and rewrite them in the correct manner.
Pero jackson series lives in a world that combines the
13
gets their new uniform today
N
Watch the statements in Column A, with those in Column B.
Column A
Column B
(a) Micrometre
1. One ten-millionth (1/10,000,000) of the distance from the North Pole to the
Equator along the latitude passing through Paris.
A unit which is acceptable to majority of people.
A unit used for measuring very small distances such as diameter of atom.
The distance between two points.
unit used for measuring distance between two cities.
(b) Kilometre
(c) Length
(d) Standard
(e) Metre
8. Fig. 2.14 shows four identical wooden
placed side by side, such that their
JESTIONS
s length? Name four early units of
ment of length.
e need standard units for measurement?
e standard international units of
ent? State the unit of length in this
thickness is 5 cm. Find the thickness of a
rod, correct to two decimal places.
11.0
term metre. Name one multiple and
Answers
Answer:
Tides are the rise and fall of sea levels caused by the combined effects of the gravitational forces exerted by the Moon and the Sun, and the rotation of the Earth.
Simplified schematic of only the lunar portion of Earth's tides, showing (exaggerated) high tides at the sublunar point and its antipode for the hypothetical case of an ocean of constant depth without land. Solar tides not shown.
In Maine (U.S.), low tide occurs roughly at moonrise and high tide with a high Moon, corresponding to the simple gravity model of two tidal bulges; at most places however, the Moon and tides have a phase shift.
File:Tide St. Simons, GA 2018.webmPlay media
Tide coming in, video stops about 1+1⁄2 hours before high tide
Tide tables can be used for any given locale to find the predicted times and amplitude (or "tidal range"). The predictions are influenced by many factors including the alignment of the Sun and Moon, the phase and amplitude of the tide (pattern of tides in the deep ocean), the amphidromic systems of the oceans, and the shape of the coastline and near-shore bathymetry (see Timing). They are however only predictions, the actual time and height of the tide is affected by wind and atmospheric pressure. Many shorelines experience semi-diurnal tides—two nearly equal high and low tides each day. Other locations have a diurnal tide—one high and low tide each day. A "mixed tide"—two uneven magnitude tides a day—is a third regular category.[1][2][a]
Tides vary on timescales ranging from hours to years due to a number of factors, which determine the lunitidal interval. To make accurate records, tide gauges at fixed stations measure water level over time. Gauges ignore variations caused by waves with periods shorter than minutes. These data are compared to the reference (or datum) level usually called mean sea level.[3]
While tides are usually the largest source of short-term sea-level fluctuations, sea levels are also subject to forces such as wind and barometric pressure changes, resulting in storm surges, especially in shallow seas and near coasts.
Tidal phenomena are not limited to the oceans, but can occur in other systems whenever a gravitational field that varies in time and space is present. For example, the shape of the solid part of the Earth is affected slightly by Earth tide, though this is not as easily seen as the water tidal movements.