Pt. Soule et Pw. Suckling, VARIATIONS IN HEATING AND COOLING DEGREE-DAYS IN THE SOUTH-EASTERN USA, 1960-1989, International journal of climatology, 15(4), 1995, pp. 355-367
Temporal trends and spatial variability of heating and cooling degree-
days are examined for a portion of the south-eastern USA for the perio
d 1960-1989. Temporal variability is examined through simple time-seri
es analyses, regression analyses, and a climate departure index (CDI).
Maps of 30-, 15-, 10-, and 5-year climatic normals for degree-days ar
e presented. The CDI indicates that heating degree-day (HDD) variabili
ty was high during the 1970s with a sudden drop to low variability dur
ing the 1980s. Simple regressions show weak downward trends for actual
HDD values across the region during the study period. However, the HD
D decline was more pronounced through the 1980s, coinciding with the p
eriod of low year-to-year variability. Isoline maps show that most sit
es recorded distinctly fewer HDD in the most recent 5-year period comp
ared with longer term averages. Although the long-term trend for cooli
ng degree-days (CDD) is slightly positive, there is considerable inter
yearly and interdecadal variability. Unlike HDD, there were no sustain
ed periods with consistently high or low variability for CDD. Mapped p
atterns of climatic normals show that CDD values peaked across the stu
dy area during the most recent 5-year period. Mapped patterns for both
HDD acid CDD can be influenced by data for large urban sites. Repeati
ng the analyses without the seven largest urban centres resulted in le
ss anomalous spatial patterns but almost no shift in study area mean-d
egree-day or CDI values and their temporal patterns. Atlanta emerged a
s the most distinct anomaly for the mapped patterns. From an applied v
iewpoint, the most significant finding occurred for the heating season
with the combination of a sustained downward trend in HDD and compara
tively low variability around the long mean (Low CDI values) during th
e last 13 years of the study period. This period represents a span whe
re the climate-driven demand for space heating was decreasing and the
heating-season generating capacities for power generation utilities we
re not challenged.