Earth and Sky Flashcards
What defines the locations of its North and South Poles and of its equator, halfway between?
Earth’s rotation
______is the direction toward which Earth rotates, and _____is its opposite.
east, west
We can use what ideas to define a system of coordinates attached to our planet.
the ideas of direction (north south east and west)
A great circle
is any circle on the surface of a sphere whose center is at the center of the sphere.
meridian
a series of great circles that pass through both the North and South Poles. Each of the circles is called a meridian; they are each perpendicular to the equator, crossing it at right angles.
How does one determine their lattitude?
Your latitude (or north-south location) is the number of degrees of arc you are away from the equator along your meridian.
How are lattitude’s measured?
Latitudes are measured either north or south of the equator from 0° to 90°.
N. The latitude of the South Pole
90 degrees
The latitude of the north Pole
90 degrees
Latitude at the equator
(The latitude of the equator is 0°.)
What do astronomers use to denote objects in the sky?
however, astronomers use coordinates called declination and right ascension.
markers in the sky to set up a system of celestial coordinates.
north celestial pole and the south celestial pole. celstial equator
vernal equinox
a point in the sky where the ecliptic (the Sun’s path) crosses the celestial equator.
Right ascension (RA)
is like longitude, except that instead of Greenwich, the arbitrarily chosen point where we start counting is the vernal equinox
How can RA be expressed?
RA can be expressed either in units of angle (degrees) or in units of time.
RA can be expressed either in units of angle (degrees) or in units of time. Why?
This is because the celestial sphere appears to turn around Earth once a day as our planet turns on its axis.
Jean Foucault
provide an unambiguous demonstration of this rotation. In 1851, he suspended a 60-meter pendulum with a mass of about 25 kilograms from the dome of the Pantheon in Paris and started the pendulum swinging evenly. (pendulum prove earth’s rotation)
How did Jean Foucault’s pendulum prove the earth was rotating?
If Earth had not been turning, there would have been no alteration of the pendulum’s plane of oscillation, and so it would have continued tracing the same path. Yet after a few minutes Foucault could see that the pendulum’s plane of motion was turning. Foucault explained that it was not the pendulum that was shifting, but rather Earth that was turning beneath it
Why doesn’t the earth get hotter when it is closer to the sun?
Although Earth’s orbit around the Sun is an ellipse, its distance from the Sun varies by only about 3%. That’s not enough to cause significant variations in the Sun’s heating.
What are seasons caused by?
seasons? As we shall show, the seasons are actually caused by the 23.5° tilt of Earth’s axis.
As Earth travels around the Sun, in which month the Northern Hemisphere “leans into” the Sun and is more directly illuminated.
June
How does the Sun’s favoring one hemisphere translate into making it warmer for us down on the surface of Earth?
There are two effects we need to consider. When we lean into the Sun, sunlight hits us at a more direct angle and is more effective at heating Earth’s surface. The second effect has to do with the length of time the Sun spends above the horizon
Why does direct sunlight make the world more hot
The sunlight isn’t spread out as it would be if it were indirect
the hours of daylight increase in summer and decrease in winter. why?
In the summer months, the northern half of the Earth, where we live, tilts towards the Sun. This means we get more sunlight, making the days longer.
summer solstice
On or about June 21 (the date we who live in the Northern Hemisphere call the summer solstice or sometimes the first day of summer), the Sun shines down most directly upon the Northern Hemisphere of Earth.
Arctic Circle
. As Earth turns on its axis, the North Pole is continuously illuminated by the Sun; all places within 23° of the pole have sunshine for 24 hours. The Sun is as far north on this date as it can get; thus, 90° – 23° (or 67° N) is the southernmost latitude where the Sun can be seen for a full 24-hour period (sometimes called the “land of the midnight Sun”).
winter solstice
first day of winter in the Northern Hemisphere
Halfway between the solstices, where is the sun?
on about March 21 and September 21, the Sun is on the celestial equator. From Earth, it appears above our planet’s equator and favors neither hemisphere. Every place on Earth then receives roughly 12 hours of sunshine and 12 hours of night.
The points where the Sun crosses the celestial equator are called
the vernal (spring) and autumnal (fall) equinoxes.
where are all seasons are much the same?
near the equator
The Sun is north of the celestial equator from about March 21 to September 21, so at the North Pole, the Sun rises when it reaches what?
the vernal equinox
Where does the sun set at the north pole?
sets when it reaches the autumnal equinox.
atmosphere. In reality, however, the atmosphere has the curious effect of allowing us to see a little way “over the horizon.” Why?
because of refraction
refraction
the bending of light passing through air or water
the Sun appears to rise earlier and to set later than it would if no atmosphere were present. Why?
refraction
morning twilight
as beginning when the Sun is 18° below the horizon, and evening twilight extends until the Sun sinks more than 18° below the horizon.
atmospheric effects like refraction require
require small corrections in many of our statements about the seasons.
The measurement of time is based on
the rotation of Earth.
Throughout most of human history, time has been reckoned by
positions of the Sun and stars in the sky.
The most fundamental astronomical unit of time
is the day
solar day
the rotation period of Earth with respect to the Sun,
sidereal day
is defined in terms of the rotation period of Earth with respect to the stars.
Is a solar or sidereal day longer?
solar
A solar day is slightly longer than a sidereal day because:
Earth not only turns but also moves along its path around the Sun in a day. It has to do this because it moves with the respect to the stars and in order to move a little bit more each day it must move 1/364th more than on a normal day (about 4 min)
apparent solar time
as time reckoned by the actual position of the Sun in the sky
local meridian
(the great circle in the sky that passes through our zenith).
before midday (ante meridiem, or a.m.),
before the Sun reaches the local meridian.
p.m. (post meridiem),
after the Sun reaches the local meridian.
Although apparent solar time seems simple, it is not really very convenient to use. Why
use. The exact length of an apparent solar day varies slightly during the year. The eastward progress of the Sun in its annual journey around the sky is not uniform because the speed of Earth varies slightly in its elliptical orbit. Another complication is that Earth’s axis of rotation is not perpendicular to the plane of its revolution. Thus, apparent solar time does not advance at a uniform rate.
After the invention of mechanical clocks that run at a uniform rate, it became necessary to
abandon the apparent solar day as the fundamental unit of time.
mean solar time
is based on the average value of the solar day over the course of the year. A mean solar day contains exactly 24 hours and is what we use in our everyday timekeeping.