Extratropical
Highlights –November 2025
1. Northern
Hemisphere
The
500-hPa circulation during November featured a canonical negative North
Atlantic Oscillation (NAO) teleconnection pattern with enhanced above average
height anomalies over Greenland and below average height anomalies stretching
from eastern North America, across the North Atlantic Ocean, to Scandinavia (Figs.
E7, E9). The main
land-surface temperature signals include above average temperatures across most
of North America and Eurasia (Fig. E1). The
main precipitation signals include above average rainfall in northern Eurasia
and below average rainfall in eastern North America and southern Eurasia (Fig.
E3).
a. North America
The
500-hPa circulation during November featured an amplified ridge over the west
half of Canada and the contiguous U.S., along with a strong maxima located over
the Canadian Maritime. A strong center of below average heights was located
over the Gulf of St. Lawrence and down the U.S. Eastern Seaboard and Midwest (Fig.
E9). During the month of November, temperatures
across North America were predominantly above average with large areas in the
Western U.S. recording values in the highest 90th percentile of occurrences (Fig.
E1). Precipitation totals were well below average
across the eastern half of North America with several areas recording values in
the driest 10th percentile (Fig. E3). Across
the U.S., nearly all regions recorded below (or near normal) rainfall with the
exception of Southern California which recorded above average rainfall due to a
series of atmospheric rivers that impacted the region during November (Figs.
E3, E5).
b. Europe and Asia
The
500-hPa circulation during November featured an amplified ridge over the Middle
East and European Russia, and below average heights across the United Kingdom,
Scandinavia, and Siberia (Fig. E9).
Temperatures were largely above normal across Europe and Asia with several
regions in the Middle East and European Russia recording values in the highest
90th percentile of occurrences (Fig. E1).
Temperatures across Siberia and the Kamchatka Peninsula were below average or
near normal (Fig. E1). Wetter than average
conditions were recorded for the United Kingdom, northwest Spain, Southern
Europe, and northern Russia, and drier than average conditions prevailed across
the Middle East (Figs. E3, E4).
Many areas in the European Plain received rainfall totals in the highest 90th
percentile of occurrences (Fig. E3).
c. Atlantic
hurricane season
The
2025 Atlantic hurricane season produced 13 named storms, with 5 becoming
hurricanes and 4 of those becoming major hurricanes (average: 3). The 2025
Accumulated Cyclone Energy (ACE) value was about 7% above normal according to
the 1951-2020 median. Based on this activity, NOAA classifies the season as
being above normal based on ACE energy, despite the total number of storms
being less than the average. An average season has 14 named storms, 7
hurricanes, and three major hurricanes. This season several storms reached
Category 5 status, to include Erin, Humberto, and Melissa.
2. Southern
Hemisphere
The
500-hPa height field during November resembled a quadrature wavetrain pattern
with a maxima in heights located over Antarctica (Fig. E15).
Temperatures were above normal or near normal across South America, Africa, and
eastern Australia (Fig. E1). Below average
rainfall was recorded across most of South America, including Brazil, which has
recorded below average rainfall for the last year, and across central Africa (Figs.
E3, E4). Above average
rainfall was recorded across South Africa with several regions reaching the
wettest 90th percentile of occurrences (Figs. E3, E4).
The
Antarctic ozone hole typically develops during August and reaches peak size in
September. The ozone hole then gradually decreases during October and November,
and dissipates on average in early December. During 2025, the size of the ozone
hole was well below the 2015-2024 range of ozone hole sizes and dissipated
earlier than is typical (Fig. S6 top). The Southern
Hemisphere vortex area also dissipated early and was below average, along with
polar stratospheric cloud area, but within the 2015-2024 range of measurements
(Fig. S6 middle and bottom).