Difference between revisions of "Nemo"

Revision as of 17:34, 9 November 2007

Welcome to the Bristol Nemo Page!

Here are a few tips and comments based on Bristol's experiences compiling and running NEMO. Hopefully, you will find some useful.

Please take a look the official NEMO webpage before continuing with this page.

Projects using Nemo at Bristol

Mediterranean Sea

Amundsen Sea

Thinning of the Pine Island Glacier, West Antarctica, has been observed during the 1990s. It has been suggested that relatively warm water at the base of the ice shelf has triggered the thinning. The source of and mechanism driving this warm water is unknown.

We are constructing a regional model of the Amunsden Sea using Nemo to investigate ocean circulation close to Pine Island Bay. Input data at the sea surface and at the open boundaries are constructed using output data from the OCCAM global ocean model.

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 ==Welcome to the Bristol Nemo Page!==
-Please take a look the [http://www.lodyc.jussieu.fr/NEMO/ official NEMO webpage].
+Here are a few tips and comments based on Bristol's experiences compiling and running NEMO. Hopefully, you will find some useful.
+Please take a look the [http://www.lodyc.jussieu.fr/NEMO/ official NEMO webpage] before continuing with this page.
+==Projects using Nemo at Bristol==
+===Mediterranean Sea===
+===Amundsen Sea===
+Thinning of the Pine Island Glacier, West Antarctica, has been observed during the 1990s.
+It has been suggested that relatively warm water at the base of the ice shelf has triggered the thinning.
+The source of and mechanism driving this warm water is unknown.
+We are constructing a regional model of the Amunsden Sea using Nemo to investigate ocean circulation close to
+Pine Island Bay.
+Input data at the sea surface and at the open boundaries are constructed using output data from the [http://www.soc.soton.ac.uk/JRD/OCCAM/ OCCAM global ocean model].
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