Metadata about the BAS ozone data

General

A paper describing the instrument meta data and observations is in preparation.  

ThedatashouldbecreditedtoJDShanklin, BritishAntarctic Survey, Madingley Road, Cambridge, England. CB3 0ET

Station names:  

Faraday .  65°15'S, 64°16'W.  Originally known as Argentine Islands (which is actually a group of islands off the coast of the Antarctic Peninsula) the station became known as Faraday in the mid 1970s.  In 1996 it was handed over to the Ukraine and its name changed to Vernadsky.  In publications, the name Faraday should be used when referring to data prior to 1996 and Faraday/Vernadsky thereafter.
Halley .  75°35'S, 26°36'W.  Please note that the station name is Halley and this should be used in all publications.  The geographical feature known as Halley Bay (which the station was called when first set up in 1956) no longer exists.  The station is on a floating ice-shelf and moves over time.  The position given is the current one, but the actual location is likely to be within 15km of this.
King Edward Point.   54°16'S, 36°30'W.  The station at King Edward Point is near Grytviken, in Cumberland Bay, South Georgia.  Observations ceased due to military action in 1982 April.
Rothera.   67°34'S, 68°08'W.  The name Rothera should be used in publications.  The SAOZ instrument can make observations throughout the year.

 

Observing season


Mu    

  King Edward Point 

   Faraday   

   Halley

2.0    

  Sep 07 - Apr 05    

   Oct 06 - Mar 08    

    Nov 04 - Feb 07

2.6    

  Aug 17 - Apr 26    

   Sep 15 - Mar 27    

   Oct 13 - Mar 01

3.2    

  Aug 01 - May 11    

   Sep 04 - Apr 08    

    Oct 01 - Mar 12

3.8    

  Jul 17 - May 26    

    Aug 27 - Apr 16    

   Sep 23 - Mar 20

4.4    

  Jun 25 - Jun 17    

    Aug 20 - Apr 23    

   Sep 18 - Mar 26

5.0    

  All year    

    Aug 15 - Apr 28    

    Sep 13 - Mar 30

5.6    

  All Year    

   Aug 10 - May 02    

   Sep 09 - Apr 03

6.2    

  All year    

   Aug 06 - May 06    

   Sep 06 - Dec 07

   

   

   

    Jan 04 - Apr 06

6.8    

  All year    

   Aug 03 - May 10    

   Sep 04 - Nov 30

   

   

   

    Jan 12 - Apr 08

7.4    

  All year    

   Jul 30 - May 13    

    Sep 02 - Nov 25

   

   

   

   Jan 17 - Apr 10

8.0    

  All year    

   Jul 28 - May 16    

   Aug 30 - Nov 22

   

   

   

    Jan 20 - Apr 12

8.6    

  All year    

   Jul 24 - May 19    

   Aug 29 - Nov 19

   

   

   

   Jan 23 - Apr 14

9.2    

  All year    

   Jul 21 - May 22    

  Aug 27 - Nov 16    

   

   

   

   Jan 26 - Apr 16

Approximate value of mu at Local Apparent Noon


Date
King Edward Point
Faraday
Halley
Jan 1
1.17
1.35
1.63
Jan 16
1.19
1.39
1.71
Feb 1
1.25
1.48
1.88
Feb 15
1.33
1.62
2.14
Mar 1
1.45
1.85
2.6
Mar 16
1.63
2.21
3.5
Apr 1
1.91
2.8
5.3
Apr 15
2.25
3.7
8.8
May 1
2.8
5.4
Sun below horizon
May 16
3.4
7.9
Sun below horizon
Jun 1
4.0
10.9
Sun below horizon
Jun 15
4.4
12.1
Sun below horizon
Jul 1
4.3
11.9
Sun below horizon
Jul 16
3.9
10.2
Sun below horizon
Aug 1
3.2
7.1
Sun below horizon
Aug 16
2.6
4.9
12.5
Sep 1
2.15
3.4
7.6
Sep 15
1.84
2.7
4.7
Oct 1
1.59
2.12
3.2
Oct 16
1.42
1.80
2.5
Nov 1
1.30
1.58
2.05
Nov 15
1.23
1.46
1.83
Dec 1
1.18
1.37
1.68
Dec 16
1.17
1.34
1.63
Minimum 
1.16
1.34
1.62

Instruments


Dobson number
Calibration
Location
Start
End
031
A
Halley
1956 September 17
1962 December
 
B
Faraday
1964 January
1967 February
 
C
Halley
1968 February
1982 January 23
 
D
Faraday/Vernadsky
1983 March 19
2005 March 29
 
E (Modern electronics)
Cambridge
Used for training
 
073
B
Halley
1965 March
1967 December
 
C
Faraday
1970 January
1984 December 20
 
D (Modern electronics)
Halley
2005 December 24
In use
103
A
Faraday
1967 February
1970 January
 
B
King Edward Point
1971 March 10
1982 April 1
 
C
Halley
1992 December 27
2005 December 31
 
D (Modern electronics)
Cambridge
Not deployed
 
123
A
Halley
1981 December 24
1992 January 10
 
C (Modern electronics)
Vernadsky
2005 March 27
In use
 
 
 
 
 
SAOZ number
 
Location
Start
End
6
 
Faraday
1990
1996
6
 
Rothera
1996 January 6
2008 January 22
29
 
Rothera
2006 December 7
In use
31
 
Rothera
Spare
 
30
 
Cambridge
Spare
 

   

Datasets - ozone

All observations at Halley and Vernadsky are made with the Dobson ozone spectrophotometer.

Observations with Dobson 103  (with valve electronics and mechanical commutator) ceased at Halley on 2005 December 26 and observations with Dobson 73 (with modern electronics) commenced on 2005 December 24.  The short overlap period allowed the instrument constants for both instruments to be slightly adjusted.  Observations with Dobson 31 (with valve electronics and mechanical commutator) ceased at Vernadsky on 2005 March 29 and observations with Dobson 123 (with modern electronics) commenced on 2005 March 27.    The short overlap period allowed the instrument constants for both instruments to be slightly adjusted.  During the overlap periods a mean of both instruments is given.  Ozone values from both the refurbished Dobsons are likely to undergo frequent revision until the instrument constants are well determined.  Ozone values from the old instruments are also likely to undergo revisions following both the on-site intercomparisons, and intercomparisons at Hoenpeissenberg.

Daily
The daily data sets are divided into seasonal blocks starting on August 1st each year and ending on 30th April.  They contain the provisional ozone data for 1972 - 2005  obtained using the Dobson ozone spectrophotometer. The definitive instrument and zenith calibration values have not yet been determined. A daily mean value is given, using all the observations for that day, assigning equal weight to each. The final daily values may differ from those given here, but should not differ from them by more than 5%.  A few moon observations which have been carried out outside this period are not included in this data set, but are available on request. A value of 0 indicates that no measurement was made on that day. Some experimental zenith observations at low solar elevations are included from April 1993 onwards, these have lower accuracies than normal observations. The Halley data for 1987/88 includes the results from ozonesonde flights.
Monthly
The monthly data sets run from August to April.  Data for 1957 - 1972 was published in BAS Scientific Report No 90 in 1975 and used ozone absorption coefficients determined by Powell, which are the same as those of Vigroux for AD, but are otherwise different.  These ozone values have been approximately corrected to the Bass-Pauer coefficients using the WMO recommended factor of 0.9743.  Note that this correction factor is for the US Standard Atmosphere, however the Antarctic atmosphere is some way from this and the correction could be improved.  Data after this period is reduced using the standard Bass-Pauer coefficients as published in Komhyr et al.
Rothera
The SAOZ instrument at Rothera measured total column nitrogen dioxide and ozone from 1997 to 2007. The values given here are preliminary and only show general trends in ozone amounts.  In particular, the calibration of the instrument is such that it reads about 10% lower than a Dobson at values around 100 DU.  A new SAOZ type instrument was installed during the 2006/7 season and it became the operational instrument from 2008 January 1.  The instrument constants for the new SAOZ were revised in mid July 2008, and previously published values were increased by about 2%.  Following a station power cut in mid June 2011, some data was lost and when data recording resumed an incorrect time was recorded.  This has been corrected, however the data between 2011 June 16 and 2011 June 29 may contain residual errors.

There is also a Bentham spectro-radiometer at Rothera, which can be used to compute ozone levels.  The original instrument was destroyed in a fire on 2001 September 28, however a replacement was commissioned and became operational on 2003 March 3.  For further information on this data set and permission to use it please contact Paul Geissler at BAS.  All values have been updated to the TOMS 8 algorithm.  The uv data is available from the WOUVDC.

 

Datasets - temperature

The 70 hPa pressure level is close to the height of the maximum ozone concentration, however this was not always reached by balloons.  The 100 hPa level is therefore used as a reference. Over the last 30 years the mean 100 hPa temperature has declined in most months. The most notable change is in November at Halley.

Halley   Radiosondes are released daily at Halley.  The sonde type changed from Vaisala RS80 to Vaisala RS92 in 2006 January.
Antarctic Peninsula    The record is a composite from several stations and the balance has changed with time.  Currently, there are flights from Marambio as part of a spring-time ozone sonde campaign, however these do not always get onto the GTS.  The Polarstern was stationed in the western Weddell Sea from early December 2004 to early January 2005 and launched one or two sondes each day; when in the area her routine flights are included.  There have been a few ozone sonde flights from Ferraz, but these have not been included in the record as they were not distributed on the GTS.  No sondes are currently launched at Bellingshausen or Vernadsky.      Vaisala RS92 radiosondes are currently released four times a week at Rothera and these form the primary contribution to the record.  There has been a radiosonde programme of several flights per week at Rothera since 2003 March, increasing to daily flights for the QUOBI project from mid June to mid October 2003.  Strong winds on 2004 October 2 & 3 damaged the hangar at Rothera and this significantly restricted the conditions under which sondes could be launched.  Sonde type changed from RS80 to RS92 in 2007.  A new launch facility become operational in 2007, and the processing system was upgraded from an MW15 to an MW31 in 2008 January, though this failed during the winter and flight control has reverted to the MW15. 

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