Ocean Cools Southwest of California = Cooler (Less Hot) Pattern Change

Middle Third of September Until A Hurricane?
08/17/2018, 1:34 pm EDT
East Coast Set-up for Eventual Tropical Development
08/21/2018, 11:55 am EDT
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For the first time since 2013 the ocean surface southwest of Baja California has cooled due to up-welling of subsurface cool water by tropical cyclone activity. The cooler regional SSTA correlates to lowering risk of anomalous heat for California.

Discussion: Due to tropical cyclone activity up-welling cooler subsurface water a large area of ocean surface west-southwest of Baja California has cooled the past couple weeks. The cooler SSTA in this region identifies the first cooler-than-normal since late summer 2013. Interestingly, mid-summer was hot in California in 2013 reversing somewhat cooler in AUG/SEP. The cooler ocean surface change was caused by tropical cyclone activity rather than a large-scale climate pattern change so there is questions on how long this cool pattern will last. However, the short-term (next 4 weeks – at least) implications are a climate pattern across California defeating any anomalous heat risk.

Model forecasts from last week indicated one more potential extreme heat event in the Los Angeles basin for MON-WED of this week. The forecast has been revised much cooler. Previously, an amplified ridge pattern northeast of Hurricane Lane was projected to give the Los Angeles area another marginal heat wave. However, Lane is moving more due west and will be another hurricane to enter waters south of Hawaii midweek.

Mega-clusters indicate the favored upper air pattern 1 and 2 weeks from now indicate a transitional pattern from a North-central U.S. trough to ridge (Fig. 1-2). However, the Southwest U.S. and particularly California is not affected by the ridge pattern(s).

Regarding ENSO, a Modoki look has definitely developed. The daily Nino4 SSTA regions which is centered on the Dateline in the equatorial West Pacific is a robust +0.95°C and has warmed 0.58°C in the past 30 days. The Nino3 SSTA region in the eastern equatorial Pacific is right at 0.0°C and has cooled slightly the past 30 days. El Nino Modoki remains a possibility for later 2018.

Fig. 1-2: Mega-clusters preferred upper air patterns on August 24 and August 31 clearly identify California as unaffected.