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The objective of the gravity survey was to identify anomalies having density differences between anomaly and background (Mickus et al. 1991).
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In this formulation the unknown values are the constant concentration values of the anomaly and background, c k a and c k b respectively.
Multiple pieces of evidence support the importance of an increase in precipitation anomalies arising from a nonlinear interaction between unchanged ENSO-driven SST anomalies and background warming.
We will show below that the increase in MMM has contributions from: (i) an increase in the frequency of El Niño and La Niña events; and (ii) an increase in precipitation anomalies arising from a nonlinear interaction between unchanged ENSO-driven SST anomalies and background (global) warming5,24,25,26,27,28.
Standardized anomalies were computed from the ratio between anomalies and the standard deviation for the reference period.
A detailed correlation between anomalies and causes is also established.
The photographer chooses between foreground and background.
5.Use strong contrast between foreground and background.
Connections between anomaly occurrence and geomagnetic perturbations are also discussed.
The relationship between OLR anomaly and precipitation is most reliable in tropical regions.
Fig. 12 Comparison between magnetic anomaly and seismic attenuation structure.
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