All are timeseries
for austral spring (SON).
Not exact matches
Increasing
austral -
spring insolation combined with sea - ice albedo feedbacks appear to be the key factors responsible
for this warming.»
They reported an annual warming of West Antarctica of 0.18 °C / decade
for 1957 — 2006, maximized in the
austral winter and
spring.
Regardless of the exact reasons
for differences in the TOGA and GOGA experiments, the model results support the notion that SSTs in the tropics to subtropics have played a role in forcing the atmospheric circulation trends over the SH in
austral spring.