hemisphere, with no obvious regular pattern. However, the distribution changes also do not appear entirely random. Conclusions: Figure 9: Progression of Solar Cycle 24
8 As can be seen in Figure 9, that the maximum of solar cycle 24 is far from distinct, with two main candidate peaks one in late 211, and another in early 214. In the SARLA data, these two points are not clearly defined by any significant convergence of active regions toward the equator. It is interesting that around the middle of January 215 it was noticed from the SARLA daily data, that active region 2262 came so close to the solar equator, that for several days it wandered between the northern and southern hemispheres (Figure ). This event shows as a dramatic, if brief convergence toward the solar equator, and if it were possible to identify the moment of solar maximum based solely upon SARLA data, this would probably be it; particularly as there was a reciprocal convergence in the northerly extent of activity in the northern hemisphere, and the southerly extent of activity in the southern hemisphere at the time. This represents the closest convergence during the entire five-year sample. Of course, this is seriously at odds with the sunspot count and radio flux definitions of the solar maximum. Unfortunately, the smoothing effect of monthly averaging of the data has rendered this event invisible in the yearly and five year plots. But to answer the question posed by the background of this project does SARLA analysis have value as a means of tracking solar cycle progress? is less easy than might at first have been thought. Although the SARLA data show a clear and marked migration of solar active regions toward the solar equator as the cycle proceeds, it is not until the point of abrupt divergence away from the equator again that we can clearly determine the end of one cycle, and the beginning of the next. As such, this will always be a retrospective analysis, and has no value in real-time solar cycle progression tracking Figure : January 215 Daily SARLA Values
9 Jan- 11 North erly Extent (Nort hern Hemis phere ) Figure 11: Adjustment of the aspect ratio of the five-year graph of SARLA values, so that the data-points become squashed together reveals the more familiar pattern that we see in the Butterfly Diagram, confirming that the convergence effect is real and measurable. When the aspect ratio of the five-year graph of daily SARLA values is adjusted so that the data-points are squashed up together, we see the reassuringly familiar pattern of the Butterfly Diagram (Figure 11). But we do not see the abrupt divergence away from the solar equator that signals the end of one solar cycle and the beginning of the next. This leads to an impression that cycle 24 had not ended by 31 December 215. Only a continued monitoring of SARLA data through the next 12 months will be likely to reveal the critical date of solar cycle change-over. The second objective of this research project was to look for any significant patterns that may be hidden in the data. During capture of the data it became very obvious that there were a significant number of periods of several days each year when solar activity was completely absent from one hemisphere or the other, and it was wondered whether this was scientifically significant. When considering this it was important to remember that the data were only being drawn from one view of the Sun that facing the Earth - and that the situation on the far side of the Sun at any given time may have been completely different i.e. there may have been no active regions in the southern hemisphere on the Earth-facing side, but there may have been on the far-side. Nonetheless, the visible portion is all that we have data for, and so the observation is made that there were a significant number of days each year, when solar active regions were absent from one hemisphere or the other on the visible side of the Sun. In their paper Asymmetrical Distribution of Sunspot Groups in the Solar Hemispheres, Li, et al. (22) identified a periodic north-south hemisphere asymmetry of sunspot distribution from historical data covering the period 1874 to 2, and suggested that there is a genuine periodic fluctuation that could lead to solar maximum being reached at a different time in each hemisphere (out of phase). They further suggest that this periodic phasing is likely to mean that solar cycle 24 will be south dominated. From the data gathered here, it is clear that there is a greater frequency of spotless days in the northern hemisphere, which tends to support this theory though it is also true to say that the southern hemisphere had longer periods of spotless days.
10 The phasing of north-south asymmetry of sunspot distribution is poorly understood, and is the subject of on-going research. It is likely to be a complex process, and has not yet been examined at five-year resolution. It is possible that continued investigation might reveal a finer periodic sub-phase within the courser 8-year phase, but this is pure conjecture. It is also important to realise that previous studies in this area have been of sunspot numbers, rather than the absences of sunspots used as a focus in this study. In summary, this project has shown very clearly that whilst SARLA data are a valuable diagnostic tool after the event, they probably have no viable role in real-time monitoring of solar cycle progress. SARLA data would appear to have no value in determining the point of solar maximum, but may be of use in determining the point of solar cycle change-over. The results have however, indicated very clearly that a continued period of observation is required in order to identify the point of divergence of active regions away from the solar equator that will signal that the next solar cycle has begun. Such a study would also collect further data that will enable a refined evaluation of the north-south asymmetry of active region distribution. References: Li, K.J. (22) Asymmetrical Distribution of Sunspot Groups in the Solar Hemispheres, Astronomical Society of Japan, vol. 54, pp RyeBrook Space 216. All rights reserved. No part of this publication may be reproduced in any form without the explicit prior permission of the Chief Executive. This publication has been created in accordance with our Learning Difference Policy. If you have a learning difference and you require the document in different format, please contact us at theryebrook@gmail.com and we will be pleased to help in any way we can.
Using Solar Active Region Latitude Analysis to Monitor Solar Cycle Progress
Using Solar Active Region Latitude Analysis to Monitor Solar Cycle Progress A Study Commissioned by RyeBrook Space Science Services RyeBrook Space 2017 Abstract: This paper seeks to answer the question
More informationLAB 2: Earth Sun Relations
LAB 2: Earth Sun Relations Name School The amount of solar energy striking the Earth s atmosphere is not uniform; distances, angles and seasons play a dominant role on this distribution of radiation. Needless
More informationThe Celestial Sphere. Chapter 1. Constellations. Models and Science. Constellations. Diurnal vs. Annular Motion 9/16/2010
The Celestial Sphere Chapter 1 Cycles of the Sky Vast distances to stars prevent us from sensing their true 3-D arrangement Naked eye observations treat all stars at the same distance, on a giant celestial
More informationYou have learned that Earth s 24-hour day night cycle is caused
76 A Year Viewed from Space C O M P U T E R S I M U L AT I O N You have learned that Earth s 24-hour day night cycle is caused by Earth s rotation around its axis. The year is another cycle caused by Earth
More informationGLOBAL SOLAR ACTIVITY IN CYCLE 24
GLOBAL SOLAR ACTIVITY IN CYCLE 24 Kiyoto Shibasaki (Solar Physics Research Inc.) SCOSTEP WDS@NiCT 1 Outline 1. Status of solar activity in Cycle 24 shown by total radio flux 2. Status of global solar activity
More informationC) the seasonal changes in constellations viewed in the night sky D) The duration of insolation will increase and the temperature will increase.
1. Which event is a direct result of Earth's revolution? A) the apparent deflection of winds B) the changing of the Moon phases C) the seasonal changes in constellations viewed in the night sky D) the
More informationMotions of the Sun Model Exploration
Name Date Bell Motions of the Sun Model Exploration 1. Go to the University of Nebraska-Lincoln Motions of the Sun Simulator: http://astro.unl.edu/naap/motion3/animations/sunmotions.swf 2. This is what
More informationTools of Astronomy Tools of Astronomy
Tools of Astronomy Tools of Astronomy The light that comes to Earth from distant objects is the best tool that astronomers can use to learn about the universe. In most cases, there is no other way to study
More informationLAB J - WORLD CLIMATE ZONES
Introduction LAB J - WORLD CLIMATE ZONES The objective of this lab is to familiarize the student with the various climates around the world and the climate controls that influence these climates. Students
More informationLab Activity: Climate Variables
Name: Date: Period: Water and Climate The Physical Setting: Earth Science Lab Activity: Climate Variables INTRODUCTION:! The state of the atmosphere continually changes over time in response to the uneven
More informationWeather to Climate Investigation: Maximum Temperature
Name: Date: Guiding Questions: Weather to Climate Investigation: Maximum Temperature What are the historical and current weather patterns or events for a location in the United States? What are the long-term
More information1-4-1A. Sun Structure
Sun Structure A cross section of the Sun reveals its various layers. The Core is the hottest part of the internal sun and is the location of nuclear fusion. The heat and energy produced in the core is
More informationCTU Presents. The Fitful Rise of Solar Cycle 24 What it Means in the Coming Year. Frank Donovan W3LPL
CTU Presents The Fitful Rise of Solar Cycle 24 What it Means in the Coming Year Frank Donovan W3LPL Introduction This presentation focuses on: The four major fall and winter DX contests: CQ WW SSB and
More informationWhich Earth latitude receives the greatest intensity of insolation when Earth is at the position shown in the diagram? A) 0 B) 23 N C) 55 N D) 90 N
1. In which list are the forms of electromagnetic energy arranged in order from longest to shortest wavelengths? A) gamma rays, x-rays, ultraviolet rays, visible light B) radio waves, infrared rays, visible
More informationLesson: Why We Have Seasons
Drexel-SDP GK-12 LESSON Lesson: Why We Have Seasons Subject Area(s) Earth and Space Associated Unit Astronomy, module 2 Lesson Title Lesson: Why We Have Seasons Grade Level 6 (3-7) Lesson # 4 of 4 Lesson
More informationby Jeffrey S. Keen BSc Hons ARCS MInstP CPhys CEng
Variation in Dowsing Measurements due to the Combined Vorticity in the Ecliptic Plane of the Earth s Orbit around the Sun, and the Spin of the Earth around its Tilted Axis by Jeffrey S. Keen BSc Hons ARCS
More informationSolar Time, Angles, and Irradiance Calculator: User Manual
Solar Time, Angles, and Irradiance Calculator: User Manual Circular 674 Thomas Jenkins and Gabriel Bolivar-Mendoza 1 Cooperative Extension Service Engineering New Mexico Resource Network College of Agricultural,
More informationExercise 6. Solar Panel Orientation EXERCISE OBJECTIVE DISCUSSION OUTLINE. Introduction to the importance of solar panel orientation DISCUSSION
Exercise 6 Solar Panel Orientation EXERCISE OBJECTIVE When you have completed this exercise, you will understand how the solar illumination at any location on Earth varies over the course of a year. You
More informationL.O: THE ANGLE OF INSOLATION ANGLE INSOLATION: THE ANGLE SUNLIGHT HITS THE EARTH
L.O: THE ANGLE OF INSOLATION ANGLE INSOLATION: THE ANGLE SUNLIGHT HITS THE EARTH 1. The graph below shows air temperatures on a clear summer day from 7 a.m. to 12 noon at two locations, one in Florida
More informationExemplar for Internal Achievement Standard. Mathematics and Statistics Level 3
Exemplar for internal assessment resource Mathematics and Statistics for Achievement Standard 91580 Exemplar for Internal Achievement Standard Mathematics and Statistics Level 3 This exemplar supports
More informationAgricultural Science Climatology Semester 2, Anne Green / Richard Thompson
Agricultural Science Climatology Semester 2, 2006 Anne Green / Richard Thompson http://www.physics.usyd.edu.au/ag/agschome.htm Course Coordinator: Mike Wheatland Course Goals Evaluate & interpret information,
More informationINFLUENCE OF THE AVERAGING PERIOD IN AIR TEMPERATURE MEASUREMENT
INFLUENCE OF THE AVERAGING PERIOD IN AIR TEMPERATURE MEASUREMENT Hristomir Branzov 1, Valentina Pencheva 2 1 National Institute of Meteorology and Hydrology, Sofia, Bulgaria, Hristomir.Branzov@meteo.bg
More informationAstronomy#2 - Notebook
Name Test Date Hour Astronomy#2 - Notebook Planet Earth LEARNING TARGETS I can describe a sphere and give evidence used to prove Earth is spherical. I can explain the difference between rotation and revolution.
More informationAstronomy Review. Use the following four pictures to answer questions 1-4.
Astronomy Review Use the following four pictures to answer questions 1-4. 1. Put an X through the pictures that are NOT possible. 2. Circle the picture that could be a lunar eclipse. 3. Triangle the picture
More informationCelestial Sphere. Altitude [of a celestial object] Zenith. Meridian. Celestial Equator
Earth Science Regents Interactive Path of the Sun University of Nebraska Resources Copyright 2011 by Z. Miller Name Period COMPANION WEBSITES: http://www.analemma.com/ http://www.stellarium.org/ INTRODUCTION:
More informationSentinel-1 Long Duration Mutual Interference
MPC-S1 Sentinel-1 Long Duration Mutual Interference Reference: Nomenclature: MPC-0432 DI-MPC-ARC Issue: 1. 0 Date: 2018,Dec.04 MPC-0432 DI-MPC-ARC V1.0 2018,Dec.04 i.1 Chronology Issues: Issue: Date: Reason
More informationLAB 3: THE SUN AND CLIMATE NAME: LAB PARTNER(S):
GEOG 101L PHYSICAL GEOGRAPHY LAB SAN DIEGO CITY COLLEGE SELKIN 1 LAB 3: THE SUN AND CLIMATE NAME: LAB PARTNER(S): The main objective of today s lab is for you to be able to visualize the sun s position
More informationGraphing Sea Ice Extent in the Arctic and Antarctic
Graphing Sea Ice Extent in the Arctic and Antarctic 1. Large amounts of ice form in some seasons in the oceans near the North Pole and the South Pole (the Arctic Ocean and the Southern Ocean). This ice,
More informationZW2000 and Your Sundial
1 The Sundial Primer created by At this point I assume that you have downloaded and set up ZW2000 on your computer. If not please read Getting Started with ZW2000. Initiate the program ZW2000. Figure 1
More informationUnusual Migration of Prominence Activities in the Southern Hemisphere during Cycles 23 24
PASJ: Publ. Astron. Soc. Japan 65, S16, 213 December 5 c 213. Astronomical Society of Japan. Unusual Migration of Prominence Activities in the Southern Hemisphere during Cycles 23 24 Masumi SHIMOJO National
More informationSolar photovoltaic energy production comparison of east, west, south-facing and tracked arrays
The Canadian Society for Bioengineering The Canadian society for engineering in agricultural, food, environmental, and biological systems. La Société Canadienne de Génie Agroalimentaire et de Bioingénierie
More informationPasswords. ScienceVocabulary
Passwords ScienceVocabulary F To the Student Mitosis. Apogee. Ion. Sometimes it seems that scientists speak a language all their own. Passwords: Science Vocabulary will help you learn the words you need
More informationGrade 6 Standard 2 Unit Test Astronomy
Grade 6 Standard 2 Unit Test Astronomy Multiple Choice 1. Why does the air temperature rise in the summer? A. We are closer to the sun. B. The air becomes thicker and more dense. C. The sun s rays are
More informationA. Windnagel M. Savoie NSIDC
National Snow and Ice Data Center ADVANCING KNOWLEDGE OF EARTH'S FROZEN REGIONS Special Report #18 06 July 2016 A. Windnagel M. Savoie NSIDC W. Meier NASA GSFC i 2 Contents List of Figures... 4 List of
More information5. In which diagram is the observer experiencing the greatest intensity of insolation? A) B)
1. Which factor has the greatest influence on the number of daylight hours that a particular Earth surface location receives? A) longitude B) latitude C) diameter of Earth D) distance from the Sun 2. In
More informationTime, coordinates and how the Sun and Moon move in the sky
Time, coordinates and how the Sun and Moon move in the sky Using the colors and magnitudes of quasars drawn from the SDSS Catalog Archive Server to distinguish quasars from stars using the light they emit
More informationWhat s the longest single-shot exposure ever recorded of any object or area of space by Hubble?
Hubblecast Episode 50: Q&A with Dr J 00:00 Have you ever wondered why Hubble can make detailed images of of galaxies, but stars appear as featureless blobs? What the most distant object ever observed is?
More informationTILT, DAYLIGHT AND SEASONS WORKSHEET
TILT, DAYLIGHT AND SEASONS WORKSHEET Activity Description: Students will use a data table to make a graph for the length of day and average high temperature in Utah. They will then answer questions based
More information1.6 TRENDS AND VARIABILITY OF SNOWFALL AND SNOW COVER ACROSS NORTH AMERICA AND EURASIA. PART 2: WHAT THE DATA SAY
1.6 TRENDS AND VARIABILITY OF SNOWFALL AND SNOW COVER ACROSS NORTH AMERICA AND EURASIA. PART 2: WHAT THE DATA SAY David A. Robinson* Rutgers University, Department of Geography, Piscataway, New Jersey
More informationThe Effects of Gravity on the Mind s Perception by Jeffrey S. Keen BSc Hons ARCS MInstP CPhys CEng
The Effects of Gravity on the Mind s Perception by Jeffrey S. Keen BSc Hons ARCS MInstP CPhys CEng www.jeffreykeen.org Abstract This paper demonstrates that by using Noetics, the mind can quantitatively
More information5 - Seasons. Figure 1 shows two pictures of the Sun taken six months apart with the same camera, at the same time of the day, from the same location.
ASTR 110L 5 - Seasons Purpose: To plot the distance of the Earth from the Sun over one year and to use the celestial sphere to understand the cause of the seasons. What do you think? Write answers to questions
More informationWorksheet: The Climate in Numbers and Graphs
Worksheet: The Climate in Numbers and Graphs Purpose of this activity You will determine the climatic conditions of a city using a graphical tool called a climate chart. It represents the long-term climatic
More information13.7 ANOTHER TEST FOR TREND: KENDALL S TAU
13.7 ANOTHER TEST FOR TREND: KENDALL S TAU In 1969 the U.S. government instituted a draft lottery for choosing young men to be drafted into the military. Numbers from 1 to 366 were randomly assigned to
More informationPractice Questions: Seasons #1
1. Seasonal changes on Earth are primarily caused by the A) parallelism of the Sun's axis as the Sun revolves around Earth B) changes in distance between Earth and the Sun C) elliptical shape of Earth's
More information18.2 Earth Cycles Days and years Calendars Years and days Leap years Calendars throughout human history 20,000 years ago. 7,000 BC. 4,000 BC.
18.2 Reading 18.2 Earth Cycles Do you ever wonder where our calendar comes from? Or why the Moon gradually changes its shape? Or why we have seasons? The answers have to do with the relative positions
More informationGeography Class 6 Chapters 3 and
CHAPTER 3 MOTIONS OF THE EARTH The Earth is always travelling in Space. That makes each person on Earth, a Space Traveller. No one feels the movement of the Earth because humans are too tiny when compared
More informationThe Large Scale Response of the Upper Ocean to Atmospheric Forcing During TOGA-COARE
499 The Large Scale Response of the Upper Ocean to Atmospheric Forcing During TOGA-COARE K.J. Richards and M.E. Inall, Department of Oceanography, University of Southampton, England G. Eldin and C. Henin,
More informationSignificant Figure Rules
Significant Figure Rules There are three rules on determining how many significant figures are in a number: 1 Non-zero digits are always significant. 2 Any zeros between two significant digits are significant.
More informationP4.2 THE THREE DIMENSIONAL STRUCTURE AND TIME EVOLUTION OF THE DECADAL VARIABILITY REVEALED IN ECMWF REANALYSES
P4.2 THE THREE DIMENSIONAL STRUCTURE AND TIME EVOLUTION OF THE DECADAL VARIABILITY REVEALED IN ECMWF REANALYSES Taehyoun Shim 1, Gyu-Ho Lim* 1 and Dong-In Lee 2 1 School of Earth and Environmental Sciences,
More informationGeographic Information Systems (GIS) and inland fishery management
THEMATIC REPORT Geographic Information Systems (GIS) and inland fishery management Stratified inland fisheries monitoring using GIS Gertjan DE GRAAF Nefisco, Amsterdam, the Netherlands Felix MARTTIN and
More informationAnalyzing Solar Energy Graphs: MY NASA DATA
LIVE INTERACTIVE LEARNING @ YOUR DESKTOP Analyzing Solar Energy Graphs: MY NASA DATA Presented by: Alissa Keil September 12, 2011 MY NASA DATA Know your Earth video http://www.youtube.com/watch? v=d2kh_z720ia
More informationMonthly Magnetic Bulletin
BRITISH GEOLOGICAL SURVEY Ascension Island Observatory Monthly Magnetic Bulletin December 2008 08/12/AS Crown copyright; Ordnance Survey ASCENSION ISLAND OBSERVATORY MAGNETIC DATA 1. Introduction Ascension
More informationName: Exam 1, 9/30/05
Multiple Choice: Select the choice that best answers each question. Write your choice in the blank next to each number. (2 points each) 1. At the North Pole in mid-november, the sun rises at a. North of
More informationLecture Tutorial: Measuring the Frequency and Period of Sunspots
Lecture Tutorial: Measuring the Frequency and Period of Sunspots Description: This data analysis activity requires students to analyze sunspots on NASA s SOHO coronagraph images to make meaning of cyclical
More informationDescription of the Temperature Observation and Averaging Methods Used at the Blue Hill Meteorological Observatory
Description of the Temperature Observation and Averaging Methods Used at the Blue Hill Meteorological Observatory Michael J. Iacono Blue Hill Meteorological Observatory November 2015 The Blue Hill Meteorological
More informationWhich phase of the Moon will be seen from the Earth at position 5? A) B) C) D)
Name Date 1. Which motion causes the Moon to show phases when viewed from the Earth? A) the rotation of the Moon on its axis B) the revolution of the Moon around the Earth C) the rotation of the Sun on
More informationWhat's Up, Earth? Header Insert Image 1 here, right justified to wrap. Grade Level. 3rd. Time Required: 60 minutes
What's Up, Earth? Header Insert Image 1 here, right justified to wrap Image 1 ADA Description:? Caption:? Image file path:? Source/Rights: Copyright? Grade Level 3rd Time Required: 60 minutes Group Size:
More informationWhich graph best shows the relationship between intensity of insolation and position on the Earth's surface? A) B) C) D)
1. The hottest climates on Earth are located near the Equator because this region A) is usually closest to the Sun B) reflects the greatest amount of insolation C) receives the most hours of daylight D)
More informationAstronomy Merit Badge Workbook
Merit Badge Workbook This workbook can help you but you still need to read the merit badge pamphlet. This Workbook can help you organize your thoughts as you prepare to meet with your merit badge counselor.
More informationIn The Sky This Quarter
WEST VIRGINIA UNIVERSITY EBERLY COLLEGE OF ARTS AND SCIENCES THE DEPARTMENT OF PHYSICS TOMCHIN PLANETARIUM AND OBSERVATORY Volume 11, Issue 1 http://planetarium.wvu.edu/ January - March 2011 On January
More information2012 Assessment Report. Mathematics with Calculus Level 3 Statistics and Modelling Level 3
National Certificate of Educational Achievement 2012 Assessment Report Mathematics with Calculus Level 3 Statistics and Modelling Level 3 90635 Differentiate functions and use derivatives to solve problems
More informationHigh Wind and Energy Specific Models for Global. Production Forecast
High Wind and Energy Specific Models for Global Production Forecast Carlos Alaíz, Álvaro Barbero, Ángela Fernández, José R. Dorronsoro Dpto. de Ingeniería Informática and Instituto de Ingeniería del Conocimiento
More informationWhich table correctly shows the dates on which the apparent paths of the Sun were observed? A) B) C) D)
1. The diagram below represents the horizon and the Sun's apparent paths, A, B, and C, on three different dates, as viewed from the same location in New York State. Which table correctly shows the dates
More informationCAN SOLAR ACTIVITY INFLUENCE THE OCCURRENCE OF RECESSIONS? Mikhail Gorbanev January 2015
CAN SOLAR ACTIVITY INFLUENCE THE OCCURRENCE OF RECESSIONS? Mikhail Gorbanev January 2015 Outline What are the sunspots, solar cycles, and solar maximums? Literature: Jevons and Chizhevsky Methodology:
More informationSolar Activity during the Rising Phase of Solar Cycle 24
International Journal of Astronomy and Astrophysics, 213, 3, 212-216 http://dx.doi.org/1.4236/ijaa.213.3325 Published Online September 213 (http://www.scirp.org/journal/ijaa) Solar Activity during the
More informationEarth Moon Motions A B1
Earth Moon Motions A B1 1. The Coriolis effect provides evidence that Earth (1) rotates on its axis (2) revolves around the Sun (3) undergoes cyclic tidal changes (4) has a slightly eccentric orbit 9.
More informationSunspot Cycle Worksheet
Sunspot Cycle Worksheet Read the Explore information and answer the Explain questions in your own words. Explore: Global warming and climate change are international concerns and the focus of much controversy.
More informationAnalysis of the 500 mb height fields and waves: testing Rossby wave theory
Analysis of the 500 mb height fields and waves: testing Rossby wave theory Jeffrey D. Duda, Suzanne Morris, Michelle Werness, and Benjamin H. McNeill Department of Geologic and Atmospheric Sciences, Iowa
More informationMeteorology. Circle the letter that corresponds to the correct answer
Chapter 3 Worksheet 1 Meteorology Name: Circle the letter that corresponds to the correct answer 1) If the maximum temperature for a particular day is 26 C and the minimum temperature is 14 C, the daily
More informationPractice Seasons Moon Quiz
1. Which diagram represents the tilt of Earth's axis relative to the Sun's rays on December 15? A) B) C) D) 2. The diagram below represents Earth in space on the first day of a season. 5. Base your answer
More informationWill a warmer world change Queensland s rainfall?
Will a warmer world change Queensland s rainfall? Nicholas P. Klingaman National Centre for Atmospheric Science-Climate Walker Institute for Climate System Research University of Reading The Walker-QCCCE
More informationPage 1. Name:
Name: 1) What is the primary reason New York State is warmer in July than in February? A) The altitude of the noon Sun is greater in February. B) The insolation in New York is greater in July. C) The Earth
More information1.4j interpret simple shadow stick data to determine local noon and observer s longitude
1.4j interpret simple shadow stick data to determine local noon and observer s longitude There are many opportunities for making observations of shadows cast with a vertical stick and the Sun. Observations
More informationAstronomy 10 Introduction to the Solar System
Astronomy 10 Introduction to the Solar System http://lpc1.clpccd.cc.ca.us/lpc/murray/astro10/a10intro.htm This is your source for all things in this class: 1. Grading policies. 2. What topics we ll covering.
More informationCoordinates on the Sphere
Survey Observations Coordinates on the Sphere Any position on the surface of a sphere (such as the Earth or the night sky) can be expressed in terms of the angular coordinates latitude and longitude Latitude
More information[04] Seasons, Phases, and Eclipses (9/7/17)
1 [04] Seasons, Phases, and Eclipses (9/7/17) Upcoming Items Homework #2 due next lecture. Read Ch. 3.3 and do the self-study quizzes for next lecture, and skim 2.4, 3.1, 3.2, & 3.4. https://pbs.twimg.com/media/dh69il_u0aenivq.jpg:large
More informationSeasonal Variations of the Urban Heat Island Effect:
Seasonal Variations of the Urban Heat Island Effect: Examining the Differences in Temperature Between the City of Philadelphia and its Outlying Suburbs By: Frank Vecchio 1 P a g e We re calling for a high
More informationCuba. General Climate. Recent Climate Trends. UNDP Climate Change Country Profiles. Temperature. C. McSweeney 1, M. New 1,2 and G.
UNDP Climate Change Country Profiles Cuba C. McSweeney 1, M. New 1,2 and G. Lizcano 1 1. School of Geography and Environment, University of Oxford. 2. Tyndall Centre for Climate Change Research http://country-profiles.geog.ox.ac.uk
More informationStudent s guide CESAR Science Case The Venus transit and the Earth-Sun distance
Student s guide CESAR Science Case The Venus transit and the Earth-Sun distance By: Abel de Burgos and Assiye Süer Name Date Introduction A transit happens when a body passes, or transits, in front of
More informationInternational Space Station (ISS) Nears A Six-Figure Orbit Count
1. Introduction Adopting the definition consistent with ubiquitous two-line element sets (TLEs) used to track virtually any artifact orbiting Earth, an orbit count n tallies the number of northbound equator
More informationAstron 104 Laboratory #7 Sunspots and the Solar Cycle
Name: Section: Astron 104 Laboratory #7 Sunspots and the Solar Cycle Section 9.4 In this exercise, you will observe how the physical appearance of the Sun changes from day to day over the period of one
More informationThe Solar Cycle or El Niño Southern Oscillation (ENSO) as a Criterion for the Definition of Public Policies
The Solar Cycle or El Niño Southern Oscillation (ENSO) as a Criterion for the Definition of Public Policies Juan Manuel Rodríguez Torres* Gerardo Zavala Guzmán** * e-mail: rodrito@ugto.mx; Departamento
More informationJackson County 2013 Weather Data
Jackson County 2013 Weather Data 61 Years of Weather Data Recorded at the UF/IFAS Marianna North Florida Research and Education Center Doug Mayo Jackson County Extension Director 1952-2008 Rainfall Data
More informationRegents Earth Science Unit 7: Water Cycle and Climate
Regents Earth Science Unit 7: Water Cycle and Climate Name Section Coastal and Continental Temperature Ranges Lab # Introduction: There are large variations in average monthly temperatures among cities
More informationThird Grade Math and Science DBQ Weather and Climate/Representing and Interpreting Charts and Data
Third Grade Math and Science DBQ Weather and Climate/Representing and Interpreting Charts and Data A document based question (DBQ) is an authentic assessment where students interact with content related
More informationTIME SERIES COMPARISONS OF MIPAS LEVEL 2 NEAR REAL TIME PRODUCTS WITH CLIMATOLOGY
TIME SERIES COMPARISONS OF MIPAS LEVEL 2 NEAR REAL TIME PRODUCTS WITH CLIMATOLOGY Vivienne Payne, Anu Dudhia, and Chiara Piccolo Atmospheric, Oceanic and Planetary Physics, Department of Physics, University
More informationPRELIMINARY DRAFT FOR DISCUSSION PURPOSES
Memorandum To: David Thompson From: John Haapala CC: Dan McDonald Bob Montgomery Date: February 24, 2003 File #: 1003551 Re: Lake Wenatchee Historic Water Levels, Operation Model, and Flood Operation This
More informationAntigua and Barbuda. General Climate. Recent Climate Trends. UNDP Climate Change Country Profiles. Temperature
UNDP Climate Change Country Profiles Antigua and Barbuda C. McSweeney 1, M. New 1,2 and G. Lizcano 1 1. School of Geography and Environment, University of Oxford. 2. Tyndall Centre for Climate Change Research
More informationAstronomy A BEGINNER S GUIDE TO THE UNIVERSE EIGHTH EDITION
Astronomy A BEGINNER S GUIDE TO THE UNIVERSE EIGHTH EDITION CHAPTER 0 Charting the Heavens Lecture Presentation 0.0 Astronmy a why is that subject! Q. What rare astronomical event happened in late summer
More information1. The pictures below show the Sun at midday. Write winter, spring or summer under the correct picture.
Test 2 1. The pictures below show the Sun at midday. Write winter, spring or summer under the correct picture. 2. Look carefully at the phases of the Moon. Number them (1 to 4) in the order that you would
More informationFibonacci Numbers. November 7, Fibonacci's Task: Figure out how many pairs of rabbits there will be at the end of one year, following rules.
Fibonacci Numbers November 7, 2010 Fibonacci's Task: Figure out how many pairs of rabbits there will be at the end of one year, following rules. Rules: 1. Start with a pair of new rabbits, born in December.
More informationCurrent Status of COMS AMV in NMSC/KMA
Current Status of COMS AMV in NMSC/KMA Eunha Sohn, Sung-Rae Chung, Jong-Seo Park Satellite Analysis Division, NMSC/KMA soneh0431@korea.kr COMS AMV of KMA/NMSC has been produced hourly since April 1, 2011.
More informationRAINFALL AVERAGES AND SELECTED EXTREMES FOR CENTRAL AND SOUTH FLORIDA. Thomas K. MacVicar
TECHNICAL PUBLICATION #83-2 March 1983 RAINFALL AVERAGES AND SELECTED EXTREMES FOR CENTRAL AND SOUTH FLORIDA by Thomas K. MacVicar "This public document was promulgated at an annual cost of $136.74, or
More informationMiSP Astronomy - Seasons Worksheet #1 L2
MiSP Astronomy - Seasons Worksheet #1 L2 Name Date Changing Hours of Daylight on Long Island (L 1, 2, 3) Introduction You sometimes hear people say, Days are longer in the summer and shorter in the winter.
More informationFIT100 Spring 01. Project 2. Astrological Toys
FIT100 Spring 01 Project 2 Astrological Toys In this project you will write a series of Windows applications that look up and display astrological signs and dates. The applications that will make up the
More informationTHE SUN. LENGTH: Course of the semester
ASTR 1030 Astronomy Lab 139 The Sun THE SUN SYNOPSIS: This exercise involves making measurements of the Sun every week throughout the semester, and then analyzing your results at semester s end. You ll
More informationWeather Dynamics. Amazing Weather!
Lesson1Weather Hurricane Igor, St. John's, 2010 Tsunami, Japan, 2011 Amazing Weather! Weather Dynamics Weather Dynamics is the study of how the movement of water and air causes weather patterns. The main
More informationIMPROVING LIGHT PENETRATION FOR GOLF GREENS Scott Robinson ArborCom Technologies Halifax, Nova Scotia
IMPROVING LIGHT PENETRATION FOR GOLF GREENS Scott Robinson ArborCom Technologies Halifax, Nova Scotia SEASONAL SUN ANGLE CHANGES Definitions Summer Solstice Sun rises and sets farthest away from south
More informationNAVIGATION THEORY QUESTIONS Basics of Navigation
NAVIGATION THEORY QUESTIONS Basics of Navigation Q610065 look at it The angle between the plane of the ecliptic and the plane of equator is approx? 23.5 degrees In which two months of the year is the difference
More informationASTRONOMY Merit Badge Requirements
ASTRONOMY Merit Badge Requirements 1) Do the following: A) Sketch the face of the moon, indicating on it the locations of at least five seas and five craters. B) Within a single week, sketch the position
More information