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This summer will be ostensibly cooler than the previous two years; however, overall, still warmer than normal for the vast majority of the country. Global temperatures have cooled slightly in comparison to the past two years, but the base state remains quite warm. ENSO conditions will be preferentially neutral to warm neutral, oscillating near “0” (neutral) throughout the three month meteorological summer. Polar indices are typically poor correlates of surface temperatures in the warm season; with that being said, they can still be utilized to provide clues insofar as the placement of mid-level features. I do not expect protracted anomalous geopotential height patterns this summer; rather, there should be more volatility to the circulation.


Key Teleconnection Expectations

  • Positive (warm phase) Pacific Decadal Oscillation
  • Positive (warm phase) Atlantic Multi-decadal Oscillation
  • Vacillating Arctic Oscillation averaging near neutral
  • Propensity for a positive North Atlantic Oscillation
  • Positive East Pacific Oscillation with ephemeral negative interludes
  • Generally Positive Pacific North American Index
  • ENSO neutral conditions throughout June-July-August
  • Neutral to Positive Global Atmospheric Angular Momentum
  • Analogs utilized generally featured precursor negative / neutral or weak La Nina winters followed by near neutral ENSO conditions for the summer season
  • Primary analog is 2006 with a secondary analog of 2014; there were commonalities with years such as 1958 and 1996, but insufficient to utilize as analogs  



The first half of June will be cooler than average with the mean trough in the Eastern US; this will gradually transition into a near normal to potentially above normal temperature regime for the second half. Thus, June should likely finish near average or slightly below normal in terms of temperatures. As summer progresses, there should be a proclivity for enhanced ridging on both the West and East Coasts of the US, enhanced in part by the warmer sea surface temperatures. The aforementioned teleconnection modalities indicate that higher geopotential heights will preferentially dominate the Western US and near the East Coast, with near or below normal geopotential heights in the Great Lakes. This regime would be propitious for increased precipitation in the OH Valley, and much of the Northeast/Mid-Atlantic. The analogs concur with that notion. Dryness may encompass the areas closer to the Southeast US coast, although, tropical cyclone activity may erase some of the negative precipitation departures later in the summer. The warmer than normal western Atlantic will increase dew points and elevate the overnight minima on the East Coast, particularly in the middle to latter part of the summer. August’s evolution is probably most indeterminate at this juncture, due in large part to ENSO fluctuation uncertainties. A rapid onset to warm ENSO conditions could yield a cooler August than expected, and vice versa. At this point, I am favoring July as the hottest month relative to normal, and subsequently, a near normal or slightly warmer than normal August. If there’s a curveball, I believe it will be that August features more troughiness/coolness over the Northeast.

Meteorological Summer (June-July-August) Temperature Departures for the NY-NJ region: -0.25 to +0.75 [near normal]

Meteorological Summer (June-July-August) Precipitation Departures for the NY-NJ region: wetter than normal [convective nature of summertime precipitation renders any forecast of greater specificity useless].


summer temps


summer precip

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