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Tracer–tracer relation in the Arctic stratosphere using fuzzy logic Cover

Tracer–tracer relation in the Arctic stratosphere using fuzzy logic

By:   
Open Access
|Jan 2012

Figures & Tables

Fig. 1. 

Scatter plot of O3 versus N2O for the whole data. The scatter shows the shape of a boomerang. The positive and negative correlation in the figure is from the region above and below the ozone maximum.

Fig. 2. 

Scatter plot of O3 against a) altitude, b) longitude, c) latitude and d) day number.

Fig. 3. 

The clusters for the choice of different search radii. The number of clusters obtained is shown within the bracket for each search radius. A search radius of 0.3 is used in the present study.

Fig. 4. 

O3 (in ppbv) observed and predicted for a) training data and b) validation data set.

Table 1. Comparison of the performance the models based on fuzzy and regression techniques. The number of data points used was 23 936 for both training and validation

Fuzzy Linear R2 RMS Norm Slope R2 RMS Norm Slope Training 0.990 274 42 395 1 0.843 1052 137 293 0.71 Validation 0.991 239 37 079 1 0.843 1052 136 971 0.71
Language: English
Page range: 17164 - 17164
Submitted on: Jan 5, 2012
Accepted on: Aug 20, 2012
Published on: Jan 1, 2012
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services

© 2012 K. Satheesan, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.