A trivariate continuous-time random walk state-space model with state-dependent innovation covariance and Milankovitch forcing reconstructs Cenozoic climate proxies via Kalman filter maximum likelihood.
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Continuous-time state space analysis of d18O, d13C, and CO2 in the Cenozoic Era
A trivariate continuous-time random walk state-space model with state-dependent innovation covariance and Milankovitch forcing reconstructs Cenozoic climate proxies via Kalman filter maximum likelihood.