Metadata Report for BODC Series Reference Number 953317
Metadata Summary
Problem Reports
Data Access Policy
Narrative Documents
Project Information
Data Activity or Cruise Information
Fixed Station Information
BODC Quality Flags
SeaDataNet Quality Flags
Metadata Summary
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Time Co-ordinates(UT) |
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Parameters |
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Problem Reports
No Problem Report Found in the Database
Data Quality Report
No problems with data quality were reported by the data originator, or identified by BODC.
Data Access Policy
Public domain data
These data have no specific confidentiality restrictions for users. However, users must acknowledge data sources as it is not ethical to publish data without proper attribution. Any publication or other output resulting from usage of the data should include an acknowledgment.
The recommended acknowledgment is
"This study uses data from the data source/organisation/programme, provided by the British Oceanographic Data Centre and funded by the funding body."
Narrative Documents
GRIMM 1.108 Aerosol Spectrometer
The GRIMM 1.108 Aerosol Spectrometer is a small, portable unit used for the continuous measurement of aerosols. Measurements are determined in either particle counts per unit volume, or mass per unit volume.
Ambient air is drawn into the instrument by a volume controlled pump, at 1.2 L min-1. Particles are size classified by a Differential Mobility Analyser (DMA), then counted by an Optical Particle Counter (OPC). The DMA neutralises the electrostatic charges of incoming particles, then imparts a charge to them. In the electrical field of the classifier, the particle trajectory is determined by the charge/mass ratio. Only particles within a narrow size range have the trajectory to exit the classifier to the OPC. As sequential size classes are counted, they are deposited on a 47 mm PTFE filter. The entire sample is deposited on the filter, which may be removed for subsequent gravimetric or chemical analysis.
Instrument specifications
Particle size bounds | 0.23/0.30/0.40/0.50/0.65/0.80/1.0/1.6/2.0/3.0/4.0/5.0/7.5/10/15/20 µm |
Count range | 1 to 2,000,000 l-1 |
Mass range | 0.1 to 100,000 µg m-3 |
Size channels | 16 channel sizes, mass in µg m-3, and l-1 |
Count range | 1 to 2,000,000 counts per filter |
Sample flow rate | 1.2 l min-1, flow controlled |
Reproducibility | ± 2 % |
Filter size | 47 mm |
Operating temperature range | 4 °C to 45 °C |
Physical parameters
Dimensions | 24 x 12 x 6 cm |
Weight | 2.4 kg |
Input/Output | 1 x RS 232, 3 x analogue |
Power Requirements | Battery or 110/220 VAC with external power supply |
Further details can be found on the manufacturer's website.
Instrument Description
Manchester Centre for Atmospheric Science (CAS) Differential Mobility Particle Sizer (DMPS)
The Manchester Centre for Atmospheric Science (CAS) Differential Mobility Particle Sizer (DMPS) measures aerosol particle size distributions. The instrument comprises two differential mobility analysers (DMA, Winklmayer et al., 1991), each with a condensation particle counter. Each DMA-CPC pairing is equipped to select particles within a different size range: ultrafine 3.4-34 nm; standard 30-830 nm. The DMA selects charged particles for detection as a function of their mobility in an electric field. Successive size fractions are counted by CPC. The DMPS returns a size/particle count spectrum every 10 minutes during sampling.
The ultrafine DMA is attached to a TSI 3025A ultrafine CPC (particle detection limit 50% at 3 nm). The standard DMA is attached to aTSI 3010 CPC (particle detection limit 50% at 10 nm).
References
Winklmayer W., Reischl G.P., Lindner A.O., Berner A., 1991. A new electromobility spectrometer for the measurement of aerosol size distributions in the size range from 1 to 1000 nm, Journal of Aerosol Science, 22, 289-296.
Instrument Description
GRIMM Optical Particle Counter
A GRIMM Optical Particle Counter (OPC) was used to resolve coarse aerosol particles. The GRIMM OPC, model 1.108, optically sizes particles in the range 0.3 µm to 20 µm. The instrument produces a particle size histogram every 6 seconds, using the intensity and angle of scattered light to size the particles.
Aerosol Properties Sampling
The University of Manchester deployed a suite of instruments to measure aerosol properties on D319. Wet and dry aerosol size spectra were measured by a combination of Differential Mobility Particle Sizers and an Optical Particle Counter. Online aerosol particle composition was determined by Aerodyne Aerosol Mass Spectrometer, and by Multi Angle Aerosol Photometer. Aerosol particle growth factors were measured by a Hygroscopicity Tandem Differential Mobility Analyser. A combination of samplers was used for the offline analysis of aerosol particle composition: a four stage Harvard compact cascade impactor, and an Anderson high-volume sampler.
Atmospheric aerosols were sampled throughout the D319 cruise through a 10 m vertical inlet stack mounted on the forecastle deck. Air was drawn in though a 2.5 µm cutoff cyclone, and distributed to the instruments listed above through a horizontal manifold, using isokinetic sampling ports.
BODC Data Processing
Data were received by BODC in tab separated ASCII format (D319_ambient_aerosol_dist_v1_1.txt). This file included date and time, aerosol size spectra, and three derived parameters: aerosol total number concentration; aerosol total surface area concentration; and aerosol total volume concentration. The derived parameters were calculated as sums across all size bins, assuming spherical particles of diameter equal to the middle of the range for that bin. The derived parameters have not been banked in the BODC database, but the original data file containing these variables is available on request.
No position data were supplied with the DMSP data. Latitude and longitude position were merged into the data file, by BODC, from the screened and processed cruise navigation file, matching on time.
Bin sizes were defined in a separate file: Aerosol_d_bins_v1.txt. The file specified lower and upper bounds for each size category. There were 64 size bins, between 10 nm and 10000 nm, evenly distributed in log diameter space. Note that the BODC parameter is defined by its upper bound only. The lower bound for each bin is the upper bound of the next, smaller, size category, or zero nm in the case of the smallest size category.
Parameter codes defined in the BODC parameter dictionary were mapped to the variables as follows:
Orginator's Parameter | Units | Description | BODC Parameter Code | Units | Comments |
---|---|---|---|---|---|
Latitude | Degrees | Latitude north (WGS84) by unspecified GPS system | ALATGP01 | Degrees | Merged from navigation file by BODC |
Longitude | Degrees | Longitude east (WGS84) by unspecified GPS system | ALONGP01 | Degrees | Merged from navigation file by BODC |
Aerosol size spectra | ml-1 | Concentration of particles per unit volume of the atmosphere ambient air [aerosol phase] by particle sizer | OPCAAER1 | ml-1 | n/a |
Aerosol size bin | nm | Size class maximum size (equivalent spherical diameter) by particle sizer | OPCABIN1 | nm | n/a |
The data were banked according to BODC standard procedures for series data. Once tagged with the appropriate parameter code, the data were loaded into BODC Series Database.
Originator's Data Processing
Two differential mobility particle sizers (DMPS) were run in parallel during the deployment: one maintained ambient humidity, while the other analysed air samples dried to < 20% relative humidity.
The "wet" DMPS maintained air at ambient humidity (aproximately 80%) and was used in combination with a separate optical particle counter (OPC, Grimm Aerosol Technik GmbH & Co. KG model 1.108, Ainring, Germany). The OPC was used to measure coarse particles, which would otherwise have been lost due to the sampling process. In order to minimise losses of coarse particles, and to maintain ambient temperature and humidity, the OPC was located close to the inlet stack.
The wet DMPS was calibrated prior to the cruise, using NIST traceable Polystyrene Latex Spheres (PSL) standard. The data submitted to BODC had already been corrected according to this calibration.
Further details of sampling strategy and methodology for this, and other D319 data sets, are available from the D319 cruise report, and from Allan et al. (2009). A detailed decription of wet and dry DMSP, and the interpolation between OPC and wet DMPS is given by Williams et al. (2007).
References
Allan J.D., Topping D.O., Good N., Irwin M., Flynn M., Williams P.I., Coe H., Baker A.R., Martino M., Niedermeier N., Wiedensohler A., Lehmann S., Muller K., Herrmann H., McFiggans G., 2009. Composition and properties of atmospheric particles in the eastern Atlantic and impacts on gas phase uptake rates, Atmospheric Chemistry and Physics, 9, 9299-9314.
Williams P.I., McFiggans G., Gallagher M.W., 2007. Latitudinal aerosol size distribution variation in the Eastern Atlantic Ocean measured aboard the FS-Polarstern, Atmospheric Chemistry and Physics, 7, 2563-2573.
Project Information
UK SOLAS, Reactive Halogens in the Marine Boundary Layer (RHaMBLe)
This project was run by the University of Manchester, aiming to quantify the impacts of marine halogens on atmospheric composition. Emphasis was placed on the roles of halogens in oxidative processes, and on aerosol formation and transformations. Observations were made of a range of reactive halogen species in the marine atmosphere.
Fieldwork included open ocean and coastal campaigns:
- Intensive field campaign at the Cape Verde observatory
- Simultaneous ship transect through the Mauretanian Upwelling region (D319)
- Coastal field project to diagnose links between particle formation and reactive halogen species
These observations provide a comprehensive characterisation of halogen compounds in the marine atmosphere. New understanding of halogen chemistry enables development of parameterisations for model tuning. RHaMBLe has extensive links with UK SOLAS funded projects, and with other UK and internationally funded projects.
More detailed information on this project may be found in the official cruise report for the RHaMBLe cruise, D319.
Weblink: http://www.nerc.ac.uk/research/programmes/solas/
Surface Ocean Lower Atmosphere Study
The Surface Ocean-Lower Atmosphere Study (SOLAS) is an international research initiative comprising over 1500 scientists in 23 countries. Its central goal is to understand the biogeochemical-physical interactions between the ocean and atmosphere, and how their coupling affects, and is affected by climate change.
UK Surface Ocean Lower Atmosphere Study
The UK Surface Ocean Lower Atmosphere Study (UK SOLAS) is the UK's contribution to the international SOLAS programme.
UK SOLAS formed interdisciplinary teams to address three primary aims
- To determine the mechanisms controlling rates of chemical transfer and improve estimates of chemical exchanges
- To evaluate the impact of these exchanges on the biogeochemistry of the surface ocean and lower atmosphere and on feedbacks between the ocean and atmosphere
- To quantify the impacts of these boundary layer processes on the global climate system
UK SOLAS started in 2003, to run for seven years. The programme was funded by the Natural Environment Research Council.
Funded projects
In total, 19 projects have been funded by UK SOLAS, over four funding rounds.
Project Title | Short Title | Principal Investigator |
---|---|---|
Impact of atmospheric dust derived material and nutrient inputs on near-surface plankton microbiota in the tropical North Atlantic | Dust | Eric Achterberg |
The role and effects of photoprotective compounds in marine plankton | - | Steve Archer |
Field observations of sea spray, gas fluxes and whitecaps | SEASAW | Ian Brooks |
Factors influencing the biogeochemistry of iodine in the marine environment | - | Lucy Carpenter |
Global model of aerosol processes - effects of aerosol in the marine atmospheric boundary layer | GLOMAP | Ken Carslaw |
Ecological controls on fluxes of dimethyl sulphide (DMS) to the atmosphere | - | David Green |
Dust outflow and deposition to the ocean | DODO | Ellie Highwood |
Investigation of near surface production of iodocarbons - rates and exchanges | INSPIRE | Gill Malin |
Reactive halogens in the marine boundary layer | RHaMBLe | Gordon McFiggans |
The role of bacterioneuston in determining trace gas exchange rates | - | Colin Murrell |
Measuring methanol in sea water and investigating its sources and sinks in the marine environment | - | Phil Nightingale |
The impact of coastal upwellings on air-sea exchange of climatically important gases | ICON | Carol Robinson |
The Deep Ocean Gas Exchange Experiment | DOGEE | Rob Upstill-Goddard |
High wind air-sea exchanges | HiWASE | Margaret Yelland |
Aerosol characterisation and modelling in the marine environment | ACMME | James Allan |
3D simulation of dimethyl sulphide (DMS) in the north east Atlantic | - | Icarus Allen |
Processes affecting the chemistry and bioavailability of dust borne iron | - | Michael Krom |
The chemical structure of the lowermost atmosphere | - | Alastair Lewis |
Factors influencing the oxidative chemistry of the marine boundary layer | - | Paul Monks |
UK SOLAS has also supported ten tied studentships, and two CASE studentships.
Fieldwork
UK SOLAS fieldwork has included eight dedicated research cruises in the North Atlantic Ocean. Continuous measurements were made aboard aboard the Norwegian weather ship, Polarfront, until her decommission in 2009. Time series have been established at the SOLAS Cape Verde Observatory, and at the Plymouth Marine Laboratory L4 station. Experiments have taken place at the Bergen mesocosm facility.
A series of collaborative aircraft campaigns have added complementary atmospheric data. These campaigns were funded by UK SOLAS, African Monsoon Multidisciplinary Analyses (AMMA-UK), Dust and Biomass Experiment (DABEX) and the Facility for Airborne Atmospheric Measurements (FAAM).
Weblink: http://www.nerc.ac.uk/research/programmes/solas/
Data Activity or Cruise Information
Cruise
Cruise Name | D319 |
Departure Date | 2007-05-19 |
Arrival Date | 2007-06-11 |
Principal Scientist(s) | Gordon B McFiggans (University of Manchester School of Earth Atmospheric and Environmental Sciences) |
Ship | RRS Discovery |
Complete Cruise Metadata Report is available here
Fixed Station Information
No Fixed Station Information held for the Series
BODC Quality Control Flags
The following single character qualifying flags may be associated with one or more individual parameters with a data cycle:
Flag | Description |
---|---|
Blank | Unqualified |
< | Below detection limit |
> | In excess of quoted value |
A | Taxonomic flag for affinis (aff.) |
B | Beginning of CTD Down/Up Cast |
C | Taxonomic flag for confer (cf.) |
D | Thermometric depth |
E | End of CTD Down/Up Cast |
G | Non-taxonomic biological characteristic uncertainty |
H | Extrapolated value |
I | Taxonomic flag for single species (sp.) |
K | Improbable value - unknown quality control source |
L | Improbable value - originator's quality control |
M | Improbable value - BODC quality control |
N | Null value |
O | Improbable value - user quality control |
P | Trace/calm |
Q | Indeterminate |
R | Replacement value |
S | Estimated value |
T | Interpolated value |
U | Uncalibrated |
W | Control value |
X | Excessive difference |
SeaDataNet Quality Control Flags
The following single character qualifying flags may be associated with one or more individual parameters with a data cycle:
Flag | Description |
---|---|
0 | no quality control |
1 | good value |
2 | probably good value |
3 | probably bad value |
4 | bad value |
5 | changed value |
6 | value below detection |
7 | value in excess |
8 | interpolated value |
9 | missing value |
A | value phenomenon uncertain |
B | nominal value |
Q | value below limit of quantification |