Tidal Characteristic Numbers of Temperature: Difference between revisions
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====Advective Flood Transport of Heat==== | ====Advective Flood Transport of Heat==== | ||
amount of heat, which is transported by means of flood current through a cross section | amount of heat, which is transported by means of flood current through a cross section<br /> | ||
Example: not available. | Example: not available. | ||
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====Advective Ebb Transport of Heat==== | ====Advective Ebb Transport of Heat==== | ||
Amount of heat, which is transported by means of ebb current through a cross section | Amount of heat, which is transported by means of ebb current through a cross section<br /> | ||
Example: not available. | Example: not available. | ||
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====Maximum Temperature==== | ====Maximum Temperature==== | ||
Maximum value of temperature during a complete tidal cycle (period between two subsequent slack water times of ebb current) | Maximum value of temperature during a complete tidal cycle (period between two subsequent slack water times of ebb current)<br /> | ||
Example: not available. | Example: not available. | ||
====Minimum Temperature==== | ====Minimum Temperature==== | ||
Minimum value of temperature during a complete tidal cycle (period between two subsequent slack water times of ebb current) | Minimum value of temperature during a complete tidal cycle (period between two subsequent slack water times of ebb current)<br /> | ||
Example: not available. | Example: not available. | ||
====Mean Temperature==== | ====Mean Temperature==== | ||
Average value of temperature during a complete tidal cycle (period between two subsequent slack water times of ebb current) | Average value of temperature during a complete tidal cycle (period between two subsequent slack water times of ebb current)<br /> | ||
Example: not available. | Example: not available. | ||
====Tidal Variation of Temperature==== | ====Tidal Variation of Temperature==== | ||
Difference between the extreme values of temperature during a complete tidal cycle (period between two subsequent slack water times of ebb current) | Difference between the extreme values of temperature during a complete tidal cycle (period between two subsequent slack water times of ebb current)<br /> | ||
Example: not available. | Example: not available. | ||
====Advective Residual Transport of Heat==== | ====Advective Residual Transport of Heat==== | ||
Residual amount of heat which is transported by means of ebb and flood currents through a cross section (the different transport directions are taken into account). If the advective transport by means of flood current is equal but in opposite direction of the ebb current transport this will result in a zero advective residual transport of heat. | Residual amount of heat which is transported by means of ebb and flood currents through a cross section (the different transport directions are taken into account). If the advective transport by means of flood current is equal but in opposite direction of the ebb current transport this will result in a zero advective residual transport of heat.<br /> | ||
Example: not available. | Example: not available. | ||
====Advective Temperature, Flood-Ebb-Ratio==== | ====Advective Temperature, Flood-Ebb-Ratio==== | ||
Flood to ebb ratio for the amounts of heat which are transported by means of flood and ebb currents | Flood to ebb ratio for the amounts of heat which are transported by means of flood and ebb currents<br /> | ||
Example: not available. | Example: not available. | ||
Revision as of 11:03, 9 June 2010
graphical representations of the characteristic numbers of salinity
Motivation
The calculation as well as the graphic visualization of various tidal characteristic numbers of temperature and also for the advective transport of heat contributes to an improved understanding of tidally dominated transport processes in estuaries. Spatial variations of temperature, advective transport of heat by means of flood and ebb currents can be highlighted for areas like coastal seas and estuaries as well.
- As the calculations are performed separately for the durations of ebb- and flood-current it can be shown that transport paths can differ significantly for the two tidal phases. From this one can get additional insight with respect to the relevant transport mechanisms dominated by the tidal currents. This can be related to locally varying flood-ebb asymmetries for ebb volume and flood volume. Also the presence of horizontal gradients can contribute to this effect.
- The variation of temperature resulting from the local maximum as well as the local minimum of temperature can be quite large. This is a consequence of the different temperature of e.g. sea and fresh water. The value for the local temperature variation is mainly the result of the product between the horizontal temperature gradient and the lagrangian drift of a water particle during a complete tidal cycle.
An automatic analysis of all tidal characteristic numbers of temperature is carried through by the computer program TDKSF.
Definitions for the Tidal Characteristic Numbers of Temperature
Flood Current
Advective Flood Transport of Heat
amount of heat, which is transported by means of flood current through a cross section
Example: not available.
Ebb Current
Advective Ebb Transport of Heat
Amount of heat, which is transported by means of ebb current through a cross section
Example: not available.
Tidal Cycle
Maximum Temperature
Maximum value of temperature during a complete tidal cycle (period between two subsequent slack water times of ebb current)
Example: not available.
Minimum Temperature
Minimum value of temperature during a complete tidal cycle (period between two subsequent slack water times of ebb current)
Example: not available.
Mean Temperature
Average value of temperature during a complete tidal cycle (period between two subsequent slack water times of ebb current)
Example: not available.
Tidal Variation of Temperature
Difference between the extreme values of temperature during a complete tidal cycle (period between two subsequent slack water times of ebb current)
Example: not available.
Advective Residual Transport of Heat
Residual amount of heat which is transported by means of ebb and flood currents through a cross section (the different transport directions are taken into account). If the advective transport by means of flood current is equal but in opposite direction of the ebb current transport this will result in a zero advective residual transport of heat.
Example: not available.
Advective Temperature, Flood-Ebb-Ratio
Flood to ebb ratio for the amounts of heat which are transported by means of flood and ebb currents
Example: not available.
back to Analysis of Calculated Results