In this study (Part III), effects of the mechanical and
thermal forcing on the 2007-08 Madden-Julian Oscillation (MJO07-08) system
during the splitting stage over the New Guinea Highlands (NGH) are
investigated. During the splitting stage of MJO07-08 convective system
following the blocking stage highlights the relatively stronger role played by
thermal forcing associated with the NGH, owing to the interaction between
land/sea breeze and the basic flow. Moreover, the mechanical forcing influences
the amount of rainfall along NGH as the weakened mesoscale convective system
(MCS) and incoming flow associated with MJO07-08 interact with the complex
terrain of NGH. This study also explores how the common ingredients and major
mechanisms for heavy rainfall, as identified in the previous studies, are
affected during the splitting of the MCS around NGH. In short, this research
provides in-depth insights into the roles of mechanical and thermal forcing on
the rainfall modification and propagation of MJO07-08 over the NGH. By
employing the Weather and Research Forecasting (WRF) model, the research
uncovers the significance of these factors influencing orographic blocking,
flow regimes, and the NGH modification of the MJO07-08 rainfall.
Author(s) Details
Justin G. Riley
NOAA Cooperative Institute for Great Lakes Research (CIGLR),
Ann Arbor, Michigan, USA.
Yuh-Lang Lin
North Carolina A&T State University, Greensboro, North
Carolina, USA.
Please see the link:- https://doi.org/10.9734/bpi/strufp/v8/1071
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