NO | 157 |
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Acronym | ATOMKI |
Name | Institute for Nuclear Research |
Address 1 | Bem tér 18/C |
Address 2 | H-4026 Debrecen, Hungary |
Address 3 | |
Country/Territory | Hungary |
Website | https://www.atomki.hu/en/ |
Name | Laszlo Haszpra |
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Prefix | Mr/Dr |
haszpra.l@gmail.com | |
Organization No | 157 |
Organization acronym | ATOMKI |
Organization name | Institute for Nuclear Research |
Organization country/territory | Hungary |
Address 1 | |
Address 2 | Bem tér 18/C |
Address 3 | H-4026 Debrecen, Hungary |
Country/territory | Hungary |
Tel | +36-30-454-3309 |
Fax | |
Last updated date | 2024-11-11 |
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Background observation | |||||||
UTC+01:00 | |||||||
ppm | |||||||
1994-09-01 00:00:00 - 2023-12-31 23:59:59: WMO CO2 X2019 |
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1994-09-01 00:00:00 - 2007-08-09 12:59:59: Li-Core Model LI-6251(NDIR) 2007-08-09 13:00:00 - 2020-02-20 23:59:59: Li-Cor Model LI-7000(NDIR) 2020-02-21 00:00:00 - 2023-12-31 23:59:59: Picarro Model G2301(CRDS) |
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1994-09-01 00:00:00 - 9999-12-31 23:59:59: 82 (m) |
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8 minutes | |||||||
1 September 1994 – 20 February 2020: Every 202 minutes a full four-point calibration is carried out using standards produced and certified by NOAA CMDL. The response function is calculated as a quadratic function. Every 32 minutes a target gas is measured. Between two 4-point calibrations, the response function is shifted following the drift of the target gas signal. From 21 February 2020: With the introduction of a high stability new analyzer the frequency of the 4-point calibration is reduced to one per month, and no target measurement is performed. The negligible drift of the response function is followed by linear interpolation between the calibrations. |
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The basic measurement period is two minutes, consisting of one-minute flushing and one-minute signal integration. Each one-minute average is based on 6-7 measurements. The multiport selector valve steps through the four monitoring elevation levels in eight minutes. Typically 7 data are recorded at each measurement elevation every hour. | |||||||
[Hourly] Hourly data are taken from the arithmetic mean of observed data for one hour after the technically bad data are rejected. [Daily] Daily data are calculated as the arithmetic mean of hourly data measured between 12 h and 16 h local standard time (early afternoon values having expanded spatial representativeness). [Monthly] Monthly data are calculated as the arithmetic mean of the daily (early afternoon) data if at least 10 daily data are available. |
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Operational/Reporting | |||||||
HMS was the operator of the station and performed the measurements between 1994 and 31 Aug 2020. Since 1 Sept 2020 ATOMKI is the operator of the station and it performs the reported measurements. Since 1 September ATOMKI handles the whole historic data series. The meteorological data observed by HMS from 1994 to 2018 are available in Yearly fixed datasets until 2021. https://gaw.kishou.go.jp/search/gas_species/co2/2021 |
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Wind direction: Wind speed: Relative humidity: Precipitation amount: Air pressure: Air temperature: Dew point temperature: Sea water temperature: Sea surface water temperature: Sea water salinity: Sea surface water salinity: |
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Meteorological data may remain as first provided, even when greenhouse gas data are updated. |
Format | Text (WDCGG Data Format Table, WDCGG Meteorological Data Format Table), NetCDF | ||||
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Relation List (Is Part Of) |
All CO2 data contributed to WDCGG by GAW stations and mobiles by 2024-09-24 All CO2 data contributed to WDCGG by GAW stations and mobiles by 2023-09-13 All CO2 data contributed to WDCGG by GAW stations and mobiles by 2022-09-07 |
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Geolocation Point |
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1 |
Haszpra, L., (1999), On the representativeness of carbon dioxide measurements. J. of Geophysical Research 104D, 26953-26960. Haszpra, L., et al., (2001) , Measuring system for the long-term monitoring of biosphere/atmosphere exchange of carbon dioxide , Journal of Geophysical Research , 106D , 3057--3070 . Haszpra, L., et al., (2005) , Long term tall tower carbon dioxide flux monitoring over an area of mixed vegetation , Agricultural and Forest Meteorology , 132 , 58-77. Haszpra, L., et al., (2008) , Trends and temporal variations of major greenhouse gases at a rural site in Central Europe. , Atmospheric Environment , 42 , 8707--8716 . Haszpra, L., et al., (2015) , How well do tall-tower measurements characterize the CO2 mole fraction distribution in the planetary boundary layer? , Atmos. Meas. Tech. , 8 , 1657-1671 . |
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