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* The variation of salinity resulting from the local maximum as well as the local minimum of salinity can be quite large. This is a consequence of fresh water inflow into an estuary. The value for the local salinity variation is mainly the result of the product between the horizontal salinity gradient and the lagrangian drift of a water particle during a complete tidal cycle. Due to the fact that salt is mainly advectively transported by means of the tidal current. The water particles which are passing at a location during a complete tidal cycle do have different regions of origin. Therefore they can also show substantial differences in salinity because estuaries are regions where fresh and sea water is mixed. For organisms which are living at the seabed and which cannot move the tidal variation of salinity is one of the significant natural stress factors (variation of the osmotic pressure due to salinity variations).
* The variation of salinity resulting from the local maximum as well as the local minimum of salinity can be quite large. This is a consequence of fresh water inflow into an estuary. The value for the local salinity variation is mainly the result of the product between the horizontal salinity gradient and the lagrangian drift of a water particle during a complete tidal cycle. Due to the fact that salt is mainly advectively transported by means of the tidal current. The water particles which are passing at a location during a complete tidal cycle do have different regions of origin. Therefore they can also show substantial differences in salinity because estuaries are regions where fresh and sea water is mixed. For organisms which are living at the seabed and which cannot move the tidal variation of salinity is one of the significant natural stress factors (variation of the osmotic pressure due to salinity variations).


'''An automatic analysis of all tidal characteristic numbers of salinity is carried through by the computer program [[TDKSF]].  
'''Automatic analyses for all of the above mentioned tidal characteristic numbers of salinity are carried out for 2D- as well as for 3D-data by the programs [[TDKSF]] and [[NCANALYSE]].'''
'''


==Definitions for the Tidal Characteristic Numbers of Salinity==
==Definitions for the Tidal Characteristic Numbers of Salinity==
===Flood Current===
===Flood Current===
====Advective Flood Transport of Salt====
====Advective Flood Transport of Salt====
salt volume, which is transported by means of flood current through a cross section
salt volume, which is transported by means of flood current through a cross section.<br />
[[Example: Advective Flood Transport of Salt in the Inner Außenweser]]. <br />
Data analysis: [[TDKSF]].
 
====Mean Salinity Flood Current====
Mean value of salinity during the flood current duration of a tide.<br />
[[Example figures: mean salinity flood current]]. <br />
Data analysis: [[NCANALYSE]].


[[Example: Advective Flood Transport of Salt in the Inner Außenweser]]
===Ebb Current===
===Ebb Current===
====Advective Ebb Transport of Salt====
====Advective Ebb Transport of Salt====
salt volume, which is transported by means of ebb current through a cross section  
salt volume, which is transported by means of ebb current through a cross section.<br />
[[Example: Advective Ebb Transport of Salt in the Inner Außenweser]]. <br />
Data analysis: [[TDKSF]].
 
====Mean Salinity Ebb Current====
Mean value of salinity during the ebb current duration of a tide.<br />
[[Example figures: mean salinity ebb current]]. <br />
Data analysis: [[NCANALYSE]].


[[Example: Advective Ebb Transport of Salt in the Inner Außenweser]]
===Tidal Cycle===
===Tidal Cycle===
====Maximum Salinity====
====Maximum Salinity====
maximum value of salinity during a complete tidal cycle (period between two subsequent slack water times of ebb current)  
maximum value of salinity during a complete tidal cycle (period between two subsequent slack water times of ebb current).<br />
[[Example figures: maximum salinity]]. <br />
Data analysis: [[TDKSF]] and [[NCANALYSE]].


[[Example: Maximum Salinity in the Inner Außenweser]]
====Minimum Salinity====
====Minimum Salinity====
minimum value of salinity during a complete tidal cycle (period between two subsequent slack water times of ebb current)  
minimum value of salinity during a complete tidal cycle (period between two subsequent slack water times of ebb current).<br />
[[Example figures: minimum salinity]]. <br />
Data analysis: [[TDKSF]] and [[NCANALYSE]].


[[Example: Minimum Salinity in the Inner Außenweser]]
====Mean Salinity====
====Mean Salinity====
average value of salinity during a complete tidal cycle (period between two subsequent slack water times of ebb current)
average value of salinity during a complete tidal cycle (period between two subsequent slack water times of ebb current).<br />
[[Example figures: mean salinity]]. <br />
Data analysis: [[TDKSF]] and [[NCANALYSE]].


[[Example: Mean Salinity in the Inner Außenweser]]
====Tidal Variation of Salinity====
====Tidal Variation of Salinity====
difference between the extreme values of salinity during a complete tidal cycle (period between two subsequent slack water times of ebb current)  
difference between the extreme values of salinity during a complete tidal cycle (period between two subsequent slack water times of ebb current).<br />
[[Example figures: tidal variation of salinity]]. <br />
Data analysis: [[TDKSF]] and [[NCANALYSE]].


[[Example: Tidal Variation of Salinity in the Inner Außenweser]]
====Advective Residual Transport of Salt====
====Advective Residual Transport of Salt====
residual salt volume 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 salt.  
residual salt volume 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 salt.<br />
[[Example: Advective Residual Transport of Salt in the Inner Außenweser]]. <br />
Data analysis: [[TDKSF]].


[[Example: Advective Residual Transport of Salt in the Inner Außenweser]]
====Advective Salt Transport, Flood-Ebb-Ratio====
====Advective Salt Transport, Flood-Ebb-Ratio====
flood to ebb ratio for the salt volumes which are transported by means of flood and ebb currents
flood to ebb ratio for the salt volumes which are transported by means of flood and ebb currents.<br />
[[Example: Flood-Ebb-Ratio for the Advective Salt Transport in the Inner Außenweser]]. <br />
Data analysis: [[TDKSF]].
 
====Mean Salinity Flood Current : Mean Salinity====
Ratio of mean salinity of flood current to mean salinity during the complete tide.<br />
[[Example figures: mean salinity flood current : mean salinity]]. <br />
Data analysis: [[NCANALYSE]].
 
====Mean Salinity Ebb Current : Mean Salinity====
Ratio of mean salinity of ebb current to mean salinity during the complete tide.<br />
[[Example figures: mean salinity ebb current : mean salinity]]. <br />
Data analysis: [[NCANALYSE]].
 
====Mean Salinity Flood Current : Mean Salinity Ebb Current====
Ratio of mean salinity of flood current to mean salinity of ebb current.<br />
[[Example figures: mean salinity flood current : mean salinity ebb current]]. <br />
Data analysis: [[NCANALYSE]].
 
====Tidal Variation of Salinity : Mean Salinity====
Ratio of tidal variation of salinity to mean salinity value of the tide.<br />
[[Example figures: tidal variation of salinity : mean salinity]]. <br />
Data analysis: [[NCANALYSE]].
 
====Maximum Salinity : Mean Salinity====
Ratio of maximum salinity of the tide to mean salinity value of the tide.<br />
[[Example figures: maximum salinity : mean salinity]]. <br />
Data analysis: [[NCANALYSE]].
 
====Minimum Salinity : Mean Salinity====
Ratio of minimum salinity of the tide to mean salinity value of the tide.<br />
[[Example figures: minimum salinity : mean salinity]]. <br />
Data analysis: [[NCANALYSE]].
 


[[Example: Flood-Ebb-Ratio for the Advective Salt Transport in the Inner Außenweser]]
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back to [[Analysis of Calculated Results]]
back to [[Analysis of Calculated Results]]
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[[Overview]]
[[Overview]]

Revision as of 10:29, 25 November 2014

Graphical representation of characteristic numbers of salinity (with German text only). This graphical representation is also available in Encapsulated PostScript format.

Graphical representation of characteristic numbers of advective salt transport (with German text only). This graphical representation is also available in Encapsulated PostScript format.

Motivation

The calculation as well as the graphic visualization of various tidal characteristic numbers of salinity and also for the advective transport of salt contributes to an improved understanding of tidally dominated transport processes in estuaries. Spatial variations of salinity, advective transport of salt by means of flood and ebb currents can be highlighted for areas like coastal seas and estuaries as well (see also animation of tidal variability of salinity in the Außenweser Estuary).

  • 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 salinity resulting from the local maximum as well as the local minimum of salinity can be quite large. This is a consequence of fresh water inflow into an estuary. The value for the local salinity variation is mainly the result of the product between the horizontal salinity gradient and the lagrangian drift of a water particle during a complete tidal cycle. Due to the fact that salt is mainly advectively transported by means of the tidal current. The water particles which are passing at a location during a complete tidal cycle do have different regions of origin. Therefore they can also show substantial differences in salinity because estuaries are regions where fresh and sea water is mixed. For organisms which are living at the seabed and which cannot move the tidal variation of salinity is one of the significant natural stress factors (variation of the osmotic pressure due to salinity variations).

Automatic analyses for all of the above mentioned tidal characteristic numbers of salinity are carried out for 2D- as well as for 3D-data by the programs TDKSF and NCANALYSE.

Definitions for the Tidal Characteristic Numbers of Salinity

Flood Current

Advective Flood Transport of Salt

salt volume, which is transported by means of flood current through a cross section.
Example: Advective Flood Transport of Salt in the Inner Außenweser.
Data analysis: TDKSF.

Mean Salinity Flood Current

Mean value of salinity during the flood current duration of a tide.
Example figures: mean salinity flood current.
Data analysis: NCANALYSE.

Ebb Current

Advective Ebb Transport of Salt

salt volume, which is transported by means of ebb current through a cross section.
Example: Advective Ebb Transport of Salt in the Inner Außenweser.
Data analysis: TDKSF.

Mean Salinity Ebb Current

Mean value of salinity during the ebb current duration of a tide.
Example figures: mean salinity ebb current.
Data analysis: NCANALYSE.

Tidal Cycle

Maximum Salinity

maximum value of salinity during a complete tidal cycle (period between two subsequent slack water times of ebb current).
Example figures: maximum salinity.
Data analysis: TDKSF and NCANALYSE.

Minimum Salinity

minimum value of salinity during a complete tidal cycle (period between two subsequent slack water times of ebb current).
Example figures: minimum salinity.
Data analysis: TDKSF and NCANALYSE.

Mean Salinity

average value of salinity during a complete tidal cycle (period between two subsequent slack water times of ebb current).
Example figures: mean salinity.
Data analysis: TDKSF and NCANALYSE.

Tidal Variation of Salinity

difference between the extreme values of salinity during a complete tidal cycle (period between two subsequent slack water times of ebb current).
Example figures: tidal variation of salinity.
Data analysis: TDKSF and NCANALYSE.

Advective Residual Transport of Salt

residual salt volume 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 salt.
Example: Advective Residual Transport of Salt in the Inner Außenweser.
Data analysis: TDKSF.

Advective Salt Transport, Flood-Ebb-Ratio

flood to ebb ratio for the salt volumes which are transported by means of flood and ebb currents.
Example: Flood-Ebb-Ratio for the Advective Salt Transport in the Inner Außenweser.
Data analysis: TDKSF.

Mean Salinity Flood Current : Mean Salinity

Ratio of mean salinity of flood current to mean salinity during the complete tide.
Example figures: mean salinity flood current : mean salinity.
Data analysis: NCANALYSE.

Mean Salinity Ebb Current : Mean Salinity

Ratio of mean salinity of ebb current to mean salinity during the complete tide.
Example figures: mean salinity ebb current : mean salinity.
Data analysis: NCANALYSE.

Mean Salinity Flood Current : Mean Salinity Ebb Current

Ratio of mean salinity of flood current to mean salinity of ebb current.
Example figures: mean salinity flood current : mean salinity ebb current.
Data analysis: NCANALYSE.

Tidal Variation of Salinity : Mean Salinity

Ratio of tidal variation of salinity to mean salinity value of the tide.
Example figures: tidal variation of salinity : mean salinity.
Data analysis: NCANALYSE.

Maximum Salinity : Mean Salinity

Ratio of maximum salinity of the tide to mean salinity value of the tide.
Example figures: maximum salinity : mean salinity.
Data analysis: NCANALYSE.

Minimum Salinity : Mean Salinity

Ratio of minimum salinity of the tide to mean salinity value of the tide.
Example figures: minimum salinity : mean salinity.
Data analysis: NCANALYSE.



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Overview