Spring tides occur in principle when the three objects are lined up so that the gravitational forces of the Sun and Moon are combined. In practice in many places the spring tides occur 1-2 days later.
Tides are a proximity effect, which means that the Moon's effect on the tides is the major effect because it's closer, while the Sun's overall gravitational force on the Earth is much stronger.
Tides happen because the Moon's gravity is much stronger on one side of the Earth than the other, because it's close, while the difference is not so much with the Sun's gravity because it's a lot further away.
There are two main types of tide. Spring tides and Neap tides (nothing to do with the time of year!) When the sun and moon are in line with the earth (Sun, Moon then Earth or Sun, Earth then Moon) this gives rises to the highest tides which we call "Spring Tides" When the moon is furthest out of line we get the weakest tides, "Neap Tides"
The Moon effects water and tides with its' gravitational pull. Because of this pull, gravity can change the area and speed of the water in the day and night.
The moon's gravity pulls the tide in and out
Gravitational pull of the sun and the moon may affect the tides. If you notice carefully the tides will be high during a full moon day.
Perpendicular to a line passing through the center of the Earth.
Winds don't blow in a straight line because of the Coriolis effect. Coriolis effect is the deflectiion of all moving particales of matter at Earth's surface to the right in the Northern Hemisphere and to the left in the Southern Hemisphere. This provides evidence for the Earth's rotation. Since the wind is not attach to the Earth, it doestn't move along with the Earth. As a result, the wind curves when it blows from a high to low pressure.
A break in the Earth's surface might be called a chasm, a fissure, or a fault line.
It is a line connecting all points at which there exists an equal vertical distance between the earth's surface and the water table.
Microwave EM radiation travels only in a straight line - line-of-sight/point to point. Bouncing waves off of the ionosphere would accomplish this.
Twice a month. When the moon is directly opposite the sun and when it is in line with the sun in relation to the earth. These are called spring tides.
In a line. Sun, Moon, Earth or Sun, Earth, Moon
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It will be a Solar Eclipse
The tidal ranges differ all over the world depending not only on the alignment of the three bodies you mention but also where on earth, on the shape of the ocean floor, and the amount of water moving. Here in Sweden along the coast the tides due to the Sun and Moon rarely exceed 35mm. The wind and air pressure are a much larger factor causing water to rise and fall well over a meter at times (but nothing to do with the moon...) There are places that daily have over 15 meter of tide and the greatest tides can reach close to 17 meters. See a map of the tidal heights at: http://upload.wikimedia.org/wikipedia/commons/5/5e/M2_tidal_constituent.jpg Around new and full moon when the Sun, Moon and Earth form a line (a condition known as syzygy), the tidal force due to the Sun reinforces that due to the Moon. The tide's range is then at its maximum: this is called the spring tide, or just springs.
It is an imaginary line, passing through 24 Parganas South and North districts, which indicates the northern-most limits of estuarine zone affected by tidal fluctuations. <ref>http://www.sundarbanbiosphere.org/html_files/faq.htm</ref>
Saddly I don't know! I would love to help but I can't.
The tidal ranges differ all over the world depending not only on the alignment of the three bodies you mention but also where on earth, on the shape of the ocean floor, and the amount of water moving. Here in Sweden along the coast the tides due to the Sun and Moon rarely exceed 35mm. The wind and air pressure are a much larger factor causing water to rise and fall well over a meter at times (but nothing to do with the moon...) There are places that daily have over 15 meter of tide and the greatest tides can reach close to 17 meters. See a map of the tidal heights at: http://upload.wikimedia.org/wikipedia/commons/5/5e/M2_tidal_constituent.jpg Around new and full moon when the Sun, Moon and Earth form a line (a condition known as syzygy), the tidal force due to the Sun reinforces that due to the Moon. The tide's range is then at its maximum: this is called the spring tide, or just springs.
The voltage is measured by high and low range. Measurements are referred to as r.m.s. , switching impulses reflected by line to line, earth to line contact.
Moon position, Sun position, seafloor topography, coastal landscape, and water depth. Winds can play a part too.
neap tide A spring tide occurs when the Sun, Moon and Earth are all in a line (full or new moon), and causes the greatest tidal differences because the Sun and Moon act together to create one large tidal bulge
Slant range is the LOS (line of site ) distance between the earth station and the satellite and it is very important in satellite link calculation .For instance to calculate the pathloss slant range would be used.Furthermore slant range is a means to describe the satellite location above the surface of the earth.