Analysis of Intraseasonal and Interannual Variability of the Asian Summer Monsoon Using a Hidden Markov Model

• Published in: Journal of climate Vol. 23; no. 20; pp. 5498 - 5516
• Main Authors: Yoo, Jin Ho, Robertson, Andrew W., Kang, In-Sik
• Format: Journal Article
• Language: English
• Published: Boston, MA American Meteorological Society 15.10.2010
• Subjects: Autocorrelation; Earth, ocean, space; El Nino; Exact sciences and technology; External geophysics; Grants; Hydrologic data; Hypothesis testing; Influence; La Nina; Markov chains; Markov models; Meteorology; Monsoons; Oceans; Phase transitions; Precipitation; Probability distribution; Propagation; R&D; Rain; Rainfall; Rainy seasons; Research & development; Southern Oscillation; Statistical methods; Studies; Summer; Transition probabilities; Wind; Asia; rainfall; atmospheric precipitation; Intraseasonal variation; El Nino Southern Oscillation; Summer; Stochastic simulation; Summer monsoon; Interannual variation; Spatial distribution; Seasonal anomaly; El Nino; Southern oscillation; Hidden Markov model; Transition probability; Intraseasonal oscillation; La Nina
• ISSN: 0894-8755; 1520-0442
• DOI: 10.1175/2010JCLI3473.1

Intraseasonal and interannual variability of Asian summer monsoon rainfall in pentad precipitation data is examined using a hidden Markov model (HMM). The spatial patterns of discrete rainfall states derived with the HMM and the associated transition probabilities between the states are shown to represent well the principal Asian summer monsoon intraseasonal oscillation (ISO), propagating eastward and northward with a period of 40–50 days. Stochastic simulations made with the HMM reasonably reproduce the canonical ISO propagation and its observed statistics such as the frequency of ISO events. The interannual modulation of the ISO associated with El Niño–Southern Oscillation (ENSO) is assessed by employing a nonhomogeneous HMM (NHMM) with summer-mean Niño-3.4 index prescribed as an input variable. ENSO influence on the ISO is found to manifest as preferences toward particular ISO phases depending on the ENSO condition, thus adding an asymmetry to the ISO. In the presence of seasonal mean anomalies, it is shown that the El Niño seasonal mean rainfall anomaly pattern is identified by the HMM as a distinct state, in addition to the ISO states, whereas the La Niña seasonal mean rainfall anomaly pattern does not appear distinct from the ISO states.