Fiskdale, MA EF0 Tornado of June 1, 2011

Below is a detailed event summary by NOAA’s National Centers for Environmental Information (2019).

Figure 1. Surface analysis at 21Z on June 1, 2011 showing geopotential height contours, surface observations, fronts and pressure centres (WPC, 2017, modified by Francis Lavigne-Theriault, 2019)

An upper level closed low over southern Ontario tracked across Quebec while at the surface, a cold front over western New York crossed southern New England in the evening of June 1. An environment characterized by high CAPE (2000-3000 J/kg) and high shear (greater than 200 m2/s2) was in place across western Massachusetts. In addition, mid level lapse rates were an impressive 7 to 8 C/km (Figure 7).

Figure 2. 500mb closed low (DelliCarpini, J., n.d.).

Thunderstorms forming ahead of the front organized into discrete supercells in an environment highly favorable for tornado formation. While convection fired early in the day along a weak low level theta-e ridge across north central Massachusetts and southern New Hampshire (Figure 3), clearing allowed for rapid destabilization in the afternoon.

Figure 3. Satellite and surface observations at 16 UTC (noon loal time) (DelliCarpini, J., n.d.).

Thunderstorms developed during the morning ahead of the cold front from eastern Pennsylvania into southeast New York and Vermont. By about 3 pm, the storms entered western Massachusetts and were in the form of discrete supercells (Figure 4).

Figure 4. Doppler radar base reflectivity at 2:50 pm EDT on June 1, 2011 (Source: Meteologix).

By 4 pm, several supercells had developed across southern Vermont, southwest New Hampshire, and western Massachusetts. At that time, the supercell which eventually produced the most significant tornado entered Hampden County from the Berkshires (Figure 5 & 6). This cell produced what was evaluated to be an EF-3 tornado touching down in Westfield and continuing on a 38 mile long trek through West Springfield, Springfield, Wilbraham, Monson, Brimfield, and Sturbridge. This tornado was on the ground for an estimated 70 minutes.

About two hours later, another supercell tracked just to the north of the storm track of the EF3 tornado. While its rotation was not as strong, it produced brief tornadoes in Wilbraham (EF1), North Brimfield (EF1), and Sturbridge (EF0). While the focus was certainly on the tornadoes and their damage, damaging winds, large hail up to two inches in diameter, and some flash flooding also occurred across southern New England.

Figure 7. Storm Prediction Center mesoanalysis at 19 UTC (3:00 pm EDT) (DelliCarpini, J., n.d.).


The Fiskdale, MA EF0 tornado of June 1, 2011 impacted Worcester County in Massachusetts. According to NOAA (2019), the EF0 tornado caused no fatalities, injuries or property damage. The tornado touched down in Worcester County four miles northwest of Fiskdale at 7:10 pm EDT and travelled 1.42 miles to lift just west-southwest of Glen Grove. This EF0 had a maximum width of 25 yards.


NOAA National Centers for Environmental Information (2019). Storm Events Database. Retrieved from:

DelliCarpini, J. (n.d.). The Massachusetts Tornado Outbreak of June 1, 2011 [PDF]. Retrieved from

NWS Weather Prediction Center Surface Analysis Archive. (2017). Surface analysis 21Z Wed Jun 1 2011. Retrieved from:

National Centers for Environmental Information reports:

A third tornado touched down briefly from the same thunderstorm that produced the north Wilbraham and north Brimfield tornadoes. This tornado touched down in Wells State Park and then continued on across Walker Pond Road and Podunk Road, lifting up just west of Route 49. Damage was generally limited to downed trees, but one of these fell onto a house on Walker Pond Road. All associated property damage estimates are included in the EF3 tornado that occurred in Hampden and Worcester Counties.