Data

Observations collected aboard Aurora Australis by AIRBOX and associated instruments – 2017-18 Season

Australian Antarctic Data Centre
SCHOFIELD, ROBYN ; RYAN, ROBERT GEORGE
Viewed: [[ro.stat.viewed]] Cited: [[ro.stat.cited]] Accessed: [[ro.stat.accessed]]
ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Adc&rfr_id=info%3Asid%2FANDS&rft_id=info:doi10.26179/5e54ab5e5d56f&rft.title=Observations collected aboard Aurora Australis by AIRBOX and associated instruments – 2017-18 Season&rft.identifier=10.26179/5e54ab5e5d56f&rft.publisher=Australian Antarctic Data Centre&rft.description=More information about these data is available in the word document in the download file. It is recommended that potential users of these data read this document before proceeding. MAX-DOAS This dataset comprises chiefly of solar scattered light spectra (level zero product) collected using a MAX-DOAS instrument. The MAX (Mult-Axis) refers to the fact that spectra are collected in a 'set' of elevation angle scans (-3, -2, -1, 0, 1, 2, 3, 5, 10, 20, 40, 90 deg). The DOAS (differential optical absorption spectroscopy) refers to the analysis method required for analysis of the scattered light spectra. Briefly, analysis of these spectra relies on fitting absorption cross sections of trace gases of interest to determine the amount of trace gas integrated along the scattered light path, for each elevation angle in each set, using an appropriate fitting algorithm. This gives the slant column density for each trace gas at each elevation angle (level one product). The differential slant column density (dSCD) is determined by taking the ratio of low elevation angle scans with zenith scans, producing tropospheric specific information. Typically some atmospheric corrections are required to be included in the analysis including a polynomial, which accounts for broadband absorption and scattering processes, and corrections for the filling in of solar Fraunhofer lines (the Ring effect). By inverting measured dSCDs, and dSCDS modelled using a radiative transfer model, vertical profile information for trace gases can be calculated using MAX-DOAS observations. Finally, since knowing the elevation angle precisely is crucial to retrieval of vertical profile information from MAX-DOAS measurements, this dataset also includes Euler angles measured using a co-located accelerometer which may, if necessary, be used to correct MAX-DOAS elevation angles for the pitch and roll of the ship in the Southern Ocean. MAX-DOAS instrument specifications: Two ultra-low straylight 75mm Avantes spectrometers: UV: 295 – 450nm, 100 μm m slit (from fibre), 0.6nm resolution, Hamamatsu backthinned detector optimized for UV, Schott BG3 filter. Visible: 430 – 565nm, 100 μ m slit (from fibre), 0.6nm resolution, Sony 2048L detector Typical instrumental stray light less than 0.05% , RMS of 1 · 10−4 (vis) and 2 · 10−4 (uv) for 1000 scans around noon. Spectrometers temperature stabilized at a fixed temperature (20 C) with a deviation of less than 0.05 C Elevation angle accuracy less than 0.1 Telescope field of view (opening angle) less than 0.3 MAX-DOAS Data details: Spectra: one binary file per spectrum. Spectra can be processed using DOASIS or QDOAS software. Spectrum files are saved in folders numbered by date. Daily log files: for spectra (extra geometric information as well as latitude, longitude, solar zenith angle) and temperature (instrument, internal and external temperature measurements). Accelerometer: One ascii file per day with pitch, roll and yaw euler angles as the columns Images: taken by a small camera, co-directional with the MAX-DOAS, for context of broad light conditions (i.e. checking sunny/cloudy weather) Calibration files: Binary and text files for dark current, offset, slit function shape and wavelength calibrations Other instruments/datasets detailed in the file: Gaseous oxidised mercury measurements Gaseous elemental mercury mini-MPL (micropulse lidar) &rft.creator=SCHOFIELD, ROBYN &rft.creator=RYAN, ROBERT GEORGE &rft.date=2020&rft.coverage=northlimit=-42.882; southlimit=-68.576; westlimit=62.867; eastLimit=158.856; projection=WGS84&rft.coverage=northlimit=-42.882; southlimit=-68.576; westlimit=62.867; eastLimit=158.856; projection=WGS84&rft_rights=This data set conforms to the CCBY Attribution License (http://creativecommons.org/licenses/by/4.0/). Please follow instructions listed in the citation reference provided at http://data.aad.gov.au/aadc/metadata/citation.cfm?entry_id=AAS_4431_CAMMPCAN_AIRBOX_2017-2018 when using these data.&rft_subject=TRACE GASES/TRACE SPECIES&rft_subject=EARTH SCIENCE&rft_subject=ATMOSPHERE&rft_subject=ATMOSPHERIC CHEMISTRY&rft_subject=EARTH SCIENCE > ATMOSPHERE > AEROSOLS > CHEMICAL COMPOSITION&rft_subject=AEROSOL BACKSCATTER&rft_subject=AEROSOLS&rft_subject=CAMMPCAN&rft_subject=AIRBOX&rft_subject=MPL > Micropulse Lidar&rft_subject=MERCURY ANALYZERS&rft_subject=AIR-ION > AIR-ION SPECTROMETER&rft_subject=R/V AA > R/V Aurora Australis&rft_subject=OCEAN > SOUTHERN OCEAN&rft_subject=CONTINENT > ANTARCTICA&rft_subject=GEOGRAPHIC REGION > POLAR&rft_place=Hobart&rft.type=dataset&rft.language=English Access the data

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This data set conforms to the CCBY Attribution License (http://creativecommons.org/licenses/by/4.0/). Please follow instructions listed in the citation reference provided at http://data.aad.gov.au/aadc/metadata/citation.cfm?entry_id=AAS_4431_CAMMPCAN_AIRBOX_2017-2018 when using these data.

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These data are publicly available for download from the provided URL.

Brief description

More information about these data is available in the word document in the download file. It is recommended that potential users of these data read this document before proceeding.

MAX-DOAS
This dataset comprises chiefly of solar scattered light spectra (level zero product) collected using a MAX-DOAS instrument. The MAX (Mult-Axis) refers to the fact that spectra are collected in a 'set' of elevation angle scans (-3, -2, -1, 0, 1, 2, 3, 5, 10, 20, 40, 90 deg). The DOAS (differential optical absorption spectroscopy) refers to the analysis method required for analysis of the scattered light spectra.
Briefly, analysis of these spectra relies on fitting absorption cross sections of trace gases of interest to determine the amount of trace gas integrated along the scattered light path, for each elevation angle in each set, using an appropriate fitting algorithm. This gives the slant column density for each trace gas at each elevation angle (level one product). The differential slant column density (dSCD) is determined by taking the ratio of low elevation angle scans with zenith scans, producing tropospheric specific information. Typically some atmospheric corrections are required to be included in the analysis including a polynomial, which accounts for broadband absorption and scattering processes, and corrections for the filling in of solar Fraunhofer lines (the Ring effect).
By inverting measured dSCDs, and dSCDS modelled using a radiative transfer model, vertical profile information for trace gases can be calculated using MAX-DOAS observations.
Finally, since knowing the elevation angle precisely is crucial to retrieval of vertical profile information from MAX-DOAS measurements, this dataset also includes Euler angles measured using a co-located accelerometer which may, if necessary, be used to correct MAX-DOAS elevation angles for the pitch and roll of the ship in the Southern Ocean.

MAX-DOAS instrument specifications:
Two ultra-low straylight 75mm Avantes spectrometers: UV: 295 – 450nm, 100 μm m slit (from fibre), 0.6nm resolution, Hamamatsu backthinned detector optimized for UV, Schott BG3 filter. Visible: 430 – 565nm, 100 μ m slit (from fibre), 0.6nm resolution, Sony 2048L detector
Typical instrumental stray light less than 0.05% , RMS of 1 · 10−4 (vis) and 2 · 10−4 (uv) for 1000 scans around noon.
Spectrometers temperature stabilized at a fixed temperature (20 C) with a deviation of less than 0.05 C
Elevation angle accuracy less than 0.1
Telescope field of view (opening angle) less than 0.3


MAX-DOAS Data details:
Spectra: one binary file per spectrum. Spectra can be processed using DOASIS or QDOAS software. Spectrum files are saved in folders numbered by date.
Daily log files: for spectra (extra geometric information as well as latitude, longitude, solar zenith angle) and temperature (instrument, internal and external temperature measurements).
Accelerometer: One ascii file per day with pitch, roll and yaw euler angles as the columns
Images: taken by a small camera, co-directional with the MAX-DOAS, for context of broad light conditions (i.e. checking sunny/cloudy weather)
Calibration files: Binary and text files for dark current, offset, slit function shape and wavelength calibrations

Other instruments/datasets detailed in the file:
Gaseous oxidised mercury measurements
Gaseous elemental mercury
mini-MPL (micropulse lidar)

Issued: 2020-02-25

Data time period: 2017-10-21 to 2018-03-23

This dataset is part of a larger collection

Click to explore relationships graph

158.856,-42.882 158.856,-68.576 62.867,-68.576 62.867,-42.882 158.856,-42.882

110.8615,-55.729

text: northlimit=-42.882; southlimit=-68.576; westlimit=62.867; eastLimit=158.856; projection=WGS84

Other Information
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