Mineral aerosol concentration data from US JGOFS Arabian Sea
Entry ID:
US_JGOFS_ArabianSea_aerosols
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Summary
Abstract:
Dataset: Aerosols, long irradiation neutron activation analysis PI: Dr. Neil Tindale of: Texas A&M University dates: January 08, 1995 to December 18, 1995 location: N: 22.8459 S: 09.8871 W: 57.2609 E: 68.2687 project: Arabian Sea ship: Thomas Thompson PI Notes and Methodology can be found at http://usjgofs.whoi.edu/PI-NOTES/arabian/Tindale.html A note from DMO on supplementary fields ... can be found at http://usjgofs.whoi.edu/PI-NOTES/arabian/DMO-aerosols.html HiVol pump sampler methods are described in: N. W. Tindale and P. P. Pease, Aerosols over the Arabian Sea: Atmospheric transport pathways and concentrations of dust and sea salt, Deep Sea Research Part II: Topical Studies in OceanographyVolume 46, Issues 8-9, August 1999, Pages 1577-1595. View article at ScienceDirect, http://www.sciencedirect.com/science/article/B6VGC-3Y0RMGY-3/2/e320... JGOFS Arabian Sea Aerosol Data This mineral aerosol concentration data set is from samples collected during several cruises on the R/V Thomas Thompson during the JGOFS Arabian Sea field program. The data set includes the sampling period for each sample; the "Day of Year", yrday, number for the start of the sampling period for each sample; and the concentration of different elements for each sample, in micrograms per cubic meter. For the sampling period, "nd" is used as a filler to indicate "no data" gaps in the data array. The dust values are estimated using aluminum concentrations determined by neutron activation analysis. While most samples cover a multi-day period, we only have data for about 150 days. We didn't participate in all of the cruises and, on the cruises where samples were collected, often sampling conditions were less than ideal (bad weather, ship maneuvering, relative wind from astern etc.). A few samples that were collected showed obvious contamination from local sources, presumably from material from the R/V Thompson or from nearby fishing boats, and these samples were discarded and are not included in the data set. While the sampling period represents the period during which sampling occurred, sampling was usually not continuous. Sampling was frequently stopped, whenever sampling conditions were no longer suitable. Thus the concentration value at any particular date represents a time integrated sample which is usually non-continuous. Cautionary comments: 1. There may be a problem with the estimate for the mineral "dust" concentration. Most researchers use the average crustal ratio to estimate mineral dust concentrations using elemental concentration data (Al, Fe, etc.). Surface sand and silt samples that were collected in Oman in the Wahibah Sands region have distinct, non-crustal ratios. If individual aerosol samples are comprised of material from distinct sources, including Oman, then it is not unreasonable for their elemental ratios to differ from the published "average" crustal ratio that is used in most aerosol studies. 2. The amount of Ti in all the aerosol samples was small, despite there being a reasonable amount of dust material in most samples. The peaks for Cr and Ti overlap in the neutron activation short irradiation analysis and if significant quantities of Cr are present, this will interfere with the Ti analysis. With the exception of one sample, the Ti values are at or below the detection limit. The sole value above the detection limit was corrected for the Cr contribution using a correction based on the Cr values from the long irradiations. The correction changed the Ti value by less than 5%. The Ti data flagged as being at or below the detection limit was not corrected for possible Cr interference. Data management office notes on supplementary fields - aerosols data lat, lon A nominal ship location is given in lat/lon. The location is the noon position most near the middle of the sampling period, e.g. for a sample which was pumped intermittently from Jan. 3 - 5, the location is given for noon, Jan. 4. Intended as an aid to understanding, not a discrete location. date_begin, date_end We have included the start and stop day for each sample which we believe constrains the sample time about as well as is useful for these data. We also have pump volume and thus a mean concentration of dust per cubic meter of air for that time frame. The actual number of hours sampled during a time block (number of days) is complicated to present. Pumps were turned on and off repetitively depending upon ship maneuvers and relative wind direction (to prevent ship exhaust contamination). Also, the total number of hours the pumps were on is a less useful measure than pump volume, because of the variability in pump efficiency due to changing barometric pressures. An hours worth of pumping does not always yield the same volume of air.
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Description:
US JGOFS Arabian Sea aerosols (short irradiation neutron activation analysis)
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Parent DIF
This data set description is a member of a collection. The
collection is described in
SOLAS
Data Set Progress
COMPLETE
Personnel
Role:
DIF AUTHOR
Phone:
+44 (0) 1603 593837
Fax:
+44 (0) 1603 593715
Email:
thomas.bell at uea.ac.uk
Contact Address:
Laboratory for Global Marine and Atmospheric Chemistry
School of Environmental Sciences
University of East Anglia
City:
Norwich
Postal Code:
NR4 7TJ
Country:
UK
Role:
DIF AUTHOR
Phone:
+44 (0) 1603 591530
Fax:
+44 (0) 1603 593715
Email:
g.bayliss-brown at uea.ac.uk
Contact Address:
SOLAS International Project Office
School of Environmental Sciences
University of East Anglia
City:
Norwich
Postal Code:
NR4 7TJ
Country:
UK
Publications/References
N. W. Tindale and P. P. Pease, Aerosols over the Arabian Sea: Atmospheric transport pathways and concentrations of dust and sea salt, Deep Sea Research Part II: Topical Studies in Oceanography, Volume 46, Issues 8-9, August 1999, Pages 1577-1595.
Creation and Review Dates
DIF Creation Date:
2009-03-31
Last DIF Revision Date:
2009-03-31
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