The Ozone Hole 2015

NASA Report

The ozone hole over Antarctica grew relatively
large in 2015, according to data acquired by the
Ozone Monitoring Instrument (OMI) on NASA’s Aura satellite and the
Ozone Monitoring and Profiler Suite (OMPS) on the NASA-NOAA Suomi NPP
satellite.

On October 2, 2015, OMI observed that the hole
had reached its largest single-day area for the year. The image above, based on
data acquired with OMI, shows the hole on that day. It spanned 28.2 million
square kilometers (10.9 million square miles)—the fourth-largest area measured
since the start of the satellite record in 1979. The largest single-day ozone
hole recorded by satellite was 29.9 million square kilometers (11.5 million
square miles) on September 9, 2000.

The ozone “hole” is not literally a hole; rather,
the phenomenon is defined as the area where the concentration of ozone drops
below the historical threshold of 220
Dobson Units. In the image above, those areas are purple and blue.

The ozone depletion phenomenon is seasonal,
starting each year during the Antarctic spring and peaking between mid-September
and early October. In 2015, the hole started slowly but then quickly expanded to
cover a large area. The average size in September–October 2015 was 25.6 million
square kilometers (9.9 million square miles)—also the fourth largest since the
start of the satellite record. The largest September–October average on record
was 26.6 million square kilometers (10.3 million square miles) in 2006.

In 2015, ozone concentrations also plunged lower
than in recent years. On October 4, ozone reached an annual minimum
concentration of 101 Dobson Units.

While the ozone hole area was large in 2015, the
size was consistent with what scientists know about ozone depletion and
chemistry. According to NASA atmospheric scientist Paul Newman, there are still
plenty of ozone-depleting chlorine and bromine compounds present in the
stratosphere. Moreover, the lower stratosphere was colder than in previous
years, which creates favorable conditions for ozone-depleting chemical
reactions.

Visit
World of Change: Antarctic Ozone Hole to see how the holes have evolved
since 1979.

• References and Related Reading

• NASA Earth Observatory (2015)
  World of Change: Antarctic Ozone Hole.

• NASA Goddard (2015, October 23)
  Ozone Hole Watch. Accessed October 26, 2015.

• NASA Goddard (2015, October 22)
  NASA Study Shows That Common Coolants Contribute to Ozone Depletion.
  Accessed October 26, 2015.

• NASA Goddard (2015, October 7)
  2015 Antarctic Ozone Hole Area Approaches Annual Maximum. Accessed October
  26, 2015.

• Ozone Monitoring and Profiler Suite blog
  (2015, October 11)
  The Ozone Hole for 2015. Accessed October 26, 2015.Caption by Kathryn
  Hansen.

Antarctic Situation at 2016
January 4
British Antarctic Survey Ozone Bulletin

Antarctic ozone today: The 2015 ozone hole is over.
The ozone distribution is that of the summer with ozone amounts more uniform
over the continent. Values currently range from around 270 DU to around 350 DU.
There are significant differences between the various satellite measurements. In
the lower half of the ozone layer temperatures are near their summer peak. At
the highest level the temperature has passed its summer peak and is now cooling.
Temperatures in the ozone layer are well above the threshold for Polar
Stratospheric Cloud (PSC) formation.

The 2015 ozone hole: Meteorological
conditions were favourable for the creation of a significant ozone hole, with a
stable polar vortex and a cold stratosphere. Ozone hole levels
were briefly reached over the Antarctic Peninsula on August 5 and over Halley
the next day in a dynamic event. Significant ozone depletion over the continent
began in mid August as the sun returned. Depletion became more widespread by
September, exceeding the mean for the last decade and greater than in the last
couple of years. Ozone declined by about 1% per day near the centre of the ozone
hole. The ozone hole peaked at some 26 million square kilometres in the first
half of October. It was the largest ozone hole ever for the time of year in the
second half of October. It became more elliptical in early November, affecting
the Falkland Islands and South Georgia over November 4 and 5, and again around
November 20 to 23. It remained amongst the largest of the decade into mid
December. The polar vortex was the largest over the past decade in the upper
part of the ozone layer from July to October and the area with PSCs was also
larger than average during this period. At lower levels the vortex was largest
ever, by a considerable amount, from October and into December.

There is no
evidence for any effect on ozone values from aerosol from the eruption of
Calbuco in southern Chile in late April. Most, if not all, of the volcanic
aerosol remained north of Antarctica.

Antarctic Situation at 2015
December 7British
Antarctic Survey Ozone Bulletin

Antarctic ozone today: Ozone depletion remains
extensive and the ozone hole still covers a large part of Antarctica, centered
on Dronning Maud Land. The ozone hole is slowly beginning to shrink and fill and
is now around 11 million square kilometres, still much larger than the average
over the last decade and close to or above the extreme. The ozone distribution
is that of late spring with ozone amounts over the continent recovering from
their minimum, and higher values around the Southern Ocean. Values currently
range from around 170 DU over Dronning Maud Land, to around 350 DU over parts of
the Southern Ocean. There are significant differences between the various
satellite measurements. Through most of the ozone layer temperatures are much
below the long term average, particularly in the lower part, but are warming. At
the highest level the temperature has reached its summer peak. Temperatures in
the ozone layer are above the threshold for Polar Stratospheric Cloud (PSC)
formation. The polar vortex remains much larger than average in size,
particularly at the base of the ozone layer, but is shrinking. The ozone hole is
entering its final phase and is expected to continue to shrink in area and to
fill, but will last into mid December.

The 2015 ozone hole: Meteorological
conditions were favourable for the creation of a significant ozone hole, with a
stable polar vortex. Ozone hole levels were briefly
reached over the Antarctic Peninsula on August 5 and over Halley the next day in
a dynamic event. Significant ozone depletion over the continent began in mid
August as the sun returned. Depletion became more widespread by September,
exceeding the mean for the last decade and greater than in the last couple of
years. Ozone declined by about 1% per day near the centre of the ozone hole. The
ozone hole peaked at some 26 million square kilometres in the first half of
October. Halley station saw its lowest ozone values since 2011 in mid-month. It
was the largest ozone hole ever for the time of year in the second half of
October. It became more elliptical in early November, affecting the Falkland
Islands and South Georgia over November 4 and 5, and again around November 20 to
23. The polar vortex was the largest over the past decade in the upper part of
the ozone layer from July to October and the area with PSCs was also larger than
average during this period. At some levels the vortex was largest, by a
considerable amount, in late October and early November

Antarctic Situation at 2015
November 16
British Antarctic Survey Ozone Bulletin

Antarctic ozone today: Ozone depletion remains
extensive and the ozone hole still covers most of Antarctica, centered on West
Antarctica. The edge of the ozone hole is likely to affect the tip of South
America and the Falkland Islands during the week. The ozone hole is slowly
beginning to shrink and fill and is now around 16 million square kilometres,
still much larger than the average over the last decade. The ozone distribution
is that of late mid spring with ozone amounts over the continent beginning to
recover from their minimum, and higher values around the Southern Ocean. Values
currently range from around 150 DU over the interior, to over 400 DU over parts
of the Southern Ocean. There are significant differences between the various
satellite measurements. Through most of the ozone layer temperatures are much
below the long term average but are warming. Temperatures in the ozone layer are
now above the threshold for Polar Stratospheric Cloud (PSC) formation but some
PSCs may still exist. The polar vortex remains much larger than average in size,
but is shrinking. The ozone hole is expected to continue to shrink in area and
to slowly fill.

The 2015 ozone hole: Meteorological
conditions were favourable for the creation of a significant ozone hole, with a
stable polar vortex. Ozone hole levels were briefly
reached over the Antarctic Peninsula on August 5 and over Halley the next day in
a dynamic event. Significant ozone depletion over the continent began in mid
August as the sun returned. Depletion became more widespread by September,
exceeding the mean for the last decade and greater than in the last couple of
years. Ozone declined by about 1% per day near the centre of the ozone hole. The
ozone hole peaked at some 26 million square kilometres in the first half of
October. Halley station saw its lowest ozone values since 2011 in mid-month. It
was the largest ever for the time of year in the second half of October. It
became more elliptical in early November, affecting the Falkland Islands and
South Georgia over November 4 and 5. The polar vortex was the largest over the
past decade in the upper part of the ozone layer from July to October and the
area with PSCs was also larger than average during this period. At some levels
the vortex was largest, by a considerable amount, in late October and early
November.

It is not clear
what effect, if any, the eruption from Calbuco in southern Chile had on the
ozone values. It seems that most of the volcanic aerosol remained north of
Antarctica.

Antarctic Situation at 2015
November 9British
Antarctic Survey Ozone Bulletin

Antarctic ozone today: Ozone depletion remains
extensive and the ozone hole still covers most of Antarctica, centered on West
Antarctica. It is slowly beginning to shrink and is now around 16 million square
kilometres. The ozone distribution is that of late mid spring with ozone amounts
over the continent beginning to recover from their minimum, and higher values
around the Southern Ocean. Values currently range from around 150 DU over the
interior, to over 400 DU over parts of the Southern Ocean. There are significant
differences between the various satellite measurements. Through most of the
ozone layer temperatures are much below the long term average but are warming.
Temperatures in the lowest part of the ozone layer are still below the threshold
for Polar Stratospheric Cloud (PSC) formation over a small part of Antarctica
and the area with PSCs remains significantly larger than average, but is rapidly
decreasing. The polar vortex remains much larger than average in size, but is
shrinking. The area of the ozone hole is expected to continue to shrink, but
towards the end of next week it will again become more eliptical.

The 2015 ozone hole: Meteorological
conditions were favourable for the creation of a significant ozone hole, with a
stable polar vortex. Ozone hole levels were briefly
reached over the Antarctic Peninsula on August 5 and over Halley the next day in
a dynamic event. Significant ozone depletion over the continent began in mid
August as the sun returned. Depletion became more widespread by September,
exceeding the mean for the last decade and greater than in the last couple of
years. Ozone declined by about 1% per day near the centre of the ozone hole. The
ozone hole peaked at some 26 million square kilometres in the first half of
October. Halley station saw its lowest ozone values since 2011 in mid-month. It
was the largest ever for the time of year in the second half of October. It
became more elliptical in early November, affecting the Falkland Islands and
South Georgia over November 4 and 5. The polar vortex was the largest over the
past decade in the upper part of the ozone layer from July to October and the
area with PSCs was also larger than average during this period.

It is not clear
what effect, if any, the eruption from Calbuco in southern Chile had on the
ozone values. It seems that most of the volcanic aerosol remained north of
Antarctica.

Annual Antarctic Ozone Hole Larger
and Formed Later in 2015

NASA’s Goddard Space Flight Center, Greenbelt, Md.-Oct. 29, 2015-The 2015
Antarctic ozone hole area was larger and formed later than in recent years, said
scientists from NASA and the National Oceanic and Atmospheric Administration
(NOAA).

On Oct. 2, 2015, the ozone hole expanded to its peak of 28.2 million square
kilometers (10.9 million square miles), an area larger than the continent of
North America. Throughout October, the hole remained large and set many area
daily records. Unusually cold temperature and weak dynamics in the Antarctic
stratosphere this year resulted in this larger ozone hole. In comparison, last
year the ozone hole peaked at 24.1 million square kilometers (9.3 million square
miles) on Sept. 11, 2014. Compared to the 1991-2014 period, the 2015 ozone hole
average area was the fourth largest.

This false-color image shows ozone concentrations above Antarctica on Oct. 2,
2015. Credits: NASA/Goddard Space Flight Center

“While the current ozone hole is larger than in
recent years, the area occupied by this year’s hole is consistent with our
understanding of ozone depletion chemistry and consistent with colder than
average weather conditions in Earth’s stratosphere, which help drive ozone
depletion,” said Paul A. Newman, chief scientist for Earth Sciences at NASA’s
Goddard Space Flight Center in Greenbelt, Maryland.

The ozone hole is a severe depletion of the ozone layer above Antarctica that
was first detected in the 1980s. The Antarctic ozone hole forms and expands
during the Southern Hemisphere spring (August and September) because of the high
levels of chemically active forms of chlorine and bromine in the stratosphere.
These chlorine- and bromine-containing molecules are largely derived from
man-made chemicals that steadily increased in Earth’s atmosphere up through the
early 1990s.

“This year, our balloon-borne instruments measured nearly 100 percent ozone
depletion in the layer above South Pole Station, Antarctica, that was 14 to 19
kilometers (9 to 12 miles) above Earth’s surface,” said Bryan Johnson, a
researcher at NOAA’s Earth System Research Laboratory in Boulder, Colorado.
“During September we typically see a rapid ozone decline, ending with about 95
percent depletion in that layer by October 1. This year the depletion held on an
extra two weeks resulting in nearly 100 percent depletion by October 15.” 

The ozone layer helps shield Earth from potentially harmful ultraviolet
radiation that can cause skin cancer, cataracts, and suppress immune systems, as
well as damage plants. The large size of this year’s ozone hole will likely
result in increases of harmful ultraviolet rays at Earth’s surface, particularly
in Antarctica and the Southern Hemisphere in the coming months.

Ozone depletion is primarily caused by man-made compounds that release chlorine
and bromine gases in the stratosphere. Beginning in 1987, the internationally
agreed-upon Montreal Protocol on Substances that Deplete the Ozone Layer has
regulated these ozone-depleting compounds, such as chlorine-containing
chlorofluorocarbons used in refrigerants and bromine-containing halon gases used
as fire suppressants. Because of the Protocol, atmospheric levels of these ozone
depleting compounds are slowly declining. The ozone hole is expected to recover
back to 1980 levels in approximately 2070.

This year, scientists recorded the minimum thickness of the ozone layer at 101
Dobson units on October 4, 2015, as compared to 250-350 Dobson units during the
1960s, before the Antarctic ozone hole occurred. Dobson units are a measure of
the overhead amount of atmospheric ozone.

The satellite ozone data come from the Dutch-Finnish Ozone Monitoring Instrument
on NASA’s Aura satellite, launched in 2004, and the Ozone Monitoring and
Profiler Suite instrument on the NASA-NOAA Suomi National Polar-orbiting
Partnership satellite, launched in 2011. NOAA scientists at the South Pole
station monitor the ozone layer above that location by using a Dobson
spectrophotometer and regular ozone-sonde balloon launches that record the
thickness of the ozone layer and its vertical distribution. Chlorine amounts are
estimated using NOAA and NASA ground measurements and observations from the
Microwave Limb Sounder aboard NASA’s Aura satellite. These satellites continue a
data record dating back to the early 1970s.

Antarctic Situation at 2015
October 26British
Antarctic Survey Ozone Bulletin

Antarctic ozone today: Ozone depletion remains
extensive and the ozone hole covers most of Antarctica. The ozone hole grew
rapidly from mid August onwards and peaked at some 26 million square kilometres
in the first half of October. It is slowly beginning to shrink and is now around
23 million square kilometres. This is the largest hole that has been recorded at
this time of year. The ozone distribution is that of late mid spring with ozone
amounts over the continent beginning to recover from their minimum, and higher
values around the Southern Ocean. Values currently range from around 130 DU over
Dronning Maud Land, to nearly 400 DU over parts of the Southern Ocean. These
highest values are lower than at the same time last year. There are significant
differences between the various satellite measurements. Temperatures in the
lower part of the ozone layer are still below the threshold for Polar
Stratospheric Cloud (PSC) formation over parts of Antarctica and the area with
PSCs remains larger than average, but is rapidly decreasing. Through most of the
ozone layer temperatures are below the long term average but are warming and in
the higher parts of the ozone layer are above the PSC formation threshold. The
polar vortex is larger than average in size.

The 2015 ozone hole:
Meteorological conditions were favourable for the creation of a significant
ozone hole, with a stable polar vortex. Ozone hole levels were briefly
reached over the Antarctic Peninsula on August 5 and over Halley the next day in
a dynamic event. Significant ozone depletion over the continent began in mid
August. Depletion became more widespread by September, exceeding the mean for
the last decade and greater than in the last couple of years. Ozone declined by
about 1% per day near the centre of the ozone hole. The ozone hole peaked at
some 26 million square kilometres in the first half of October. It was the
largest ever for the time of year in the second half of October. The polar
vortex was the largest over the past decade in the upper part of the ozone layer
from July to September and the area with PSCs was also larger than average
during this period. Halley station saw its lowest ozone values since 2011.

Antarctic Situation at 2015 September 28
British Antarctic Survey Ozone Bulletin

Antarctic ozone today: Ozone depletion is now extensive and the ozone hole
covers Antarctica. The ozone hole grew rapidly from mid August onwards and is
near its largest at some 25 million square kilometres. This is a larger hole
than the average of those over the last decade. The ozone distribution is that
of mid spring with lowest and still decreasing ozone amounts across the
continent, particularly the Atlantic
sector, and higher (and increasing) values around the Southern Ocean. Ozone is
declining by about 1% per day near the centre of the ozone hole. Values
currently range from around 130 DU over West Antarctica to near 400 DU over
parts of the Southern Ocean. These highest values are lower than at the same
time last year. There are significant differences between the various satellite
measurements. Temperatures in the lower part of the ozone layer are below the
threshold for Polar Stratospheric Cloud (PSC) formation over much of Antarctica
and the area with PSCs is larger than average, but is now decreasing. Through
most of the ozone layer temperatures are below the long term average but are
beginning to warm and in the higher parts of the ozone layer are above the PSC
formation threshold. The polar vortex is near average in size at most levels
except the highest and lowest, where it is significantly larger than average.

Antarctic Situation at 2015
September 21British
Antarctic Survey Ozone Bulletin

Antarctic ozone today: Ozone depletion is now
extensive and ozone hole levels have been reached across much of Antarctica. The
ozone hole grew rapidly from mid August onwards and now covers some 25 million
square kilometres. This is larger than the average of those over the last
decade. The ozone distribution is that of early spring with generally lower and
decreasing ozone amounts across the continent, particularly the Atlantic sector,
and higher (and increasing) values around the Southern Ocean. Ozone is declining
by about 1% per day near the centre of the ozone hole. Values currently range
from around 150 DU over the Weddell Sea area to around 370 DU over parts of the
Southern Ocean. These highest values are lower than at the same time last year.
There are significant differences between the various satellite measurements.
Temperatures in the lower part of the ozone layer are below the threshold for
Polar Stratospheric Cloud (PSC) formation over much of Antarctica and the area
with PSCs is larger than average. Through most of the ozone layer temperatures
are below the long term average but are beginning to warm and in the higher
parts of the ozone layer are above the PSC formation threshold. The polar vortex
is near average in size at most levels except the highest and lowest, where it
is significantly larger than average.

The 2015 ozone hole:
Ozone hole levels were briefly reached over the Antarctic Peninsula on
August 5 with significant depletion beginning in mid August. Depletion became
more widespread by September, exceeding the mean for the last decade and greater
than in the last couple of years.

Antarctic Situation at 2015
September 14British
Antarctic Survey Ozone Bulletin

Antarctic ozone today: Ozone depletion is now
becoming extensive and ozone hole levels have been reached across over half of
Antarctica. The ozone hole grew rapidly from mid August onwards and now covers
some 22 million square kilometres. This is a little larger than the average of
those over the last decade. The ozone distribution is that of early spring with
generally lower and decreasing ozone amounts across the continent, particularly
the Atlantic sector, and higher (and increasing) values around the Southern
Ocean. Ozone is declining by about 1% per day near the centre of the ozone hole.
Values currently range from around 180 DU over the Weddell Sea to around 380 DU
over parts of the Southern Ocean. There are significant differences between the
various satellite measurements. Temperatures in the ozone layer are below the
threshold for Polar Stratospheric Cloud (PSC) formation over much of Antarctica
and the area with PSCs is larger than average. Through most of the ozone layer
temperatures are below the long term average but are beginning to warm. The
polar vortex is near average in size at most levels except the highest and
lowest, where it is significantly larger than average.

The 2015
ozone hole:
Ozone hole levels
were briefly reached over the Antarctic Peninsula on August 5 with significant
depletion beginning in mid August. Depletion became more widespread by
September, exceeding the mean for the last decade and greater than in the last
couple of years.

Antarctic Situation at 2015
September 11British
Antarctic Survey Ozone Bulletin

Antarctic ozone today: Ozone depletion is now
becoming more extensive and ozone hole levels have been reached across over half
of Antarctica. The ozone hole covers some 15 million square kilometres. The
ozone distribution is that of early spring with generally lower and decreasing
ozone amounts across the continent and higher (and increasing) values around the
Southern Ocean. Ozone is declining by about 1% per day near the centre of the
ozone hole. Values currently range from around 190 DU to around 380 DU over
parts of the Southern Ocean. There are significant differences between the
various satellite measurements. Temperatures in the ozone layer are below the
threshold for Polar Stratospheric Cloud (PSC) formation over much of Antarctica.
Through most of the ozone layer temperatures are below the long term average but
are beginning to warm. The polar vortex is near average in size at most levels
except the highest, where it is significantly larger than average.

The 2015 ozone hole: Ozone hole levels
were briefly reached over the Antarctic Peninsula on August 5 with significant
depletion beginning in mid August. Depletion became more widespread by
September, approaching the mean for the last decade and greater than in the last
couple of years.

Antarctic Situation at 2015
August 28British
Antarctic Survey Ozone Bulletin

Antarctic ozone today: Ozone depletion is now
becoming more extensive and ozone hole levels have been reached over parts of
West Antarctica and the Weddell Sea. They were briefly reached over the
Antarctic Peninsula on August 5. The ozone distribution is that of early spring
with generally lower and decreasing ozone amounts across the continent and
higher (and increasing) values around the Southern Ocean. Values currently range
from around 220 DU to around 370 DU over parts of the Southern Ocean. There are
significant differences between the various satellite measurements. Temperatures
in the ozone layer are below the threshold for Polar Stratospheric Cloud (PSC)
formation over much of Antarctica. Through most of the ozone layer temperatures
are below the long term average and near their coldest, but are beginning to
warm at the highest levels. The polar vortex is near average in size at most
levels except the highest, where it is larger than average.

Antarctic Situation at 2015
August 10British
Antarctic Survey Ozone Bulletin

Antarctic ozone today: Ozone depletion is now
taking place and ozone hole levels were reached over the Antarctic Peninsula on
August 5. The ozone distribution is that of winter with generally lower and
decreasing ozone amounts across the continent and higher (and increasing) values
around the Southern Ocean. Values currently range from around 240 DU over parts
of the continent, to around 400 DU over parts of the Southern Ocean. There are
significant differences between the various satellite measurements. Temperatures
in the ozone layer are below the threshold for Polar Stratospheric Cloud (PSC)
formation over much of Antarctica. Through most of the ozone layer temperatures
are below the long term average and near their coldest, but are beginning to
warm at the highest levels. The polar vortex is near average in size at most
levels except the highest, where it is larger than average.

Antarctic Situation at 2015
August 3British
Antarctic Survey Ozone Bulletin

Antarctic ozone today: The ozone distribution is
that of winter with generally lower and decreasing ozone amounts across the
continent and higher (and increasing) values around the Southern Ocean. Values
currently range from around 230 DU over the Pole, to around 400 DU over parts of
the Southern Ocean. There are significant differences between the various
satellite measurements. Temperatures in the ozone layer are below the threshold
for Polar Stratospheric Cloud (PSC) formation over much of Antarctica. Through
most of the ozone layer temperatures are below the long term average, but are
beginning to warm at the highest levels.

The Ozone
Hole August 2015

The
Ozone Hole September 2015

The
Ozone Hole October 2015

The
Ozone Hole November 2015

The
Ozone Hole December 2015