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. 2011 Feb 22;108(10):4248–4251. doi: 10.1073/pnas.1014107108

Table 1.

Change in length (day of year, days) of ragweed pollen season as a function of latitude for National Allergy Bureau and Aerobiology Research Laboratories sites along a south–north latitudinal gradient

Start
End
Start
End
Location Latitude Years of data 1995 2009 Change
Georgetown, TX 30.63°N 17 198 ± 7 320 ± 7 195 ± 7 313 ± 7 −4 d
Oklahoma City, OK 35.47°N 19 212 ± 7 300 ± 10 227 ± 9 316 ± 15 +1 d
Rogers, AR 36.33°N 15 231 ± 7 295 ± 8 227 ± 6 296 ± 8 −3 d
Papillion, NE 41.15°N 21 212 ± 3 281 ± 6 208 ± 4 288 ± 10 +11 d
Madison, WI 43.00°N 27 208 ± 2 272 ± 4 205 ± 3 281 ± 6 +12 d
LaCrosse, WI 43.80°N 22 213 ± 3 271 ± 3 205 ± 5 276 ± 5 +13 d*
Minneapolis, MN 45.00°N 19 208 ± 5 270 ± 6 206 ± 7 284 ± 7 +16 d*
Fargo, ND 46.88°N 15 216 ± 4 252 ± 8 217 ± 4 269 ± 8 +16 d*
Winnipeg, MB, Canada 50.07°N 16 207 ± 7 264 ± 6 197 ± 7 279 ± 7 +25 d*
Saskatoon, SK, Canada 52.07°N 16 206 ± 12 250 ± 6 197 ± 13 268 ± 7 +27 d*

Years represent the number of years for which pollen data were available. Regression analysis was used to determine the “best-fit” line for all years for a given location. This analysis was then used to determine the start and end day of each year (±95% confidence interval) for the duration of the ragweed pollen season in 1995 and again in 2009.

*Significant increase in the length (days) of the ragweed pollen season.