Robert Hart and Richard Grumm
Updated 16 April 2003 to note non-record 10 April 2003 cut-off cyclone.
Description
The rarity of observed and forecast conditions across the eastern half of the U.S. and SE Canada is depicted here.
The magnitude of rarity is defined as the maximum absolute number of standard deviations fields depart from daily norms (the anomaly magnitude).
This is calculated for each of four variables: height, temperature, wind, and moisture.
Example current and forecast plan-view anomaly fields are available for output from the Ensemble webpage
The vertical mass-weighted mean anomaly is calculated for each of the above four variables (MHEIGHT, MTEMP, MWIND, and MMOIST respectively.)
The total anomaly (measure of rarity or extreme) is the mean of the four anomalies:
A brief summary of interpretting MTOTAL (assuming a 2.50 grid resolution):
(Standard Deviations) |
based on 52-year database |
|
 
Therefore, MTOTAL can be interpretted rougly as how unusual the atmospheric conditions
are across the eastern United States, Southeast Canada, and the adjacent
waters.
PERSPECTIVE:
Latest conditions and forecasts:
Important NOTE: Model-forecast tropical cyclones are not intended to be included as part of the rarity index shown here.
Other current model forecasts: [
NAM |
Archive of model forecasts.
To compare the current and forecast climate departures above to past events, check the
historical rankings analysis from 1948-current.
Notes on recent events:
Important Note: These preliminary updates to the "official" rankings are not included until the departures are recalculated using the NCEP 2.5 degree reanalysis fields. These typically aren't available for 1-3 months after the event and tend to have an MTOTAL value slightly less than those analyzed by the higher-resolution NAM,and GFS grids. When comparing the forecast MTOTAL values to historical cases, the 2.5 deg GFS forecasts (plotted above) should be used.
Robert Hart, FSU Meteorology,Tallahasse, FL
Bogus (falsely predicted) tropical cyclones can produce erroneously large forecast anomalies, especially beyond 72hrs.
Last Updated: 3 October 2005
Rich Grumm, NWS State College