Friday Map Discussion: 28 September 2007

 

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 Hi Folks,

 

        The focus of Friday map discussion for 28 Sep'07 was on recent 850 hPa/surface temperature relationships in the Northeast and July/August decadal changes

in the 1000-500 hPa thickness for the Northern Hemisphere (NH) relative to earlier decades.

 

        The following links were referenced in support of the discussion:

 

http://www.cdc.noaa.gov (interactive plotting pages)

 

http://www.spc.noaa.gov (forecast tools under research)

 

http://weather.uwyo.edu/upperair/sounding.html (U-WY sounding page)

 

        The following images are attached:

 

1. PowerPoint slides of maximum temperature for 0000 UTC 26 and 27 Sep'07.

 

2. ALB/GYX soundings for 0000 UTC 26 and 27 Sep'07.

 

3. SPC 850 hPa maps for 0000 UTC 26 and 27 Sep'07.

 

4. NH 1000-500 hPa thickness for July-August for (1998-2007)-(1978-1997).

 

5. NH 850 hPa temperature for July-August for (1998-2007)-(1978-1997).

 

.........................

 

        At 00Z/26 850 hPa temperatures reached 19-21 C across eastern New York and southern/central New England. These anomalously warm 850 hPa temperatures were accompanied by clear skies and strong 25-35 kt westerly winds just above the surface. Maximum temperatures reported at 00Z/26 (25th) varied between 29-32 C away from coastal locations that were impacted by a sea breeze. At 00Z/27 850 hPa temperatures cooled by 1-4 C over the region while westerly winds still blew at 20-30 kt and skies remained generally clear. Maximum temperatures increased to 31-34 C.

 

        To help put the 850 hPa temperatures into perspective, Jay Cordeira computed the number of occasions the 850 hPa temperatures reached or exceeded 20 C at

Gray/Portland (GYX/PWM) from 1957 through 31 August 2007. Inspection of the table below shows that in round numbers a 20 C 850 hPa temperature at GYX/PWM occurs on average once or twice per year. Of interest, is that 20.6 C reading at GYX on 00Z/26 breaks the record for the latest occurrence of such hot temperatures at this station by 11 days (previous record occurred on 14 Sep'93).

 

        At issue is why widespread 35+ C maximum temperatures were not observed in eastern New York and southern/central New England on the 25th in the face of record warmth at 850 hPa, a relatively brisk offshore flow and generally clear skies. The 00Z/26-27 GYX/ALB soundings indicate the presence of surface- and near-surface-based inversions beneath near-adiabatic layers. The 12Z/25 GYX/ALB soundings (not shown) indicate that warm air was firmly entrenched at 850 hPa with little evidence for any warm air advection eastward to Atlantic Canada. The 850 hPa temperatures rose during the day by 1-3 C to the values indicated above beneath a strong 500 hPa ridge.

 

        Given that horizontal temperature advection didn't contribute to any additional warming in the 12 h ending 00Z/26, the reported 1-3 C 850 hPa temperature increase could only be from subsidence warming beneath the ridge aloft or an increase in planetary boundary layer (PBL) depth and warming in conjunction with surface sensible heating. The latter can be ruled out because of the observed surface- and near-surface-based inversions at GYX/ALB at 00Z/26, as well as the reported surface maximum temperature, are consistent with a PBL that failed to mix out fully. Was the late September insolation insufficient to achieve full PBL mix-out due to surface sensible heating? And, if so, why did a surface-based mixed layer develop the next day (26th) with higher surface air temperatures (by 1-3 C) despite cooler 850 hPa temperatures (by 4 C at GYX)?

 

Warm season surface-850 hPa temperature relationships under clear skies and offshore low-level wind conditions over the Northeast are supposed to be well understood. Yet, here was a case when expectation (at least by me) was not fully met. At issue is why (perhaps advancing senility is a factor for me?).

 

.........................

 

Occurrences of 850 hPa temperatures of 20.0 C and greater at GYX/PWM from 1957 to 31 Aug'07 (source: Jay Cordeira)

 

- 90 Occurrences of greater than or equal to 20C at 850 hPa throughout the *entire* year. All occurred June-September; ~2 times per year.

 

By decade:

 

1957-1966: 13 (10 unique events)

1967-1976: 14 (7 unique events)

1977-1986: 12 (8 unique events; extreme was 26.0C on 00Z 21 July 1977)

1987-1996: 30 (14 unique events)

1996-2007: 21 (10 unique events)

 

yielding 49 unique events or a return of ~1 event per year.

 

- 6 of those 90 events occurred during the month of September:

 

## -ID-- YYYY MM DD HH   T850  Z850

 -- ----- ---- -- -- --   ----  ----

 1 74389 1958  9  1  0    21.6   1486.

 2 74389 1960  9  9  0    20.7   1564.

 3 74389 1993  9 14 23    20.7   1551.

 4 74389 2001  9  9 23    20.4   1585.

 5 74389 2002  9 10  0    20.4   1547.

 6 74389 2002  9 11  0    20.0   1416.

 7 74389 2007  9 26  0    20.6   1517.

 

...........................

 

        Prompted by record low levels of arctic sea ice, the focus of the last part of map discussion was on the July-August change in 1000-500 hPa thickness and 850 hPa temperature for 1998-2007 versus 1978-1997. The changes are startling. The NH is dominated by 1000-500 hPa thickness increases of 10-30 m and 850 hPa temperature increases of 0.5-1.5 C in the last 10 years as compared to the previous 20 years. Over continental areas warming is especially evident over the northwestern US, northeast Canada, northwestern Europe and to a somewhat lesser extent over northeastern Asia. Over oceanic regions warming is also evident at higher latitudes relative to lower latitudes. A curious feature is the +2 C warming at 850 hPa between Hawaii and California. Whether this warming is indicative of a decrease in oceanic stratocumulus cloud frequency in this region remains to be seen.

 

        The spatial extent and magnitude of the overall NH warming in the last 10 years seems to be too large to be written off as a data analysis problem. Of obvious interest is why the warming "centers of action" are located where they are and to what extent the observed warming has impacted the accelerating melting of sea ice at high latitudes in the NH in the last 10 years. It is also of interest to understand what physical mechanisms govern the smaller patches of observed cooling.

 

                Lance

 

****************

Response from Harald Richter:

 

Mappers,

 

Lance inquired ...

 

At issue is why widespread 35+ C maximum temperatures were not observed in eastern New York and southern/central New England on the 25th in the face of record warmth at 850 hPa, a relatively brisk offshore flow and generally clear skies.  ...... Was the late September insolation insufficient to achieve full PBL mix-out due to surface sensible heating? And, if so, why did a surface-based mixed layer develop the next day (26th) with higher surface air temperatures (by 1-3 C) despite cooler 850 hPa temperatures (by 4 C at GYX)?

 

 .... here was a case when expectation (at least by me) was not fully met. At issue is why (perhaps advancing senility is a factor for me?).

 

While senility is quite a tempting option, I shall mention another wild guess of an explanation from across the seven seas.  The 12z/25 GYX sounding shows comparatively cool low-level temps (the surface sported a mere ~14 C).  Advection aside, BL mixing/insolation probably worked overtime to heat up the lowest 300 hPa column as it did by 00z/26.  Correspondingly, the 12z/26 GYX sounding shows ~23 C at the surface, and a much warmer layer of air above the surface layer (850 temp of ~19 C as opposed to ~16 C 24h earlier).  The increasing GYX low-level humidity might have contributed to this warmth by trapping the ol' LW.  In short, the max. surface temperature on Sep 26 had a healthy headstart.

 

Harald (dreaming of double-digit dewpoints in YMML)