Ocean Modeling Discussion

ROMS/TOMS

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PostPosted: Wed May 06, 2015 2:37 am 
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Dear all,

I want to calculate ocean heat content which is defined by temperature. Does anyone know how to convert potential temperature to temperature. Thanks.

Alex


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PostPosted: Wed May 06, 2015 4:33 am 
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Joined: Mon Apr 28, 2003 5:44 pm
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Location: Rutgers University
There is a "seawater" toolbox

in Matlab
http://www.cmar.csiro.au/datacentre/ext ... awater.htm

or Python
https://pypi.python.org/pypi/seawater/

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PostPosted: Wed May 06, 2015 5:07 am 
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Joined: Wed Jan 02, 2008 3:15 pm
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Location: University of Copenhagen
Dear,

You can use the attachment file.

Hope can help you.


Attachments:
sw_temp.m [1.86 KiB]
Downloaded 169 times
File comment: the complementary function,

sw_ptmp: Potential temperature

sw_ptmp.m [3.6 KiB]
Downloaded 177 times
File comment: sw_temp: Temperature from potential temperature
sw_temp.m [1.86 KiB]
Downloaded 186 times
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PostPosted: Thu May 07, 2015 4:48 am 
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Thanks a lot. I will try them. :D


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PostPosted: Fri May 08, 2015 2:19 am 
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wilkin wrote:


Dear Wilkin,

Could I ask another question, why roms use potential temperature instead of temperature? Actually, I am very new to ocean model, I am wondering if the ocean models prefer potential temperature. Thanks.

Alex


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PostPosted: Fri May 08, 2015 3:39 am 
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If you could put seawater in a container that insulates it from exchanging heat with any of the surrounding water, then move it from one depth to another, its temperature will change by virtue of the compression due to pressure. However, its potential temperature would not. That's basically the definition of potential temperature. So this is what we want in an ocean model - the model temperature only changes in response to heat exchange from surface fluxes or mixing with adjacent water of a different temperature. Just moving from one depth to another does nothing.

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PostPosted: Fri May 08, 2015 11:34 am 
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wilkin wrote:
If you could put seawater in a container that insulates it from exchanging heat with any of the surrounding water, then move it from one depth to another, its temperature will change by virtue of the compression due to pressure. However, its potential temperature would not. That's basically the definition of potential temperature. So this is what we want in an ocean model - the model temperature only changes in response to heat exchange from surface fluxes or mixing with adjacent water of a different temperature. Just moving from one depth to another does nothing.



Thanks for your explanation. :D


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