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The major disadvantage of this method is that although we could extend this algorithm to any dimensional data we only use it for Two dimension applications. Because the computation time of higher dimensional data would be proportional to the number of IMF's of the succeeding dimensions. Hence, it could exceed the computation capacity for a Geo-Physical data processing system when the number of EMD in the algorithm is large. Hence, we have mentioned below faster and better techniques to tackle this disadvantage.
=== Multi-dimensional ensemble empirical mode decomposition
Source:<ref name=":7" /> A Fast and efficient data analysis is very important for large sequences hence the MDEEMD focuses on two important things
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