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A multiple length scale correlation operator for ocean data assimilation Cover

A multiple length scale correlation operator for ocean data assimilation

Open Access
|Dec 2016

Figures & Tables

Fig. 1

2D correlation functions f2,2=γ1c2,1+γ2c2,2where the length scale parameters are L 1=10 and L 2=50 for c 2,1 and c 2,2, respectively, and ν 1=ν 2=3. The left panel shows a cross-section of c 2,1 (dashed black), c 2,2 (dotted black) and two different linearly combined functions: f 2,2 with γ1=0.7,γ2=0.3 (red), and f2,2with γ1=0.3,γ2=0.7 (blue). The right panel shows a cross-section at xˆ2=0 of their normalised spectrum. The black lines highlight the normalised spectrum values (2M+2-d)M/(2M+2)M=0.41 and 1/2M=0.0625. See text for details.

Fig. 2

Evolution of the ratio k/k 1 with respect to γ1. k is the kurtosis of the 2D correlation function f2,2=γ1c2,1+γ2c2,2, with L 1=10 and L 2=50 for c 2,1 and c 2,2, respectively, and ν 1=ν 2=3. k 1 is the kurtosis of the function c 2,1 (and c 2,2).

Fig. 3

Surface temperature increments on 1 December 2010 with the original formulation (top left panel) and a combination of two functions (top right panel) for the Gulf Stream region. The increments are calculated from the same initial states and the same set of observations. The factor γ2 defining the amount of the large scale to be used in the combination is shown on the bottom panel.

Table 1. RMSE for SNGL and DUAL in different areas

RMSE
VariableAreaSNGLDUAL%
SST in situGlobal0.4550.462+1.5North Atlantic0.5160.527+2.1Southern Ocean0.4680.484+3.4Temperature profileGlobal0.6140.616+0.3North Atlantic0.8120.806−0.7Southern Ocean0.5680.565−0.5Salinity profileGlobal0.1260.124−1.6North Atlantic0.2180.214−1.8Southern Ocean0.1080.103−4.6Mixed layer depthGlobal40.3537.08−8.1North Atlantic44.1342.94−2.7Southern Ocean63.7656.44−11.5SSHGlobal0.0710.075+5.6North Atlantic0.0750.074−1.3Southern Ocean0.0890.097+9.0

[i] The last column represents the normalised difference (DUAL–SNGL)/SNGL in percentage.

Fig. 4

Hovmoller plots of the observation minus background innovation mean for temperature profiles for SNGL (left panel) and DUAL (right panel) in Southern Ocean. Blue colours denote a warm model bias, whereas red colours represent a cold model bias.

Fig. 5

Hovmoller plots of the observation minus background innovation mean for salinity profiles for SNGL (left panel) and DUAL (right panel) in Southern Ocean. Blue colours denote a salty model bias, whereas red colours represent a fresh model bias.

Language: English
Page range: 29744 - 29744
Submitted on: Sep 13, 2015
Accepted on: Feb 2, 2016
Published on: Dec 1, 2016
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services

© 2016 Isabelle Mirouze, Edward W. Blockley, Daniel J. Lea, Matthew J. Martin, Michael J. Bell, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.