0000003078 00000 n 949 44 0000007345 00000 n h. Discuss how these factors could play an important role in the management of aquaculture systems. 0000006230 00000 n The average salinity of seawater is S = 35 which means that SW is 3.5% salt and 96.5% H2O by weight.
$E}k���yh�y�Rm��333��������:� }�=#�v����ʉe 0000003507 00000 n 0000021165 00000 n salinity, and the temperature decreases greatly with depth, but the salinity does not.
0000001554 00000 n 0000004227 00000 n it is impossible to define a simple relationship between salinity and the decrease in evaporation. Why is salinity important? 0000008819 00000 n <> 0000005032 00000 n 0000004844 00000 n Finally, the article discusses why salinity is a problem and the effect of global warming on ocean salinity. 0000069648 00000 n $O./� �'�z8�W�Gб� x�� 0Y驾A��@$/7z�� ���H��e��O���OҬT� �_��lN:K��"N����3"��$�F��/JP�rb�[䥟}�Q��d[��S��l1��x{��#b�G�\N��o�X3I���[ql2�� �$�8�x����t�r p��/8�p��C���f�q��.K�njm͠{r2�8��?�����. ��3�������R� `̊j��[�~ :� w���!
0000001719 00000 n 0000003257 00000 n endobj 0000008101 00000 n 949 0 obj <> endobj trailer <>startxref 0 %%EOF 226 0 obj <>]/Pages 186 0 R/Type /Catalog/Version /1.4/ViewerPreferences <>>> endobj 240 0 obj <> stream 0000000016 00000 n trailer 0000140668 00000 n 0000141228 00000 n 0000002084 00000 n <>/XObject<>/ProcSet[/PDF/Text/ImageB/ImageC/ImageI] >>/MediaBox[ 0 0 612 792] /Contents 4 0 R/Group<>/Tabs/S/StructParents 0>> Absolute salinity is both more accurate and more precise than practical salinity and can be used to estimate salinity not only across the ocean, but at greater depths and temperature ranges 24. xڝ�wTT��Ͻwz��0�z�.0��. The definition of salinity of the ocean is also explained. 0000001199 00000 n 4 0 obj 0000021964 00000 n TEOS-10 is derived from a Gibbs function, which requires more complex … f. Graph your data as salinity vs. DO and temperature vs. DO. 0000002046 00000 n �}�,b�� 0000008276 00000 n 0000005279 00000 n
Estuaries can have varying salinity levels throughout their length and can range from 0.5-30 …
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Salinity, along with temperature, determines the density of seawater, and hence its vertical flow patterns in thermohaline circulation. ;�� q�GT�!��e�D��:��r����G��؟:��LA�&�gd�8q�T���_�J{��!닌3ǽ���"�y��ϑ��=3��0됚-��{įBlHYFV�,��������J��'���C���q4xt?���G5����D*x�9����d�:\|�@��5��+S�.��f@o�[X/Ny撤�m�aD�ג��4������jY����wh�QX�|��,:P��C��Z{���Z�rIO�� ���=�z��5�c 0000010247 00000 n endobj
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