Abstract
We analyze the influence of atmospheric boundary-layer development on new particle formation (NPF) during the morning transition. Continuous in-situ measurements of vertical profiles of temperature, humidity and aerosol number concentrations were quasi-continously measured near Melpitz, Germany, by unmanned aerial systems to investigate the potential connection between NPF and boundary-layer dynamics in the context of turbulence, temperature and humidity fluctuations. On 3 April 2014 high number concentrations of nucleation mode particles up to \(6.0 \times 10^4~\text {cm}^{-3}\) were observed in an inversion layer located about 450 m above ground level. The inversion layer exhibited a spatial temperature structure parameter \(C_T^2\) 15 times higher and a spatial humidity structure parameter \(C_q^2\) 5 times higher than in the remaining part of the vertical profile. The study provides hints that the inversion layer is responsible for creating favorable thermodynamic conditions for a NPF event. In addition, this layer showed a strong anti-correlation of humidity and temperature fluctuations. Using estimates of the turbulent mixing and dissipation rates, it is concluded that the downward transport of particles by convective mixing was also the reason of the sudden increase of nucleation mode particles measured on ground. This work supports the hypothesis that many of the NPF events that are frequently observed near the ground may, in fact, originate at elevated altitude, with newly formed particles subsequently being mixed down to the ground.
Similar content being viewed by others
References
Altstädter B, Platis A,Wehner B, Scholtz A,Wildmann N, Hermann M, Käthner R, Baars H, Bange J, Lampert A (2015)ALADINA: an unmanned research aircraft for observing vertical and horizontal distributions of ultrafine particles within the atmospheric boundary layer. Atmos Meas Tech 8(4):1627–1639. doi:10.5194/amt-8-1627-2015
Bange J, Spieß T, van den Kroonenberg AC (2007) Characteristics of the early-morning shallow convective boundary layer from helipod flights during STINHO-2. Theor Appl Climatol 90:113–126
Barbaro E, Arellano JVG, Ouwersloot HG, Schröter JS, Donovan DP, Krol MC (2014) Aerosols in the convective boundary layer: Shortwave radiation effects on the coupled land-atmosphere system. J Geophys Res Atmos 119(10):5845–5863
Berkowicz R, Prahm LP (1979) Generalization of K theory for turbulent diffusion. part I: Spectral turbulent diffusivity conceptpectral turbulent diffusivity concept. J Appl Meteorol 18(3):266–272
Bigg E (1997) A mechanism for the formation of new particles in the atmosphere. Atmos Res 43(2):129–137
Birmili W, Wiedensohler A (2000) New particle formation in the continental boundary layer: meteorological and gas phase parameter influence. Geophys Res Lett 27(20):3325–3328
Birmili W, Tomsche L, Sonntag A, Opelt C, Weinhold K, Nordmann S, Schmidt W (2013) Variability of aerosol particles in the urban atmosphere of Dresden (Germany): efects of spatial scale and particle size. Meteorol Z 22(2):195–211
Boy M, Hellmuth O, Korhonen H, Nilsson E, ReVelle D, Turnipseed A, Arnold F, Kulmala M (2006) MALTE-model to predict new aerosol formation in the lower troposphere. Atmos Chem Phys 6(12):4499–4517
Caughey S, Palmer S (1979) Some aspects of turbulence structure through the depth of the convective boundary layer. Q J R Meteorol Soc 105(446):811–827
Crumeyrolle S, Manninen H, Sellegri K, Roberts G, Gomes L, Kulmala M, Weigel R, Laj P, Schwarzenboeck A (2010) New particle formation events measured on board the ATR-42 aircraft during the EUCAARI campaign. Atmos Chem Phys 10(14):6721–6735
Davidson PA (2004) Turbulence: an introduction for scientists and engineers. Oxford University Press, Oxford 235 pp
Draxler R, Rolph G (2003) HYSPLIT (hybrid single-particle lagrangian integrated trajectory). NOAA Air Resources Laboratory, Silver Spring
Easter RC, Peters LK (1994) Binary homogeneous nucleation: temperature and relative humidity fluctuations, nonlinearity, and aspects of new particle production in the atmosphere. J Appl Meteorol 33(7):775–784
Größ J, Birmili W, Hamed A, Sonntag A, Wiedensohler A, Spindler G, Maninnen HE, Nieminen T, Kulmala M, Hõrrak U, Plass-Dülmer C (2015) Evolution of gaseous precursors and meteorological parameters during new particle formation events in the Central European boundary layer. Atmos Chem Phys Discuss 15(2):2305–2353. doi:10.5194/acpd-15-2305-2015, http://www.atmos-chem-phys-discuss.net/15/2305/2015/
Hanna SR (1968) A method of estimating vertical eddy transport in the planetary boundary layer using characteristics of the vertical velocity spectrum. J Atmos Sci 25(6):1026–1033
Hellmuth O (2006) Columnar modelling of nucleation burst evolution in the convective boundary layer-first results from a feasibility study Part I: Modelling approach. Atmos Chem Phys 6(12):4175–4214
Jaatinen A, Hamed A, Joutsensaari J, Mikkonen S, Birmili W, Wehner B, Spindler G, Wiedensohler A, Decesari S, Mircea M, Facchini MC, Junninen H, Kulmala M, Lehtined KEJ, Laaksonen A (2009) A comparison of new particle formation events in the boundary layer at three different sites in Europe. Boreal Environ Res 14:481–498
Kannosto J, Lemmetty M, Virtanen A, Mäkelä J, Keskinen J, Junninen H, Hussein T, Aalto P, Kulmala M (2008) Mode resolved density of atmospheric aerosol particles. Atmos Chem Phys Discuss 8(2):7263–7288
Kolmogorov A (1941) Local structure of turbulence in an incompressible fluid for very large Reynolds numbers. Dokl Akad Nauk SSSR 30:299–303
Korhonen P, Kulmala M, Laaksonen A, Viisanen Y, McGraw R, Seinfeld J (1999) Ternary nucleation of \(H_{2}SO_{4}\), \(NH_{3}\), and \(H_{2}O\) in the atmosphere. J Geophys Res Atmos 104(D21):26,349–26,353
Kulmala M, Vehkamäki H, Petäjä T, Dal Maso M, Lauri A, Kerminen VM, Birmili W, McMurry PH (2004) Formation and growth rates of ultrafine atmospheric particles: a review of observations. J Aerosol Sci 35(2):143–176
Kulmala M, Riipinen I, Sipilä M, Manninen HE, Petäjä T, Junninen H, Dal Maso M, Mordas G, Mirme A, Vana M, Hirsikko A, Laakso L, Harrison RM, Hanson I, Leung C, Lehtined KEJ, Kerminen VM (2007) Toward direct measurement of atmospheric nucleation. Science 318(5847):89–92
Lumley L, Panofsky H (1964) The structure of atmospheric turbulence. Wiley, New York 239 pp
Manninen HE, Petäjä T, Asmi E, Riipinen I, Nieminen T, Mikkilä J, Hõrrak U, Mirme A, Mirme S, Laakso L, Kerminen VM, Kulmala M (2009) Long-term field measurements of charged and neutral clusters using Neutral cluster and Air Ion Spectrometer (NAIS). Boreal Environ Res 14:591–605
Nilsson ED, Kulmala M (1998) The potential for atmospheric mixing processes to enhance the binary nucleation rate. J Geophys Res Atmos 103(D1):1381–1389
Nilsson E, Rannik Ü, Kulmala M, Buzorius G, O’dowd C (2001) Effects of continental boundary layer evolution, convection, turbulence and entrainment, on aerosol formation. Tellus B 53(4):441–461
Nojgaard JK, Nguyen QT, Glasius M, Sorensen LL (2012) Nucleation and Aitken mode atmospheric particles in relation to \(O_{3}\) and NOX at semirural background in Denmark. Atmos Environ 49:275–283. doi:10.1016/j.atmosenv.2011.11.040
O’Dowd C, McFiggans G, Creasey DJ, Pirjola L, Hoell C, Smith MH, Allan BJ, Plane J, Heard DE, Lee JD, Pilling MJ, Kulmala M (1999) On the photochemical production of new particles in the coastal boundary layer. Geophys Res Lett 26(12):1707–1710
O’Dowd C, Yoon Y, Junkermann W, Aalto P, Kulmala M, Lihavainen H, Viisanen Y (2009) Airborne measurements of nucleation mode particles II: boreal forest nucleation events. Atmos Chem Phys 9(3):937–944
Pirjola L, O’Dowd CD, Brooks IM, Kulmala M (2000) Can new particle formation occur in the clean marine boundary layer? J Geophys Res Atmos 105(D21):26,531–26,546
Ramanathan V, Crutzen P, Kiehl J, Rosenfeld D (2001a) Aerosols, climate, and the hydrological cycle. Science 294(5549):2119–2124
Ramanathan V, Crutzen PJ, Lelieveld J, Mitra A, Althausen D, Anderson J, Andreae M, Cantrell W, Cass G, Chung C, Clarke AD, Coakley J, Collins W, Conant W, Dulac F, Heintzenberg J, Heymsfield A, Holben B, Howell S, Hudson J, Jayaraman A, Kiehl J, Krishnamurti T, Lubin D, McFarquhar G, Novakov T, Ogren J, Podgorny I, Prather K, Priestly K, Prospero J, Quinn P, Rajeev K, Rasch P, Rupert SRS, Satheesh S, Shaw G, Sheridan P, Valero F (2001b) Indian Ocean experiment: an integrated analysis of the climate forcing and effects of the great Indo-Asian haze. J Geophys Res 106(D22):28,371–28,398
Rosenfeld D (2000) Suppression of rain and snow by urban and industrial air pollution. Science 287(5459):1793–1796
Seinfeld JH, Pandis SN (2012) Atmospheric chemistry and physics: from air pollution to climate change. Wiley, New York
Siebert H, Stratmann F, Wehner B (2004) First observations of increased ultrafine particle number concentrations near the inversion of a continental planetary boundary layer and its relation to ground-based measurements. Geophys Res Lett 31(9):L09102
Siebert H, Wehner B, Hellmuth O, Stratmann F, Boy M, Kulmala M (2007) New-particle formation in connection with a nocturnal low-level jet: observations and modeling results. Geophys Res Lett. doi:10.1029/2007GL029,891
Sipilä M, Berndt T, Petäjä T, Brus D, Vanhanen J, Stratmann F, Patokoski J, Mauldin RL, Hyvärinen AP, Lihavainen H, Kulmala M (2010) The role of sulfuric acid in atmospheric nucleation. Science 327(5970):1243–1246
Spindler G, Grüner A, Müller K, Schlimper S, Herrmann H (2013) Long-term size-segregated particle (PM10, PM2.5, PM1) characterization study at Melpitz-influence of air mass inflow, weather conditions and season. J Atmos Chem 70(2):165–195
Stratmann F, Siebert H, Spindler G, Wehner B, Althausen D, Heintzenberg J, Hellmuth O, Rinke R, Schmieder U, Seidel C et al (2003) New-particle formation events in a continental boundary layer: first results from the SATURN experiment. Atmos Chem Phys 3(5):1445–1459
Tatarskii VI (1971) The effects of the turbulent atmosphere on wave propagation. Israel Program for Scientific Translations, Jerusalem: 472 pp
van den Kroonenberg A, Martin S, Beyrich F, Bange J (2012) Spatially-averaged temperature structure parameter over a heterogeneous surface measured by an unmanned aerial vehicle. Boundary-Layer Meteorol 142(1):55–77
Weber AP, Friedlander SK (1997) In situ determination of the activation energy for restructuring of nanometer aerosol agglomerates. J Aerosol Sci 28(2):179–192
Wehner B, Siebert H, Stratmann F, Tuch T, Wiedensohler A, Petäjä T, Dal Maso M, Kulmala M (2007) Horizontal homogeneity and vertical extent of new particle formation events. Tellus B 59(3):362–371
Wehner B, Siebert H, Ansmann A, Ditas F, Seifert P, Stratmann F, Wiedensohler A, Apituley A, Shaw R, Manninen H, Kulmala M (2010) Observations of turbulence-induced new particle formation in the residual layer. Atmos Chem Phys 10(9):4319–4330
Westin K, Boiko A, Klingmann B, Kozlov V, Alfredsson P (1994) Experiments in a boundary layer subjected to free stream turbulence. Part 1. Boundary layer structure and receptivity. J Fluid Mech 281:193–218
Wiedensohler A, Covert DS, Swietlicki E, Aalto P, Heintzenberg J, Leck C (1996) Occurrence of an ultrafine particle mode less than 20 nm in diameter in the marine boundary layer during Arctic summer and autumn. Tellus B 48(2):213–222
Wiedensohler A, Cheng Y, Nowak A, Wehner B, Achtert P, Berghof M, Birmili W, Wu Z, Hu M, Zhu T, Takegawa N, Kita K, Kondo Y, Lou S, Hofzumahaus A, Holland F, Wahner A, Gunthe S, Rose D, Su H, Pöschl U (2009) Rapid aerosol particle growth and increase of cloud condensation nucleus activity by secondary aerosol formation and condensation: a case study for regional air pollution in northeastern China. J Geophys Res Atmos 114(D2):D00G08
Wiedensohler A, Birmili W, Nowak A, Sonntag A, Weinhold K, Merkel M, Wehner B, Tuch T, Pfeifer S, Fiebig M, Fjäraa A, Asmi E, Sellegri K, Depuy R, Venzac H, Villani P, Laj P, Aalto P, Ogren J, Swietlicki E, Williams P, Roldin P, Quincey P, Hüglin C, Fierz-Schmidhauser R, Gysel M, Weingartner E, Riccobono F, Santos S, Grüning C, Faloon K, Beddows D, Harrison R, Monahan C, Jennings S, O’Dowd C, Marinoni A, Horn HG, Keck L, Jiang J, Scheckman J, McMurry PH, Deng Z, Zhao C, Moerman M, Henzing B, de Leeuw G, Löschau G, Bastian S (2012) Mobility particle size spectrometers: harmonization of technical standards and data structure to facilitate high quality long-term observations of atmospheric particle number size distributions. Atmos Meas Tech 5:657–685
Wildmann N, Mauz M, Bange J (2013) Two fast temperature sensors for probing of the atmospheric boundary layer using small remotely piloted aircraft (RPA). Atmos Meas Tech 6:2101–2113. doi:10.5194/amt-6-2101-2013
Wildmann N, Hofsäß M, Weimer F, Joos A, Bange J (2014a) MASC-a small remotely piloted aircraft (RPA) for wind energy research. Adv Sci Res 11(1):55–61
Wildmann N, Ravi S, Bange J (2014b) Towards higher accuracy and better frequency response with standard multi-hole probes in turbulence measurement with remotely piloted aircraft (RPA). Atmos Meas Tech 7(4):1027–1041
Wyngaard J, LeMone M (1980) Behavior of the refractive index structure parameter in the entraining convective boundary layer. J Atmos Sci 37(7):1573–1585
Wyngaard JC, Izumi Y, Collins SA (1971) Behavior of the refractive-index-structure parameter near the ground. J Opt Soc Am 61:1646–1650
Acknowledgments
The authors thank the UAS pilots Lutz Bretschneider and Markus Auer for flying ALADINA and MASC safely over Melpitz. We thank Achim Grüner for technical support during preparing and conducting the campaigns in Melpitz. Thanks also to Johannes Größ for providing the NAIS-data from Melpitz. We thank Joe Smith and Ralf Käthner for the ground-crew support. This work is supported by the Deutsche Forschungsgemeinschaft (LA 2907/5-1, WI 1449/22-1, BA 1988/14-1).
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Platis, A., Altstädter, B., Wehner, B. et al. An Observational Case Study on the Influence of Atmospheric Boundary-Layer Dynamics on New Particle Formation. Boundary-Layer Meteorol 158, 67–92 (2016). https://doi.org/10.1007/s10546-015-0084-y
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s10546-015-0084-y