Trace gas measurements at Hateruma station in 2018

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The present data set is time series of trace gases (ethane, propane, ozone, NO, NO2, NOy, and CO) and meteorological parameters measured at Hateruma Island, Japan. Hateruma is the southernmost inhabited island in Japan. It is approximately 250 km east of Taiwan and 500 km southwest of Okinawa Island. The prevailing winds at Hateruma are southeastely in summer and northwesterly in winter.

Description

Creator
Release date
2023/02/17
Temporal coverage
2018/01/01 - 2018/12/31
Data provider
NIES
Email: cgerdb_admin(at)nies.go.jp
DOI
File format
Data volume
1.80 MB
Version
ver.1.0 (Last updated: 2023/02/17)
Language
English

Data Set

Parameters
Ethane, propane, ozone, NO, NO2, NOy, CO, and meteorological parameters
Observation period
From Jan. 1, 2018 (ongoing)
Location   24.0608°N, 123.8093°E
Altitude   Elevation: 10.8 m
  Sampling height: 36.5 m above ground
Measurement
method
Measurements of CO, ethane, and propane were made with outside air drawn from a main tower (sampling inlet: 36.5 m above ground and 46.5 m above sea level). CO was measured with a gas chromatograph/reduction gas detector (GC/RGD; Peak Performer 2, Peak Laboratories) (Tohjima et al., 2014). Ethane and propane were measured with an automated preconcentration/gas chromatography/mass spectrometry (GC/MS) instrument (7890B/5977B, Agilent Technologies) designed for hourly measurements of natural and anthropogenic halocarbons (Yokouchi et al., 2006; Saito et al., 2010). Air for NO/NO2/NOy and O3 measurements were drawn from a sub tower (sampling inlet: 14.8 m above ground and 24.8m above sea level). Measurements of NO, NO2, and NOy were made by HSS-100 (Sonoma Technology Inc. (STI)) with a blue light converter for NO2 (NOx converter) and a molybdenum converter for NOy (NOy converter) (Galbally, 2020). Ozone concentration was observed by UV absorption method with an ozone monitor (Dylec 1100, Dylec Co., Ltd).
Calculation method
Ethane and propane measurements were calibrated using a gravimetrically prepared standard gas (Taiyo Nippon Sanso Co. Ltd.). The conversion efficiencies of the converters were daily monitored with NO2 gas (≈5 ppb) generated by a gas dilution system with gas phase titration (NOx: 79±3%, NOy: 98±1%). Detection limit of the NO measurement was about 2 ppt in 1 minute acquisition. The ozone monitor was calibrated with Standard Reference Photometer No. 35 (National Institute for Standard and Technology) located at NIES.
Keywords
[Free Keywords]
VOC,SLCP
[GCMD_Platform]
Land-based Platforms > Permanent Land Sites > GROIND STATIONS
[GCMD_Science]
EARTH SCIENCE > ATMOSPHERE > ATMOSPHERIC CHEMISTRY > CARBON AND HYDROCARBON COMPOUNDS > ATMOSPHERIC
CARBON MONOXIDE > CARBON MONOXIDE SURFACE
EARTH SCIENCE > ATMOSPHERE > ATMOSPHERIC CHEMISTRY >
CARBON AND HYDROCARBON COMPOUNDS > ETHANE
EARTH SCIENCE > ATMOSPHERE > ATMOSPHERIC CHEMISTRY >
CARBON AND HYDROCARBON COMPOUNDS > NON-METHANE
HYDROCARBONS/VOLATILE ORGANIC COMPOUNDS
EARTH SCIENCE > ATMOSPHERE > ATMOSPHERIC CHEMISTRY >
OXYGEN COMPOUNDS > ATMOSPHERIC OZONE > OZONE SURFACE
EARTH SCIENCE > ATMOSPHERE > ATMOSPHERIC CHEMISTRY >
NITROGEN COMPOUNDS > NITROGEN OXIDES
EARTH SCIENCE > ATMOSPHERE > ATMOSPHERIC CHEMISTRY >
NITROGEN COMPOUNDS > NITROGEN DIOXIDE
EARTH SCIENCE > ATMOSPHERE > ATMOSPHERIC TEMPERATURE
> SURFACE TEMPERATURE > AIR TEMPERATURE
EARTH SCIENCE > ATMOSPHERE > ATMOSPHERIC WINDS >
SURFACE WINDSWIND DIRECTION
EARTH SCIENCE > ATMOSPHERE > ATMOSPHERIC WATER VAPOR >
WATER VAPOR INDICATORS > HUMIDITY > RELATIVE HUMIDITY
EARTH SCIENCE > ATMOSPHERE > ATMOSPHERIC WINDS >
SURFACE WINDS > WIND SPEED
Update history
[2023/02/17]
Version 1.0 was released (ver.1.0)

Reference Information

References
Measurement report: Assessment of Asian emissions of ethane, propane, carbon monoxide, and NOx based on observations from the island of Hateruma, doi:10.5194/acp-2022-703.

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Saito T, Hashimoto S, Mukai H, Tanimoto H, Tohjima Y, and Sasakawa M (2023), Trace gas measurements at Hateruma station in 2018, Ver.x.x*1, NIES, DOI:10.17595/20230217.001. (Reference date*2: YYYY/MM/DD) 
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