Abstract
In epidemiological studies, outdoor exposure to pollen is typically estimated using rooftop monitoring station data, whilst exposure overwhelmingly occurs at street level. In this study the relationship between street level and roof level grass pollen concentrations was investigated for city centre street canyon environments in Aarhus, Denmark, and London, UK, during the grass pollen seasons of 2010 and 2011 respectively. For the period mid-day to late evening, street level concentrations in both cities tended to be lower than roof-level concentrations, though this difference was found to be statistically significant only in London. The ratio of street/roof level concentrations was compared with temperature, relative humidity, wind speed and direction, and solar radiation. Results indicated that the concentration ratio responds to wind direction with respect to relative canyon orientation and local source distribution. In the London study, an increase in relative humidity was linked to a significant decrease in street/roof level concentration ratio, and a possible causative mechanism involving moisture mediated pollen grain buoyancy is proposed. Relationships with the other weather variables were not found to be significant in either location. These results suggest a tendency for monitoring station data to overestimate exposure in the canyon environment.
Similar content being viewed by others
Notes
The precise height above ground level of a monitoring station will depend upon local urban topography. Ideally a station should be situated above any surrounding physical structures such as trees or buildings that may interfere with local airflow patterns (Lacey and Venette 1995), pp 424–425).
The briefer sampling period in London was due to the collection of additional data sets not presented in this study.
A single rod samples air at 21.7 l min−1, over twice the rate of the 7-Day sampler (10 l min−1).
The H/W ratio of the Upper Street canyon depends on wind direction because the height of the buildings on either side differ. For winds from the East side of the street the ratio is 0.69. The exact height of the buildings on the West side is not known; however, it is slightly taller, thus the H/W ratio will be slightly greater.
In the context of a street canyon, this is equivalent to the leeward side of the street.
References
Alcázar P, Comtois P (2000) The influence of sampler height and orientation on airborne Ambrosia pollen counts in Montreal. Grana 39(6):303–307
Alcázar P, Galán C, Cariñanos P, Domíguez-Vilches E (1999) Effects of sampling height and climatic conditions in aerobiological studies. J Investig Allergol Clin Immunol 9(4):253–261
Aylor DE (2002) Settling speed of corn (Zea mays) pollen. J Aerosol Sci 33(11):1601–1607
Aylor DE (2003) Rate of dehydration of corn (Zea mays L.) pollen in the air. J Exp Bot 54(391):2307–2312
Berkowicz R, Palmgren F, Hertel O, Vignati E (1996) Using measurements of air pollution in streets for evaluation of urban air quality - meteorological analysis and model calculations. Sci Total Environ 189(190):259–265
Berkowicz R, Hertel O, Larsen SE, Sørensen NN, Nielsen M (1997) Modelling traffic pollution in streets. Ministry of Environment and Energy. National Environmental Research Institute, Roskilde
British Aerobiology Federation (1994) Airborne pollens and spores: a guide to trapping and counting. British Aerobiology Federation
Bryant RH, Emberlin JC, Norris-Hill J (1989) Vertical variation in pollen abundance in North-Central London. Aerobiology 5(2):123–137
Colls JJ, Micallef A (1999) Measured and modelled concentrations and vertical profiles of airborne particulate matter within the boundary layer of a street canyon. Sci Total Environ 235(1–3):221–233
Dabberdt WF, Hoydysh WG (1991) Street canyon dispersion: sensitivity to block shape and entrainment. Atmos Environ Part A Gen Top 25(7):1143–1153
Danish Geodata Agency (2012) Conditions for use of open public geographic data [Online]. Available at: http://www.gst.dk/NR/rdonlyres/AD386601-C92E-479F-8BE8-FD9878B193A7/0/Conditionsforuseofopenpublicgeographicdata.pdf, [Accessed 23 September 2012]
Edina (2011) Digimap collections [Online]. Available at: http://edina.ac.uk/digimap, [Accessed 17 February 2011]
Emberlin J, Norris-Hill J (1991) Spatial variation of pollen deposition in North London. Grana 30(1):190–195
ESRI (2011) ArcGIS Desktop: Release 10. Environmental Systems Research Institute, Redlands
Feo Brito F, Mur Gimeno P, Martínez C, Tobías A, Suárez L, Guerra F, Borja JM, Alonso AM (2007) Air pollution and seasonal asthma during the pollen season. A cohort study in Puertollano and Ciudad Real (Spain). Allergy 62(10):1152–1157
Fitzgerald JW (1975) Approximation formulas for the equilibrium size of an aerosol particle as a function of its dry size and composition and the ambient relative humidity. J Appl Meteorol 14:1044–1049
Hajat S, Haines A, Atkinson RW, Bremner SA, Anderson HR, Emberlin J (2001) Association between air pollution and daily consultations with general practitioners for allergic rhinitis in London, United Kingdom. Am J Epidemiol 153(7):704–714
Hertel O, Goodsite ME (2009) Urban air pollution climates throughout the world. In: Hester RE, Harrison R (eds) Air quality in urban environments. Issues in Environmental Science and Technology, vol 28, RSC Publishing, pp 1–22
Hertel O, Ellermann T, Palmgren F, Berkowicz R, Løfstrøm P, Frohn LM, Geels C, Skjøth CA, Brandt J, Christensen J, Kemp K, Ketzel M (2007) Integrated air-quality monitoring - combined use of measurements and models in monitoring programmes. Environ Chem 4(2):65–74
Hirst JM (1952) An automatic volumetric spore trap. Ann Appl Biol 39(2):257–265
Käpylä M (1983) The variation of airborne pollen concentrations around a big building in a town. In: 5th Nordic Symposium on Aerobiology, Session III, pp 39–42
Lacey J, Venette J (1995) Outdoor air sampling techniques. In: Cox CS, Wathes CM (eds) Bioaerosols handbook, 1st edn. CRC, Boca Raton, pp 407–471
MATLAB (2008) MATLAB version 7.7.0.471 (R2008b). The MathWorks, Natick, MA
McDonald JE (1962) Collection and washout of airborne pollens and spores by raindrops. Science 135(3502):435–437
Momas I, Nikasinovic L, Seta N, Callais F, Just J, Sahraoui F, Grimfeld A (2003) Personal exposure to outdoor urban air pollution and nasal inflammation in asthmatic and healthy children: an epidemiological study in Paris. Epidemiology 14(5):S62–S63
Nakamura Y, Oke TR (1988) Wind, temperature and stability conditions in an East–west orientated urban canyon. Atmos Environ 22(12):2691–2700
Norris-Hill J, Emberlin J (1991) Diurnal variation of pollen concentration in the air of north-central London. Grana 30(1):229–234
Oke TR (1988) Street design and urban canopy layer climate. Energy Build 11:103–113
Palmgren F, Berkowicz R, Hertel O, Vignati E (1996) Effects of reduction of NO x on the NO2 levels in urban streets. Sci Total Environ 189/190:409–415
Peel RG, Kennedy R, Smith M, Hertel O (2013) Relative efficiencies of the Burkard 7-day, Rotorod and Burkard Personal samplers for Poaceae and Urticaceae pollen under field conditions. Ann Agric Environ Med (in press)
Pryor SC, Barthelmie RJ (2000) Particle dry deposition to water surfaces: processes and consequences. Mar Pollut Bull 41(1–6):220–231
Rantio-Lehtimäki A, Koivikko A, Kupias R, Mäkinen Y, Pohjola A (1991) Significance of sampling height of airborne particles for aerobiological information. Allergy 46(1):68–76
Raynor GS, Ogden EC, Hayes JV (1973) Variation in ragweed pollen concentration to a height of 108 meters. J Allergy Clin Immunol 51(4):199–207
Sampling Technologies (1998) Operating instructions for the Rotorod sampler. Sampling Technologies, Minnetonka
Skjøth CA, Ørby PV, Becker T, Geels C, Schlünssen V, Sigsgaard T, Bønløkke JH, Sommer J, Søgaard P, Hertel O (2013) Identifying urban sources as cause to elevated grass pollen concentrations using GIS and remote sensing. Biogeosciences 10:541–554
Spieksma FTM, van Noort P, Nikkels H (2000) Influence of nearby stands of Artemisia on street-level versus roof-top-level ratio’s of airborne pollen quantities. Aerobiology 16(1):21–24
Stach A, Emberlin J, Smith M, Adams-Groom B, Myszkowska D (2008) Factors that determine the severity of Betula spp. pollen seasons in Poland (Poznań and Krakow) and the United Kingdom (Worcester and London). Int J Biometeorol 52:311–321
UK Meteorological Office (2010) MIDAS Land Surface Stations data (1853-current), [Internet]. NCAS British Atmospheric Data Centre, 2006. Available from: http://badc.nerc.ac.uk/view/badc.nerc.ac.uk__ATOM__dtaent_ukmo-midas
Warner FE, McCartney HA, Emberlin J (2000) Wind tunnel comparison of the collection efficiency of three Hirst-type volumetric sampler drum coatings. Aerobiology 16(1):25–28
Acknowledgements
The first author would like to extend special thanks to Stine Rødjajn for help with sample collection, to Janne Sommer at Astma-Allergi Danmark for providing access to data and facilities, and to Dr. Harry Morrow Brown for generously lending equipment. The Danish Air Quality Monitoring Programme, and in particular Thomas Ellermann, are also thanked for contributing meteorological data.
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Peel, R.G., Kennedy, R., Smith, M. et al. Do urban canyons influence street level grass pollen concentrations?. Int J Biometeorol 58, 1317–1325 (2014). https://doi.org/10.1007/s00484-013-0728-x
Received:
Revised:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00484-013-0728-x