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A simple estimation of equatorial Pacific response from windstress to untangle Indian Ocean Dipole and Basin influences on El Niño
Atmospheric teleconnections, Linear Continuously Stratified model LCS, El Niño Southern Oscillation ENSO, Equatorial Pacific Ocean dynamics, 0, Convolution to impulse response of a linear system, Indian Ocean Dipole mode IOD and Basin-wide warming/cooling IOB
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