Atmospheric aerosol and Cloud Condensation Nuclei concentrations from Macquarie Island from 2016 to 2018.

Ambient aerosol data, including condensation nuclei larger than 10 nm (CN10) and cloud condensation nuclei at a range of supersaturations, were collected in the clean air laboratory at the Australian research station on Macquarie Island located in the Southern Ocean. Data from two instruments are re...

Full description

Bibliographic Details
Main Authors: Humphries, Ruhi, Ward, Jason, Keywood, Melita, Alexander, Simon
Format: Dataset
Language:unknown
Published: CSIRO 2021
Subjects:
Online Access:https://dx.doi.org/10.25919/ete8-3t69
https://data.csiro.au/collections/collection/CIcsiro:53051v1/DItrue
id ftdatacite:10.25919/ete8-3t69
record_format openpolar
spelling ftdatacite:10.25919/ete8-3t69 2023-05-15T17:09:58+02:00 Atmospheric aerosol and Cloud Condensation Nuclei concentrations from Macquarie Island from 2016 to 2018. Humphries, Ruhi Ward, Jason Keywood, Melita Alexander, Simon 2021 https://dx.doi.org/10.25919/ete8-3t69 https://data.csiro.au/collections/collection/CIcsiro:53051v1/DItrue unknown CSIRO https://data.aad.gov.au/metadata/records/Antarctic_Meteorology dataset Dataset 2021 ftdatacite https://doi.org/10.25919/ete8-3t69 2022-02-08T13:43:19Z Ambient aerosol data, including condensation nuclei larger than 10 nm (CN10) and cloud condensation nuclei at a range of supersaturations, were collected in the clean air laboratory at the Australian research station on Macquarie Island located in the Southern Ocean. Data from two instruments are reported in this dataset: - TSI CPC 3772 – measures the total number concentration of aerosols with diameters larger than 10 nm (CN10) - DMT CCNC-100 – measures the total number concentration of cloud condensation nuclei at specified supersaturations as determined by the user. Sample air was drawn into the clean air laboratory through a sample inlet positioned 1.5 m above the roofline (~4 m above ground level). The sample line was a bespoke design with a TSP (Total Suspended Particles) weather hat mounted atop a vertical 3” stainless tubing which provided both protection and vertical stability in the high wind environment. Through a bored-out Swagelok bulkhead fitting, ¾” stainless steel tubing penetrated to the height of the weather hat. The weather hat had 3 tie-down holes for guy wires to be attached for stabilisation. The top metre of the inlet, together with the weather hat were heated continuously to prevent icing with self-regulating heater tape designed to prevent ice build-up on commercial walk-in freezer doors. Heater tape was covered in insulation and then weather and UV-proof heat-shrink. The ¾” tubing that penetrated through the roof was connected inside the lab to a PM2.5 very sharp cut cyclone (VSCC), with a bypass flow set by a mass flow controller to be 16.67 LPM moving through the VSCC. Both the CCNC and CPC sampled air off the bypass flow at flow rates of 0.5 LPM and 1.0 LPM, respectively. Once quality controlled, CPC concentration data were resampled from 1 Hz to an hourly timebase, with various statistics calculated and presented including: • cn_med – median CN number concentration (units cm-3) • cn_mad – median absolute deviation of CN (units cm-3) • cn_avg – mean CN number concentration (units cm-3) • cn_std – standard deviation of CN (units cm-3) • cn_count – number of 1 Hz sample points used to calculate statistics (no units) The CCNC was run on a regular supersaturation schedule, set to change between 0.2, 0.4, 0.5, 0.6, 0.8 and 1.0% supersaturation every 10 minutes, resulting in a full supersaturation spectra every hour. After correcting for calibration pressures, all of these supersaturations increased by 0.0504%. After resampling from 1Hz data, for each supersaturation (0.x504), the following statistics were reported for each hour: • ccn_0.x504_med – median CN number concentration (units cm-3) • ccn_0.x504_mad– median absolute deviation of CN (units cm-3) • ccn_0.x504_avg – mean CN number concentration (units cm-3) • ccn_0.x504_std – standard deviation of CN (units cm-3) • ccn_0.x504_count – number of 1 Hz sample points used to calculate statistics (no units) Merged dataset The final dataset reports both CCN and CN hourly statistics, with variables from each instrument stated above, using UTC+10 time zone. Data are provided as both hdf and csv files. For hdf files, the required key to access the data is ”data”. Dataset Macquarie Island Southern Ocean DataCite Metadata Store (German National Library of Science and Technology) Southern Ocean
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
description Ambient aerosol data, including condensation nuclei larger than 10 nm (CN10) and cloud condensation nuclei at a range of supersaturations, were collected in the clean air laboratory at the Australian research station on Macquarie Island located in the Southern Ocean. Data from two instruments are reported in this dataset: - TSI CPC 3772 – measures the total number concentration of aerosols with diameters larger than 10 nm (CN10) - DMT CCNC-100 – measures the total number concentration of cloud condensation nuclei at specified supersaturations as determined by the user. Sample air was drawn into the clean air laboratory through a sample inlet positioned 1.5 m above the roofline (~4 m above ground level). The sample line was a bespoke design with a TSP (Total Suspended Particles) weather hat mounted atop a vertical 3” stainless tubing which provided both protection and vertical stability in the high wind environment. Through a bored-out Swagelok bulkhead fitting, ¾” stainless steel tubing penetrated to the height of the weather hat. The weather hat had 3 tie-down holes for guy wires to be attached for stabilisation. The top metre of the inlet, together with the weather hat were heated continuously to prevent icing with self-regulating heater tape designed to prevent ice build-up on commercial walk-in freezer doors. Heater tape was covered in insulation and then weather and UV-proof heat-shrink. The ¾” tubing that penetrated through the roof was connected inside the lab to a PM2.5 very sharp cut cyclone (VSCC), with a bypass flow set by a mass flow controller to be 16.67 LPM moving through the VSCC. Both the CCNC and CPC sampled air off the bypass flow at flow rates of 0.5 LPM and 1.0 LPM, respectively. Once quality controlled, CPC concentration data were resampled from 1 Hz to an hourly timebase, with various statistics calculated and presented including: • cn_med – median CN number concentration (units cm-3) • cn_mad – median absolute deviation of CN (units cm-3) • cn_avg – mean CN number concentration (units cm-3) • cn_std – standard deviation of CN (units cm-3) • cn_count – number of 1 Hz sample points used to calculate statistics (no units) The CCNC was run on a regular supersaturation schedule, set to change between 0.2, 0.4, 0.5, 0.6, 0.8 and 1.0% supersaturation every 10 minutes, resulting in a full supersaturation spectra every hour. After correcting for calibration pressures, all of these supersaturations increased by 0.0504%. After resampling from 1Hz data, for each supersaturation (0.x504), the following statistics were reported for each hour: • ccn_0.x504_med – median CN number concentration (units cm-3) • ccn_0.x504_mad– median absolute deviation of CN (units cm-3) • ccn_0.x504_avg – mean CN number concentration (units cm-3) • ccn_0.x504_std – standard deviation of CN (units cm-3) • ccn_0.x504_count – number of 1 Hz sample points used to calculate statistics (no units) Merged dataset The final dataset reports both CCN and CN hourly statistics, with variables from each instrument stated above, using UTC+10 time zone. Data are provided as both hdf and csv files. For hdf files, the required key to access the data is ”data”.
format Dataset
author Humphries, Ruhi
Ward, Jason
Keywood, Melita
Alexander, Simon
spellingShingle Humphries, Ruhi
Ward, Jason
Keywood, Melita
Alexander, Simon
Atmospheric aerosol and Cloud Condensation Nuclei concentrations from Macquarie Island from 2016 to 2018.
author_facet Humphries, Ruhi
Ward, Jason
Keywood, Melita
Alexander, Simon
author_sort Humphries, Ruhi
title Atmospheric aerosol and Cloud Condensation Nuclei concentrations from Macquarie Island from 2016 to 2018.
title_short Atmospheric aerosol and Cloud Condensation Nuclei concentrations from Macquarie Island from 2016 to 2018.
title_full Atmospheric aerosol and Cloud Condensation Nuclei concentrations from Macquarie Island from 2016 to 2018.
title_fullStr Atmospheric aerosol and Cloud Condensation Nuclei concentrations from Macquarie Island from 2016 to 2018.
title_full_unstemmed Atmospheric aerosol and Cloud Condensation Nuclei concentrations from Macquarie Island from 2016 to 2018.
title_sort atmospheric aerosol and cloud condensation nuclei concentrations from macquarie island from 2016 to 2018.
publisher CSIRO
publishDate 2021
url https://dx.doi.org/10.25919/ete8-3t69
https://data.csiro.au/collections/collection/CIcsiro:53051v1/DItrue
geographic Southern Ocean
geographic_facet Southern Ocean
genre Macquarie Island
Southern Ocean
genre_facet Macquarie Island
Southern Ocean
op_relation https://data.aad.gov.au/metadata/records/Antarctic_Meteorology
op_doi https://doi.org/10.25919/ete8-3t69
_version_ 1766066350399160320