BAS Ozone
Bulletin 01/01
The 2001 ozone hole reached an area of over 25 million square
kilometres at its maximum, but it is now shrinking and filling.
At around 18 million square kilometres in size, it is still
significantly larger than at this time last year. The hole
is offset from the pole, with lowest values, below 150 DU (50%
depletion), over Dronning Maud Land and significant depletion
extends towards Africa. The winter high ozone belt in the
south temperate regions generally surrounds Antarctica,
particularly over the Pacific sector.
1. Data from the British Antarctic Survey (BAS) Halley
station (76-deg south, 27-deg west, on the Brunt ice shelf).
a)
Ozone. Ozone measurements in the first half of August are
made using moonlight and are of very low accuracy. Some
early Halley observations using moonlight gave total ozone values
around 220 DU at the beginning of August, a depletion of about
25%. In September values dropped, from around 180 DU at the
beginning of the month, at around 2 DU per day. From the
equinox to late October values were around 125 DU, which is 60%
below the normal. The minimum daily mean value recorded
this year was 116 DU. Values are now increasing, but at 170
DU remain 50% below the normal.
Halley preliminary mean daily total ozone, (DU)
Dobson No 103: Instrument constants revised 2001 October 26.
(0 indicates no data)
2001 August 1 – 2001 October 31
0 223 229 234 223 210 0 0
0 0
0 0 0 0 0
0 0 0 0 0
0 0 0 0 0
0 0 0 0 0
0
0 0 0 0 0
0 168 164 172 184
174
158 158 144 144 137 146 148 142 125
121
120 126 144 136 133 144 127 161 169
136
121 116 120 125 135 132 127 130 147
132
129 130 136 130 125 120 146 137 132
123
138 139 152 142 134 140 140 173 176 222
Halley provisional monthly mean total ozone (DU)
Period Aug Sep Oct Nov Dec Jan Feb Mar Apr Year
2001/02 224 148 138
2000/01 179 151 137 267 299 286 261 251 245 231
1999/00 205 172 143 172 254 281 258 250 256 221
1998/99 221 162 140 183 255 272 259 254 267 224
1997/98 218 171 141 210 286 267 262 264 261 231
1957-72 295 285 300 355 350 320 300 295 285 310
Note that August
and April do not have observations on every day, and that the
routine measurement season is now longer than it was in 1957 -
72. Measurements made at the start of the season are of
lower accuracy than in mid summer due to the low solar elevation
or use of moonlight. Gif images showing the data are
available on the BAS ozone web-page.
b)
Radiosonde data. The 100 hPa temperature at Halley remained
at winter values of around –83�C until late October. At
-75�C it remains substantially below the normal (-62�C), but
has undergone some warming in the last week. It was a few degrees
below the normal for most of the first half of 2001, except for a
short period between mid March and the end of April.
2. Data from the British Antarctic Survey (BAS) Rothera
station (68-deg south, 68-deg west on Adelaide Island).
a)
Ozone. Ozone measurements from Rothera are made using a
SAOZ (Systeme d'Automatique Observations Zenithales)
spectrometer. This research instrument has a preliminary
calibration such that it reads about 15% low compared to Dobson
measurements at 100 DU, and is in agreement at 300 DU. Rothera
recorded sub 200 DU between July 27 and 29. Values
generally declined from a peak of 340 DU at the beginning of July
to 150 DU in mid September and climbed above 250 DU near the end
of the month. They dropped to around 140 DU in mid October.
The mean daily total ozone values generally show a similar
pattern of variation to that seen at Vernadsky, though day to day
variation does not show such pronounced wave activity and minimum
values are a little lower.
Rothera preliminary mean daily total ozone, (DU)
(0 indicates no data or data not available)
2001 July 1 - 2001 October 22
321 329 304 311 334 316 314 345 348 316
311 291 324 0
0 268 265 258 285 279
285 227 253 294 293 270 196 194 187
211 272
0 264 254 223 270 259 245
214 255 255
289 277 259 259 234 232 233 258 283
0
0 266 206 199 205 229 185
213 192 205 214
206 199 177 246 246 200 186 170 171
169
0 0 160 168 203
154 150 198 131 124
159 231 319 311 294 260 196 230 263
222
218 0 178 192 193 183
195 175 164 156
136 149 139 144 136 152 160 144 129
125
130 157
Rothera provisional monthly mean total ozone (DU)
Period Jul Aug Sep Oct Nov Dec Jan Feb Mar Apr May Jun
2001/02 283 238 205
2000/01 231 230 137 168 334 294 273 278 279 278 280 276
1999/00 274 243 157 175 229 289 282 265 264 290 282 293
1998/99 288 239 159 166 252 264 270 279 267 277 300 287
1997/98
270 280 267 263
b)
Stratospheric clouds. Nacreous or mother-of-pearl clouds
are regularly seen from stations along the Antarctic Peninsula
between early May and October, with a peak in July. There
is some evidence that their frequency of occurrence has increased
since the mid 1950s. This year, clouds were sighted
from Rothera on August 3, 20, 27 and September 5, 6 and 25.
3. Data
from the Ukrainian Antarctic Research Centre Vernadsky
station (65-deg south, 64-deg west on the coast of the Antarctic
Peninsula, formerly the BAS Faraday station).
a)
Ozone. Ozone values at Vernadsky generally declined from
about 280 DU at the beginning of August to around 210 DU (a
depletion of about 35%) in mid September. A significant rise
above 350 DU took place around the equinox, then values dropped
to around 170 DU (a depletion of about 50%) in mid October. They
rose to near normal values at the end of the month. There was
considerable diurnal variation in the ozone readings at Vernadsky
when the station lay under a strong stratospheric ozone gradient.
Vernadsky preliminary mean daily total ozone (DU).
Dobson No 31: Instrument constants revised 2001 October 18
2001 August 1 – 2001 October 31
308 293 285 234 297 258 247 236 250 208
306 299 248 256 243 236 249 232 252
222
267 286 208 228 196 224 196 212 199
200 219
279 224 191 245 285 253 268 244 185
202
216 257 205 239 273 190 168 261 183
157
161 229 365 345 322 296 263 238 289
299
317 215 167 325 316 236 243 235 218
213
195 182 187 185 180 190 234 177 173
183
158 176 187 147 187 291 220 403 351
388 362
Vernadsky provisional monthly mean total ozone (DU)
Period Aug Sep Oct Nov Dec Jan Feb Mar Apr Year
2001/02 245 244 234
2000/01 242 162 193 343 308 293 284 279 276 264
1999/00 249 189 202 283 297 292 271 262 293 260
1998/99 241 200 218 305 278 288 289 273 279 263
1997/98 261 251 235 240 297 281 266 280 281 266
1957-72 310 330 345 370 345 320 300 295 310 325
b)
Radiosonde data. Radiosonde flights from Marambio and
Rothera show that the 100 hPa temperature is now close to the
normal. It was significantly below the normal in the second
half of October.
c)
Nacreous clouds were sighted at Vernadsky on July 27, 28, August
6, 10 ,13, 15, 28, 29 and September 4.
4. Information from other sources.
TOVS satellite images from the US NCEP/NWS/NOAA Climate
Prediction Center and EP/TOMS images from the US NASA/GSFC give a
global perspective on the ozone hole. TOVS and TOMS
currently have significantly different calibrations, with TOVS
reading some 30 DU higher than TOMS. TOMS values are close
to ground-based values. BAS have made ozone hole movies
from TOMS images, which are on our web page and are regularly
updated.
A low ozone event with central
values below 200 DU occurred on the edge of the sunlit polar
vortex between June 15 and June 28. The hole developed and
reached over 25 million square kilometres in mid September, but
is now shrinking and filling. The area remains
significantly larger than that of last year and by early November
was still around 18 million square kilometres. The hole is
past its deepest, and minimum values are now above 125 DU. The
edge of the ozone hole passed over the tip of South America, the
Falklands and South Georgia during the period from October 15 to
26.
NOAA analyses show that the 50 hPa
temperature was generally below the normal since early July and
that in some parts of Antarctica conditions are still suitable
for Type I PSC formation.
Further information is available on the BAS ozone web page, which
contains earlier bulletins, data, graphs and general ozone
information. It is often updated several times a week.
The email ozone bulletins will only be issued occasionally this
year so for the latest information see:
http://www.antarctica.ac.uk/met/jds/ozone
Note that all ozone values in this bulletin are preliminary and
are subject to revision from time to time when the instrument
constants are re-evaluated. Final data will be archived
with WOUDC, Toronto in due course, but preliminary data back to
1973 are available from BAS on request. All Dobson ozone
data are reduced to the Bass-Paur scale as recommended by the
WMO. The reference period used for the normals is 1957 -
1972. If you use or pass on data in this bulletin please
make acknowledgement to J D Shanklin, British Antarctic Survey.