BAS Ozone Bulletin 02/00


The 2000 ozone hole continues to shrink and fill. It is now centred over Dronning Maud Land and is strongly elliptical stretching towards the eastern Atlantic and towards George V Land. Ozone values have risen over Victoria Land and West Antarctica and strong stratospheric warming has taken place in this area. The ozone hole covers around 7 million square kilometres, near the lower limit for the time of year over the last decade. Central values are now above 160 DU. Lower stratospheric temperatures are now above -75°C throughout the continent. A broad collar of ozone rich air surrounds Antarctica. At its largest in early September the ozone hole reached 28.4 million square kilometres and was the largest ever recorded ozone hole. It also formed unusually early as it is normally late September before it reaches its maximum extent. Minimum ozone values were measured in early October and were amongst the lowest on record. The edge of the ozone hole passed over the tip of South America and the Falkland Islands for significant periods between October 6 and 24.

 

Satellite imagery gives a global perspective on the ozone hole. TOVS and TOMS currently have significantly different calibrations, with TOVS reading some 50 DU higher than TOMS. TOMS values are close to ground-based values. Our 2000/2001 ozone hole movie, produced from TOMS images, is generally updated every week. The temperature at 100 hPa, near the centre of the ozone layer, is now above -75°C over the entire continent but a few parts of the Antarctic stratosphere are still cold enough for stratospheric clouds to persist. The coldest area is centred over Dronning Maud Land. Strong warming has taken place over the Pacific sector of Antarctica and is beginning to occur at Halley. Stratospheric clouds were sighted from Vernadsky, Rothera and Halley. A mini ozone hole, with central values below 200 DU, periodically formed to the east of the Antarctic Peninsula over the Weddell Sea during July. This mini ozone hole probably formed due to processing of ozone through PSCs, which are far enough north to be sunlit. The feature was particularly marked on July 10 and again on July 20.

 

Ozone values over the Arctic are normally at their lowest in September and this year was no exception as can be see from the TOMS images. Although the values were low, they were low because of stratospheric dynamics and not chemistry. The temperature in the Arctic ozone layer was above -55°C, far too warm for stratospheric clouds to form. Hence there was no chemical depletion taking place and no ozone hole above the Arctic. In mid October there were regions of low ozone over Siberia. Stratospheric temperatures in this area are generally above -65°C, so again these features have a dynamic, not chemical origin.



1. Data from the British Antarctic Survey (BAS) Halley station (76-deg south, 27-deg west, on the Brunt ice shelf).

 

  1.  
  2. Ozone. Ozone measurements in the first half of August were made using moonlight and are of very low accuracy.


Halley preliminary mean daily total ozone, (DU)
Dobson No 103: Instrument constants revised 1999 October 8.
(0 indicates no data)


2000 August 1 - 2000 November 2

0 0 0 0 0 0 0 0 0 201

151 174 182 0 0 165 153 149 0 0

0 0 0 0 0 0 255 188 165 180 179

189 184 196 192 199 206 183 167 152 170

172 165 167 155 138 143 152 129 127 123

135 134 129 129 120 110 121 114 108 107

118 119 120 124 112 112 105 120 119 119

121 131 135 125 119 123 129 141 139 138

138 150 160 159 154 168 164 173 171 164 164

188 234


Halley provisional monthly mean total ozone (DU)


Period Aug Sep Oct Nov Dec Jan Feb Mar Apr Year
2000/01 179 151 137
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
1996/97 173 155 148 181 260 278 265 247 243 217
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.

  1.  
  2. Stratospheric clouds, which are instrumental in the mechanism of ozone depletion, were observed from the station on July 10, 12, August 2 and 22.



2. Data from the British Antarctic Survey (BAS) Rothera station (68-deg south, 68-deg west on Adelaide Island).

 

  1.  
  2. 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. The lowest values are around 105 DU once the 15% correction is applied to the measurements given below. 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.

  3. Rothera preliminary mean daily total ozone, (DU)
    (0 indicates no data or data not available)


    2000 July 1 - 2000 October 31


    273 249 276 0 0 288 236 205 144 173

    225 279 264 245 225 232 243 225 201 246

    225 178 213 201 225 233 245 0 242 220 246

    232 211 228 203 228 240 231 246 246 286

    298 252 226 217 238 241 0 0 188 196

    179 175 184 220 193 232 262 287 273 258 202

    195 208 193 184 187 162 127 111 114 108

    138 128 121 115 0 0 124 111 94 92

    104 119 101 98 111 120 110 127 198 225

    189 149 136 124 120 125 137 134 139 0

    0 105 100 112 117 110 104 114 119 130

    124 139 164 260 234 259 296 327 244 259 299


    Rothera provisional monthly mean total ozone (DU)


    Period Jul Aug Sep Oct Nov Dec Jan Feb Mar Apr May Jun
    2000/01 231 230 137 168
    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

  4. 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 they were observed from Rothera on June 23, 26, July 10, August 21 and 22.

 

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).

 

  1.  
  2. Ozone.

  3. Vernadsky preliminary mean daily total ozone (DU).
    Dobson No 31: Instrument constants revised 1999 October 25


    2000 August 1 - 2000 September 27


    255 245 265 236 248 263 252 246 246 286

    277 255 213 213 229 252 245 205 214 207

    198 192 204 238 196 219 258 291 316 298 242

    239 237 213 209 195 177 148 141 142 147

    164 138 130 145 141 164 160 133 119 118

    120 158 134 139 149 148 131 157 187 271

    259 245 225 169 161 160 156 158 187 139

    132 128 121 132 138 144 131 130 145 155

    144 149 180 240 269 260 304 358 292 285 297

    344


    Vernadsky provisional monthly mean total ozone (DU)


    Period Aug Sep Oct Nov Dec Jan Feb Mar Apr Year
    2000/01 242 162 193
    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
    1996/97 208 203 265 225 272 307 281 277 283 258
    1957-72 310 330 345 370 345 320 300 295 310 325

  4. Stratospheric clouds were seen from Vernadsky on June 19, July 8, 17, 18, 21, 26, August 4 and September 12, 21 and 22.



4. Information from other sources.


The use of data from TOVS satellite images from the US NCEP/NWS/NOAA Climate Prediction Center and EP/TOMS images is acknowledged.



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 be issued less frequently this year so for the latest information see: http://www.antarctica.ac.uk/met/jds/ozone The next bulletin will not be issued until late January.


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.