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Michael B. Natoli and Eric D. Maloney

cycle and its variability is required in order to benefit forecast skill locally and convective parameterizations. This paper aims to add to the body of work on the variability of the diurnal cycle on intraseasonal time scales. Here, the focus is on the overlooked boreal summer season with a focus on the Philippines and South China Sea. The mean state of the MC diurnal cycle has been studied extensively, primarily focusing on the islands of Sumatra, Borneo, and New Guinea. Houze et al. (1981

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Emily M. Riley Dellaripa, Eric D. Maloney, Benjamin A. Toms, Stephen M. Saleeby, and Susan C. van den Heever

-resolving model (CRM) simulations of an MJO event over New Guinea by Vincent and Lane (2016) also showed increased DCP amplitude over New Guinea land prior to the arrival of MJO active conditions. However, TRMM 3B42 and Climate Prediction Center morphing technique (CMORPH) observations examined by Vincent and Lane (2016) over New Guinea contradicted their modeling results by showing a similar DCP amplitude just prior to and during the most active MJO conditions over the MC. Several papers based on

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