bluewave

Probably a function of the more Niña-like -PDO with the WPAC warm pool. Plus the ongoing drought. So another case of the 500mb ridges becoming stronger more expansive during the 2020s than we have typically seen in the past.

Back to 90s by later this week at the usual warm spots as the below average rainfall and drought continues.

The Nina-like WPAC warm pool forcing in DJF 2015-2016 and 2023-2024 did enhance the warmth in the Northeast those winters above the typical super El Niño winters like 1997-1998 and 1982-1983. While the PDO was positive in 2015-2016, we got the record MJO 5 in December adding to the historic +13 warmth. 2023-2024 had both a -PDO and strong MJO 4-7 activity. So both winters featured record Niña-like MJO activity for super El Niños. But even without the Niña influence in 1997-1998, that winter was still very warm. Plus the winters have warmed since 1997-1998. So perhaps that winter would be just as warm today as 2015-2016 and 2023-2024 was even without the La Niña influence. Since the stronger Southeast trough in 1997-1998 was all Pacific air with the record east based super El Niño. Top 15 warmest winters in NYC Time Series Summary for NY CITY CENTRAL PARK, NY Click column heading to sort ascending, click again to sort descending. 1 2001-2002 41.5 0 2 2022-2023 41.0 0 2015-2016 41.0 Super El Niño Nina Influence 3 2023-2024 40.6 Super El Niño Nina influence 4 2011-2012 40.5 0 5 1931-1932 40.1 0 6 1997-1998 39.6 Super El Niño No Niña influence 7 2016-2017 39.3 0 8 2019-2020 39.2 0 9 1990-1991 39.1 0 10 1998-1999 38.6 0 11 1948-1949 38.5 0 12 1889-1890 38.4 0 13 1952-1953 38.1 0 14 1982-1983 37.9 Super El Niño No Niña influence - 1936-1937 37.9 0 15 1996-1997 37.8 0 - 1932-1933 37.8 0

First time since 1988 here around HVN that the strongest May wind gusts occurred so late in the month. So an unusually strong late May storm system. Very impressive omega block for this time of year.

I think that it could also go beyond the RONI in that the 500 mb ridges are expanding in the mid-latitudes outside the tropical oceans which RONI measures. The 500 mb ridge across the North Pacific from east of Japan to south of the Aleutians has been unprecedented during the 2020s. Also note the slightly weaker mirroring of the pattern in the South Pacific to the east of New Zealand. So it’s been warming the SSTs underneath the ridge causing the -PDO to remain negative. In the old days ,the -PDO was more a function of colder SSTs off of California rather than the extensive warm pool from east of Japan to south of the Aleutians that we have today.

Yeah, we can see the overlapping influences between the El Niño, MJO, and -PDO heading into early June. The ridging showing up south of Alaska into Western Canada is the correlation with the El Nino and +AAM. The extension of the ridge further east across much of the CONUS is more -PDO and MJO 8-1 related for this time of year. So effectively a 500 mb composite in early June that reflects these influences. A coupled El Niño will vary in its sensible weather related to the other influences. Also the pattern in recent years of the 500 mb ridges becoming stronger and more expansive with weaker troughs during any given ENSO state.

Nice way to end the ski season up there.

My guess is that the recent drop was enhanced by the +EPO -PNA pattern in May.

Starting to see the seasonal -PDO drop heading into summer which has been common during the the 2020s.

Looks like that deep low dropping SSE from Canada will produce some strong wind gusts here tomorrow especially eastern sections.

I think the cooler February reference was in regard to long ranger seasonal models like the CanSIPS and EPS monthly which had the cooler stock February El Niño composite for the Mid-Atlantic.

A top 10 warmest spring for many and some areas also top 10 driest.

Shifting back to the over the top warming pattern with temperatures approaching 100° in Montana and cooler to the south.

Yeah, a super El Niño can actually be warmer than expected when overlapping with Niña-like influences. First, the westward lean to the forcing back to MJO 7 probably helped drop the Nino-ridge further south than is typical for El Niño in February. Then the big ridge east of Japan and the strong +WPO along with the EPAC Nino forcing carved out a trough just off the West Coast leading to the -PDO. So the Nino trough typically in the Mid-Atlantic was suppressed out toward Bermuda. Also note the Aleutian Low splitting with a piece over the Bering and just off the West Coast. The one bright spot that month was the record STJ streak near DC and narrow snow band into Central NJ. But it was too narrowly focused to extend much beyond the localized geographic region.

Stations in NJ will finish spring near first place for the most 90 days. Time Series Summary for HARRISON, NJ - Mar through May 90° Days Click column heading to sort ascending, click again to sort descending. 1 2026 7 5 2 2018 6 0 3 2001 5 2 4 2021 4 0 - 2016 4 0 - 2010 4 10 - 2004 4 2 - 2002 4 3 5 2022 3 0 - 2017 3 0 - 2009 3 13 - 2006 3 1 - 2000 3 4 Time Series Summary for NEWARK LIBERTY INTL AP, NJ - Mar through May Click column heading to sort ascending, click again to sort descending. 1 1991 8 0 2 2026 6 5 - 1986 6 0 3 2002 5 0 - 1959 5 0 - 1896 5 0 4 2022 4 0 - 2021 4 0 - 2018 4 0 - 2000 4 0 - 1987 4 0 - 1977 4 0 - 1965 4 0 - 1939 4 0 Time Series Summary for NEW BRUNSWICK 3 SE, NJ - Mar through May Click column heading to sort ascending, click again to sort descending. 1 2026 6 5 2 2016 4 0 - 2010 4 0 - 1976 4 0 3 2021 3 0 - 2017 3 0 - 2012 3 0 - 2009 3 0 - 2002 3 0 - 2001 3 1 - 2000 3 0 Time Series Summary for SOMERSET AIRPORT, NJ - Mar through May Click column heading to sort ascending, click again to sort descending. 1 2026 5 5 2 2021 4 1 3 2022 3 0 - 2017 3 0 - 2012 3 0 - 2009 3 0 - 2002 3 0 - 2000 3 2 Time Series Summary for SUSSEX AIRPORT, NJ - Mar through May Click column heading to sort ascending, click again to sort descending. 1 2026 3 6 - 2022 3 4 2 2023 2 0 - 2018 2 0 - 2013 2 5 - 2009 2 1 - 2002 2 0