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In order to determine the interobserver concordance, a frequently used statistical tool is available: the kappa coefficient (k).

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On the contrary, a value of k = 0 reflects that the observed concordance is precisely the one that is expected by chance.

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The present article explains the theoretical background of this coefficient, the methodology employed for its calculation and the way in which its value is correctly interpreted.

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Through climate services, basic climate information and data are transformed into products and specific climatic applications useful for various sectors' users.


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