MLchartDataset catalogue

Tides

Term · Environment · MLC-T-ENV-028096

1. The rise and fall of ocean waters produced by the gravitational pull of the moon and the sun.

2. The alternate rising and falling of the sea caused by the gravitational attraction of the earth, sun and moon.

3. A variation in the surface level of the oceans caused by the gravitational pull of the moon and sun. Tides fluctuate between high and low twice a day.

4. The periodic rising and falling of the water that results from gravitational attraction of the moon and sun acting upon the rotating earth. Although the accompanying horizontal movement of the water resulting from the same cause is also sometimes called the tide, it is preferable to designate the latter as tidal current, reserving the name tide for the vertical movement.

5. The periodic (occurring at regular intervals) variations in the surface water level of the oceans, bays, gulfs, and inlets. Tides are the result of the gravitiational attraction of the sun and the moon on the earth. The attraction of the moon is far greater than the attraction of the sun due to the close proximity of the earth and the moon. The sun is 360 times further from the earth than the moon. Therefore, the moon plays a larger role than the sun in producing tides. Every 27.3 days, the earth and the moon revolve around a common point. This means that the oceans and other water bodies which are affected by the earth-moon system experience a new tidal cycle every 27.3 days. Because of the physical processes which occur to produce the tidal system, there are two high tides and two low tides each day. Because of the angle of the moon with respect to the earth, the two high tides each day do not have to be of equal height. The same holds true for the two low tides each day. Tides also differ in height on a daily basis. The daily differences between tidal heights is due to the changing distance between the earth and the moon. Scientists use measurements of the height of the water level to examine tides and the various phenomena which influence tides, such as hurricanes and winter storms.

6. Alternate rising and falling of the sea caused by the gravitational attraction of the earth, sun and moon.

Table 1. Record
IdentifierMLC-T-ENV-028096
FieldEnvironment
SubjectEcosystems
ReferencesEstuaries Glossary; Chesapeake Bay Glossary; Student's Guide to Global Climate Change; NOAA Coastal Services Center Glossary of Coastal Terminology; NOAA National Weather Service Glossary
Record as JSON
{
  "id": "MLC-T-ENV-028096",
  "term": "Tides",
  "field": "Environment",
  "definition": "1. The rise and fall of ocean waters produced by the gravitational pull of the moon and the sun.\n\n2. The alternate rising and falling of the sea caused by the gravitational attraction of the earth, sun and moon.\n\n3. A variation in the surface level of the oceans caused by the gravitational pull of the moon and sun. Tides fluctuate between high and low twice a day.\n\n4. The periodic rising and falling of the water that results from gravitational attraction of the moon and sun acting upon the rotating earth. Although the accompanying horizontal movement of the water resulting from the same cause is also sometimes called the tide, it is preferable to designate the latter as tidal current, reserving the name tide for the vertical movement.\n\n5. The periodic (occurring at regular intervals) variations in the surface water level of the oceans, bays, gulfs, and inlets. Tides are the result of the gravitiational attraction of the sun and the moon on the earth. The attraction of the moon is far greater than the attraction of the sun due to the close proximity of the earth and the moon. The sun is 360 times further from the earth than the moon. Therefore, the moon plays a larger role than the sun in producing tides. Every 27.3 days, the earth and the moon revolve around a common point. This means that the oceans and other water bodies which are affected by the earth-moon system experience a new tidal cycle every 27.3 days. Because of the physical processes which occur to produce the tidal system, there are two high tides and two low tides each day. Because of the angle of the moon with respect to the earth, the two high tides each day do not have to be of equal height. The same holds true for the two low tides each day. Tides also differ in height on a daily basis. The daily differences between tidal heights is due to the changing distance between the earth and the moon. Scientists use measurements of the height of the water level to examine tides and the various phenomena which influence tides, such as hurricanes and winter storms.\n\n6. Alternate rising and falling of the sea caused by the gravitational attraction of the earth, sun and moon.",
  "subject": "Ecosystems",
  "references": [
    "Estuaries Glossary",
    "Chesapeake Bay Glossary",
    "Student's Guide to Global Climate Change",
    "NOAA Coastal Services Center Glossary of Coastal Terminology",
    "NOAA National Weather Service Glossary"
  ],
  "url": "https://mlchart.com/terminology/environment/tides/"
}

Record 28,096 of 30,736 in Environment terminology (MLC-0121). Request the full dataset.