Wh. Klein et al., VERIFICATION OF MONTHLY MEAN FORECASTS FOR FIRE WEATHER ELEMENTS IN THE CONTIGUOUS UNITED-STATES, Journal of climate, 9(12), 1996, pp. 3317-3327
The authors first review a system for specifying monthly mean anomalie
s of midday temperature (T), dewpoint (D), and wind speed (W) at a lar
ge network of surface stations across the United States. Multiple regr
ession equations containing approximately three terms were derived for
each element and month from concurrent fields of 700-mb height anomal
y (H) observed over North America and vicinity, plus the previous mont
h's observed local anomaly of T, D, or W, during the 20-year period 19
64-1983. Results of testing this forecast system on prognostic values
of H prepared twice a month at the National Weather Service from 1973
to 1990 and on observed values of H during the independent period from
1984 to 1990 are presented. The authors pooled the data for all month
s and 122 stations to compute Heidke skill scores (HSS) for two, three
, four, and five classes for each weather element. All scores showed s
kill that dropped steadily as the number of classes increased. In all
cases skill was highest for T and lowest for W, the same result as tha
t obtained in the original derivation. In order to examine the distrib
ution of skill, we computed the HSS separately for each class. The ski
ll scores for the first and last classes were greater than those for t
he middle class for all elements and months. It is encouraging that fo
recasts above the 90th percentile, the most critical category for fire
potential, consistently showed greater skill than forecasts for any o
ther class. Geographical and seasonal variations of skill based on pro
gnostic height was also examined. The results showed that skill is str
ongly dependent on location, month, and weather element. Mean annual s
cores were positive for each element in all parts of the country, whil
e monthly scores were highest in January and lowest in October. Althou
gh the forecasts based on prognostic heights were more skillful than c
limatology for all weather elements, they improved over month-to-month
persistence only for T and D. If the height forecasts had been perfec
t, the skill scores for these elements would have been about two to th
ree times as large as those for prognostic heights and four to five ti
mes as large as the persistence scores. When the test period was divid
ed into two subperiods, values of HSS were considerably higher in the
later period, despite a drop in persistence scores from the early to t
he later period. The authors attribute this improvement to increased a
ccuracy of medium-range numerical model predictions during the 1980s.