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E a S T 7 4 T H S T R E E T August 2021 Schedule
E A S T 7 4 T H S T R E E T KEY St udi o key on bac k SEPT EM BER 2021 SC H ED U LE EF F EC T IVE 09.01.21–09.30.21 Bolld New Class, Instructor, or Time ♦ Advance sign-up required M O NDA Y T UE S DA Y W E DNE S DA Y T HURS DA Y F RII DA Y S A T URDA Y S UNDA Y Atthllettiic Master of One Athletic 6:30–7:15 METCON3 6:15–7:00 Stacked! 8:00–8:45 Cycle Beats 8:30–9:30 Vinyasa Yoga 6:15–7:00 6:30–7:15 6:15–7:00 Condiittiioniing Gerard Conditioning MS ♦ Kevin Scott MS ♦ Steve Mitchell CS ♦ Mike Harris YS ♦ Esco Wilson MS ♦ MS ♦ MS ♦ Stteve Miittchellll Thelemaque Boyd Melson 7:00–7:45 Cycle Power 7:00–7:45 Pilates Fusion 8:30–9:15 Piillattes Remiix 9:00–9:45 Cardio Sculpt 6:30–7:15 Cycle Beats 7:00–7:45 Cycle Power 6:30–7:15 Cycle Power CS ♦ Candace Peterson YS ♦ Mia Wenger YS ♦ Sammiie Denham MS ♦ Cindya Davis CS ♦ Serena DiLiberto CS ♦ Shweky CS ♦ Jason Strong 7:15–8:15 Vinyasa Yoga 7:45–8:30 Firestarter + Best Firestarter + Best 9:30–10:15 Cycle Power 7:15–8:05 Athletic Yoga Off The Barre Josh Mathew- Abs Ever 9:00–9:45 CS ♦ Jason Strong 7:00–8:00 Vinyasa Yoga 7:00–7:45 YS ♦ MS ♦ MS ♦ Abs Ever YS ♦ Elitza Ivanova YS ♦ Margaret Schwarz YS ♦ Sarah Marchetti Meier Shane Blouin Luke Bernier 10:15–11:00 Off The Barre Gleim 8:00–8:45 Cycle Beats 7:30–8:15 Precision Run® 7:30–8:15 Precision Run® 8:45–9:45 Vinyasa Yoga Cycle Power YS ♦ Cindya Davis Gerard 7:15–8:00 Precision Run® TR ♦ Kevin Scott YS ♦ Colleen Murphy 9:15–10:00 CS ♦ Nikki Bucks TR ♦ CS ♦ Candace 10:30–11:15 Atletica Thelemaque TR ♦ Chaz Jackson Peterson 8:45–9:30 Pilates Fusion 8:00–8:45 -
TYPHOONS and DEPRESSIONS OVER the FAR EAST Morning Observation, Sep Teinber 6, from Rasa Jima Island by BERNARDF
SEPTEMBER1940 MONTHLY WEATHER REVIEW 257 days west of the 180th meridian. In American coastal appear to be independent of the typhoon of August 28- waters fog was noted on 10 days each off Washington and September 5, are the following: The S. S. Steel Exporter California; on 4 days off Oregon; and on 3 days off Lower reported 0700 G. C. T. September 6, from latitude 20'18' California. N., longitude 129'30'E.) a pressure of 744.8 mm. (993.0 nib.) with west-northwest winds of force 9. Also, the TYPHOONS AND DEPRESSIONS OVER THE FAR EAST morning observation, Sep teinber 6, from Rasa Jima Island By BERNARDF. DOUCETTE, J. (one of the Nansei Island group) was 747.8 mm. (997.0 5. mb.) for pressure and east-northeast, force 4, for winds. [Weather Bureau, Manila, P. I.] Typhoon, September 11-19) 1940.-A depression, moving Typhoon, August %!-September 6,1940.-A low-pressure westerly, passed about 200 miles south of Guam and area far to the southeast of Guam moved west-northwest, quickly inclined to the north, intensifying to typhoon rapidly developing to typhoon intensity as it proceeded. strength, September 11 to 13. It was stationary, Sep- When the center reached the regions about 250 miles tember 13 and 14, about 150 miles west-northwest of west of Guam, the direction changed to the northwest, Guam, and then began a northwesterly and northerly and the storm continued along this course until it reached course to the ocean regions about 300 miles west of the the latitude of southern Formosa. -
Basic Principles of Celestial Navigation James A
Basic principles of celestial navigation James A. Van Allena) Department of Physics and Astronomy, The University of Iowa, Iowa City, Iowa 52242 ͑Received 16 January 2004; accepted 10 June 2004͒ Celestial navigation is a technique for determining one’s geographic position by the observation of identified stars, identified planets, the Sun, and the Moon. This subject has a multitude of refinements which, although valuable to a professional navigator, tend to obscure the basic principles. I describe these principles, give an analytical solution of the classical two-star-sight problem without any dependence on prior knowledge of position, and include several examples. Some approximations and simplifications are made in the interest of clarity. © 2004 American Association of Physics Teachers. ͓DOI: 10.1119/1.1778391͔ I. INTRODUCTION longitude ⌳ is between 0° and 360°, although often it is convenient to take the longitude westward of the prime me- Celestial navigation is a technique for determining one’s ridian to be between 0° and Ϫ180°. The longitude of P also geographic position by the observation of identified stars, can be specified by the plane angle in the equatorial plane identified planets, the Sun, and the Moon. Its basic principles whose vertex is at O with one radial line through the point at are a combination of rudimentary astronomical knowledge 1–3 which the meridian through P intersects the equatorial plane and spherical trigonometry. and the other radial line through the point G at which the Anyone who has been on a ship that is remote from any prime meridian intersects the equatorial plane ͑see Fig. -
Celestial Navigation Tutorial
NavSoft’s CELESTIAL NAVIGATION TUTORIAL Contents Using a Sextant Altitude 2 The Concept Celestial Navigation Position Lines 3 Sight Calculations and Obtaining a Position 6 Correcting a Sextant Altitude Calculating the Bearing and Distance ABC and Sight Reduction Tables Obtaining a Position Line Combining Position Lines Corrections 10 Index Error Dip Refraction Temperature and Pressure Corrections to Refraction Semi Diameter Augmentation of the Moon’s Semi-Diameter Parallax Reduction of the Moon’s Horizontal Parallax Examples Nautical Almanac Information 14 GHA & LHA Declination Examples Simplifications and Accuracy Methods for Calculating a Position 17 Plane Sailing Mercator Sailing Celestial Navigation and Spherical Trigonometry 19 The PZX Triangle Spherical Formulae Napier’s Rules The Concept of Using a Sextant Altitude Using the altitude of a celestial body is similar to using the altitude of a lighthouse or similar object of known height, to obtain a distance. One object or body provides a distance but the observer can be anywhere on a circle of that radius away from the object. At least two distances/ circles are necessary for a position. (Three avoids ambiguity.) In practice, only that part of the circle near an assumed position would be drawn. Using a Sextant for Celestial Navigation After a few corrections, a sextant gives the true distance of a body if measured on an imaginary sphere surrounding the earth. Using a Nautical Almanac to find the position of the body, the body’s position could be plotted on an appropriate chart and then a circle of the correct radius drawn around it. In practice the circles are usually thousands of miles in radius therefore distances are calculated and compared with an estimate. -
Understanding Celestial Navigation by Ron Davidson, SN Poverty Bay Sail & Power Squadron
Understanding Celestial Navigation by Ron Davidson, SN Poverty Bay Sail & Power Squadron I grew up on the Jersey Shore very near the entrance to New York harbor and was fascinated by the comings and goings of the ships, passing the Ambrose and Scotland light ships that I would watch from my window at night. I wondered how these mariners could navigate these great ships from ports hundreds or thousands of miles distant and find the narrow entrance to New York harbor. Celestial navigation was always shrouded in mystery that so intrigued me that I eventually began a journey of discovery. One of the most difficult tasks for me, after delving into the arcane knowledge presented in most reference books on the subject, was trying to formulate the “big picture” of how celestial navigation worked. Most texts were full of detailed "cookbook" instructions and mathematical formulas teaching the mechanics of sight reduction and how to use the almanac or sight reduction tables, but frustratingly sparse on the overview of the critical scientific principles of WHY and HOW celestial works. My end result was that I could reduce a sight and obtain a Line of Position but I was unsatisfied not knowing “why” it worked. This article represents my efforts at learning and teaching myself 'celestial' and is by no means comprehensive. As a matter of fact, I have purposely ignored significant detail in order to present the big picture of how celestial principles work so as not to clutter the mind with arcane details and too many magical formulas. The USPS JN & N courses will provide all the details necessary to ensure your competency as a celestial navigator. -
Chapter 7 Mapping The
BASICS OF RADIO ASTRONOMY Chapter 7 Mapping the Sky Objectives: When you have completed this chapter, you will be able to describe the terrestrial coordinate system; define and describe the relationship among the terms com- monly used in the “horizon” coordinate system, the “equatorial” coordinate system, the “ecliptic” coordinate system, and the “galactic” coordinate system; and describe the difference between an azimuth-elevation antenna and hour angle-declination antenna. In order to explore the universe, coordinates must be developed to consistently identify the locations of the observer and of the objects being observed in the sky. Because space is observed from Earth, Earth’s coordinate system must be established before space can be mapped. Earth rotates on its axis daily and revolves around the sun annually. These two facts have greatly complicated the history of observing space. However, once known, accu- rate maps of Earth could be made using stars as reference points, since most of the stars’ angular movements in relationship to each other are not readily noticeable during a human lifetime. Although the stars do move with respect to each other, this movement is observable for only a few close stars, using instruments and techniques of great precision and sensitivity. Earth’s Coordinate System A great circle is an imaginary circle on the surface of a sphere whose center is at the center of the sphere. The equator is a great circle. Great circles that pass through both the north and south poles are called meridians, or lines of longitude. For any point on the surface of Earth a meridian can be defined. -
A Modern Look at the Earth's Climate Mechanism and the Cosmo-Geophysical System of the Earth
A modern look at the Earth's climate mechanism and the cosmo-geophysical system of the Earth Bogdan Góralski Library of the Historical Institute of the University of Warsaw I. Introduction Is the earth's climate getting warmer? My research shows that indeed the atmosphere and hydrosphere of the northern hemisphere warmed up during XIX-XXI centuries but the southern hemisphere getting colder. However, this warming of the northern hemisphere is not caused by excessive carbon dioxide emission caused by the developing human civilization, but is caused by the gravitational-magnetic influences of the Solar System on the rotating Earth as a result of which the outer layer of the Earth's rotates. Being in the move the Earth's coating changes its position relative to the ecliptic plane and along with its movement, over surface of the Earth's, is the shift of the zones of life-giving rainfalls that are stable relative to ecliptic plane. This results in a global economic and social events in the form of regional crises in areas affected by the drought or excessive precipitation. Physical phenomena related to the movement of the Earth's coating and evidence of the occurrence of this phenomenon are presented in the following work. Jakuszowice, 27 July 2019, 15: 10 Bogdan Góralski II. Scheme of the climate mechanism of the Earth 1. Northern hemisphere climate warming and southern hemisphere cooling. Increased magnetic activity of the Sun caused by gravitational interactions of solar system planets is marked in increase of solar wind power and reduction of power of cosmic rays in Earth's atmosphere, gravitational influence of the Sun, Moon, planets on Earth's coating (Earth's coating = crust + earth's mantle) causing rotate of Earth's coating around liquid earth core. -
Exercise 3.0 the CELESTIAL HORIZON SYSTEM
Exercise 3.0 THE CELESTIAL HORIZON SYSTEM I. Introduction When we stand at most locations on the Earth, we have the distinct impression that the Earth is flat. This occurs because the curvature of the small area of the Earth usually visible is very slight. We call this “flat Earth” the Plane of the Horizon and divide it up into 4 quadrants, each containing 90o, by using the cardinal points of the compass. The latter are the North, South, East, and west points of the horizon. We describe things as being vertical or “straight up” if they line up with the direction of gravity at that location. It is easy for us to determine “straight up” because we have a built in mechanism for this in the inner ear (the semicircular canals). Because it seems so “natural”, we build a coordinate system on these ideas called the Horizon System. The Celestial Horizon System is one of the coordinate systems that astronomers find useful for locating objects in the sky. It is depicted in the Figure below. Figure 1. The above diagram is a skewed perspective, schematic diagram of the celestial sphere with circles drawn only for the half above the horizon. Circles on the far side, or western half, of the celestial sphere are drawn as dashed curves. All the reference circles of this system do not share in the rotation of the celestial sphere and, therefore, this coordinate system is fixed with respect to a given observer. The basis for the system is the direction of gravity. We can describe this as the line from the observer on the surface of the Earth through the center of the Earth. -
Theory of Direction Kaustav B
Research Article Nanotechnology & Applications Theory of Direction Kaustav B. Arya* *Correspondence: Kaustav B. Arya, Assam Jatiya Bidyalay, Guwahati, Assam (Research works in IASST), Assam, India, Tel: +91- 9435013881; E-mail: [email protected]. Guwahati, Assam (Research works in IASST), Assam, India. Received: 30 September 2018; Accepted: 16 October 2018 Citation: Kaustav B. Arya. Theory of Direction. Nano Tech Appl. 2018; 1(2): 1-2. ABSTRACT Here, the research tries to find a connection between law of gravitation and magnetic poles. Keywords Electromagnetism shows that magnetic fields are created vertically Gravitation, Magnetic poles, Earth, Space. if electricity flows horizontally. Introduction In this way our planet has magnetic poles north and south vertically. The law of gravitation indicates that every object of the universe But in this huge universe it is always possible to have such objects attracts each other. On the other side we determine our earth’s which rotate vertically from north to south in their rotatory motion. magnetic poles as north and south. Geological poles are south That’s why, following the electromagnetism concept, they will (to earth’s north) and north (to earth’s south). The magnetism have their magnetic poles horizontally or with the directions describes that different poles attract each other. Therefore, to west and east in relation with our concept. Overall this theory of mention the principle of gravitation we can clear ourselves that direction tells that gravitation has its existence maybe because of the connection points of any two objects always face with different opposite pole concept for which all moving objects are balanced directions (poles) because they have attraction. -
(Go's, on the Magic Line .V
Groceries Damaged don't want to begin It wrong, yet 1 Standard by Fire don't know the right," . , "I don't believe much - in saying and Water. things," ; the young farmer remarked ; "my; policy is to do them. And now, are you going to stay - here in this lonely .place much longer? is l 4 It TP snowing and it ia. late." . T suppose I : ought to go," she said doubtfully, "but it Is' so' lovely here in the silence." ' "Look here,"; he said suddenly, "don't you keep your tea things in , . ' that little cupboard? I.. have got tc The New Year begins earliest on OTflrtlir svtia lov lata TTr if go to town, and when I come back the 180th meridian, is part not that at the ieep the sun over you on your I'll brings somethingfor a little, sup--J 21 af the world which lies exactly oppo- voyage, it is apparent that you will j per, "and we can watch. the old year site Greenwich, TV xrA7a- .& (Go's, on the magic line .v. jvui Qliuuug UlUb ALU, J VJ Ul out.. Then I'll take you home in the M If ' ' where day vma-- UL 1 ,:: saltors have to jump a tMMbivua uaj uuif UUICOO jr j sleigh." - either forwards accord- HC!' or backwards, have provided for this by striking out "How good of you." She held out ing as they are sailing with or against an extra day on calendar. you "" "' the If her hand to him. "You havenft ENT the sun. -
A Basic Requirement for Studying the Heavens Is Determining Where In
Abasic requirement for studying the heavens is determining where in the sky things are. To specify sky positions, astronomers have developed several coordinate systems. Each uses a coordinate grid projected on to the celestial sphere, in analogy to the geographic coordinate system used on the surface of the Earth. The coordinate systems differ only in their choice of the fundamental plane, which divides the sky into two equal hemispheres along a great circle (the fundamental plane of the geographic system is the Earth's equator) . Each coordinate system is named for its choice of fundamental plane. The equatorial coordinate system is probably the most widely used celestial coordinate system. It is also the one most closely related to the geographic coordinate system, because they use the same fun damental plane and the same poles. The projection of the Earth's equator onto the celestial sphere is called the celestial equator. Similarly, projecting the geographic poles on to the celest ial sphere defines the north and south celestial poles. However, there is an important difference between the equatorial and geographic coordinate systems: the geographic system is fixed to the Earth; it rotates as the Earth does . The equatorial system is fixed to the stars, so it appears to rotate across the sky with the stars, but of course it's really the Earth rotating under the fixed sky. The latitudinal (latitude-like) angle of the equatorial system is called declination (Dec for short) . It measures the angle of an object above or below the celestial equator. The longitud inal angle is called the right ascension (RA for short). -
How Long Is a Year.Pdf
How Long Is A Year? Dr. Bryan Mendez Space Sciences Laboratory UC Berkeley Keeping Time The basic unit of time is a Day. Different starting points: • Sunrise, • Noon, • Sunset, • Midnight tied to the Sun’s motion. Universal Time uses midnight as the starting point of a day. Length: sunrise to sunrise, sunset to sunset? Day Noon to noon – The seasonal motion of the Sun changes its rise and set times, so sunrise to sunrise would be a variable measure. Noon to noon is far more constant. Noon: time of the Sun’s transit of the meridian Stellarium View and measure a day Day Aday is caused by Earth’s motion: spinning on an axis and orbiting around the Sun. Earth’s spin is very regular (daily variations on the order of a few milliseconds, due to internal rearrangement of Earth’s mass and external gravitational forces primarily from the Moon and Sun). Synodic Day Noon to noon = synodic or solar day (point 1 to 3). This is not the time for one complete spin of Earth (1 to 2). Because Earth also orbits at the same time as it is spinning, it takes a little extra time for the Sun to come back to noon after one complete spin. Because the orbit is elliptical, when Earth is closest to the Sun it is moving faster, and it takes longer to bring the Sun back around to noon. When Earth is farther it moves slower and it takes less time to rotate the Sun back to noon. Mean Solar Day is an average of the amount time it takes to go from noon to noon throughout an orbit = 24 Hours Real solar day varies by up to 30 seconds depending on the time of year.