Wednesday 08/07/2015

Uncertainties of derived surface fluxes are from uncertainties of

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Fig. 1: Multi-annual (1985-2000) mean of divergences (DIV) from four mass corrected DIVs. ERAINT (res) is from the residual method as described by Liu et al . (2015).

NOTE:



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Fig. 2a: DIV differences between datasets shown and ERAINT.
(* before land flux constrain)



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Fig. 2b: As Fig. 2a, but over 2001-2008. ERA40 is missing since I only get the mass corrected DIV over 1985-2000.
(* before land flux constrain)



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Fig. 3a: As Fig. 2a (over 1985-2000), but after land constrain.



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Fig. 3b: As Fig. 3a, but over 2001-2008.



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Fig. 4a: Standard deviation of mean DIVs before land flux constrain.



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Fig. 4b: As Fig. 4a, but after land flux constrain.



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Fig. 5a: Zonal means (1985-2000) over (a) globe, (b) global ocean and (c) global land.
NOTE: this is before land flux constrain.



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Fig. 5b: As Fig. 5a, but over 2001-2008.



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Fig. 5c: As Fig. 5a (over 1985-2000), but after land flux constrain.



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Fig. 5d: As Fig. 5c, but over 2001-2008.



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Fig. 6a: Zonal mean (1985-2000) difference between data sets shown and ERAINT.
NOTE: this is before land flux constrain.



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Fig. 6b: As Fig. 6a, but over 2001-2008.



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Fig. 6c: As Fig. 6a (over 1985-2000), but after land flux constrain.



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Fig. 6d: As Fig. 5c, but over 2001-2008.



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Fig. 7a: Northward transport (PW) over (a) 1985-2000 and (b) 2001-2008 for different datasets.
NOTE: this is before land flux constrain.



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Fig. 7b: As Fig. 7a, but after land flux constrain.



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Fig. 8a: DIV difference between two peroid means (1985-2000 minus 2001-2008).
NOTE: this is before land flux constrain.



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Fig. 8b: As Fig. 8a, but after land flux constrain.



Transport near Equator

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