Remote weather associated with North Pacific subtropical sea-level high properties.

The article offers information on the remote weather related to North Pacific (NP) subtropical sea-level properties. It is mentioned that the variability of climate in NP during summer is dominated by midlatitude events than in South Pacific (SP). The dominant climate in midlatitude is a pattern of weather composites, correlations, and regressions. Lower sea-level pressure (SLP) over central Canada and western tropical Pacific, and higher SLP in east of Japan led to stronger NP high properties. To force or reinforce the NP high, several mechanisms was proposed including suppressed convection.