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Dive into the research topics where Adam Kristensson is active.

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Featured researches published by Adam Kristensson.


Atmospheric Environment | 2002

Chemical and physical characterization of emissions from birch wood combustion in a wood stove.

Emma Hedberg; Adam Kristensson; Michael Ohlsson; Christer Johansson; Per-Åke Johansson; Erik Swietlicki; Vaclav Vesely; Ulla Wideqvist; Roger Westerholm

The purpose of this study was to characterize the emissions of a large number of chemical compounds emitted from birch wood combustion in a wood stove. Birch wood is widely used as fuel in Swedish household appliances. The fuel load was held constant during six experiments. Particles < 2.5 mum diameter were collected and the size distribution of the particles was measured. The results were compared to the size distribution in road traffic emissions. It could be seen that the number distribution differed between the sources. In traffic exhaust, the number of particles maximized at 20 nm, while the number distribution from wood burning ranged from 20 to 300 nm. The ratio K/Ca on particles was found. to be significantly different in wood burning compared to road dust, range 30-330 for the former and 0.8+/-0.15 for the latter. The source profile of common elements emitted from wood-burning differed from that found on particles at a street-level site or in long-distance transported particles. The ratio toluene/benzene in this study was found to be in the range 0.2-0.7, which is much lower than the ratio 3.6+/-0.5 in traffic exhaust emissions. Formaldehyde and acetone were the most abundant compounds among the volatile ketones and aldehydes. The emission factor varied between 180-710mg/kg wood for formaldehyde and 5-1300mg/kg wood for acetone. Of the organic acids analyzed (3,4,5)-trimethoxy benzoic acid was the most abundant compound. Of the PAHs reported, fluorene, phenanthrene, anthracene, fluoranthene and pyrene contribute to more than 70% of the mass of PAH. Of the elements analyzed, K and Si were the most abundant elements, having emission factors of 27 and 9mg/kg wood, respectively. Although fluoranthene has a toxic equivalence factor of 5% of benzo(a)pyrene (B(a)P), it can be seen that the toxic potency of fluoranthene in wood burning emissions is of the same size as B(a)P. This indicates that the relative carcinogenic potency contribution of fluoranthene in wood smoke would be about 40% of B(a)P


Journal of Geophysical Research | 2010

Soluble Mass, Hygroscopic Growth, and Droplet Activation of Coated Soot Particles during LACIS Experiment in November (LExNo)

S. Henning; Heike Wex; T. Hennig; Alexei Kiselev; Jefferson R. Snider; D. Rose; U. Dusek; Göran Frank; Ulrich Pöschl; Adam Kristensson; Merete Bilde; R. Tillmann; Astrid Kiendler-Scharr; Thomas F. Mentel; S. Walter; J. Schneider; C. Wennrich; Frank Stratmann

The LACIS Experiment in November (LExNo) campaign was conducted in November 2005 at the Atmospheric Composition Change the European Network of Excellence (ACCENT) site Leipzig Aerosol Cloud Interaction Simulator (LACIS). The goal of LExNo was to provide deeper insight into the activation properties of coated soot particles imitating aged combustion aerosol particles. The aerosols were prepared by starting with spark-generated soot particles. In some experiments the soot particles were compacted by exposure to propanol vapor; in others this step was bypassed. The soot was thermally coated with ammonium sulfate, levoglucosan, or a mixture of both ammonium sulfate and levoglucosan. The synthesized particles were investigated using aerosol mass spectrometry, a Hygroscopicity Tandem differential mobility analyzer, two Wyoming static diffusion cloud condensation nuclei (CCN) instruments, a Droplet Measurement Technologies continuous flow CCN instrument, and LACIS. A close correlation between the hygroscopic growth factor at 98% relative humidity and the critical supersaturation of CCN activation was observed. Closure between hygroscopic growth, CCN activation, and chemical composition of the investigated particles was achieved with two different single-parameter Kohler model approaches and with a third approach, a standard Kohler model using as input parameter the soluble mass as determined by aerosol mass spectrometry. (Less)


Atmospheric Environment | 2003

Model simulation of ultrafine particles inside a road tunnel

Lars Gidhagen; Christer Johansson; Johan Ström; Adam Kristensson; Erik Swietlicki; Liisa Pirjola; H.-C. Hansson

A monodispersive aerosol dynamic model, coupled to a 3D hydrodynamical grid model, has been used to study the dynamics of ultrafine particles inside a road tunnel in Stockholm, Sweden. The model results were compared to measured data of particle number concentrations, traffic intensity and tunnel ventilation rate. Coagulation and depositional losses to the tunnel walls were shown to be important processes during traffic peak hours, together contributing to losses of 77% of the particles smaller than 10nm and 41% of the particles of size 10-29nm. Particle growth due to water uptake or the presence of a micron-sized, resuspended particle fraction did not have any significant effect on the number of particles lost due to coagulation. Model simulation of particle number concentration response to temporal variations in traffic flow showed that constant emission factors could be used to reproduce the concentration variations of the particles larger than 29nm, while vehicle-speed-dependent factors are suggested to reproduce the variation of the smallest fractions. The emission factors for particle number concentrations estimated from the model simulation are in general higher and show a larger contribution from light-duty vehicles than what has been reported from a tunnel in California. The model study shows that combined measurements and model simulations in road tunnels can be used to improve the determinations of vehicle emission factors for ultrafine particles under realistic driving conditions


Tellus B | 2008

Characterization of new particle formation events at a background site in Southern Sweden: relation to air mass history

Adam Kristensson; M. Dal Maso; Erik Swietlicki; Tareq Hussein; J. Zhou; V.-M. Kerminen; Markku Kulmala

Particle formation events were analysed from aerosol number size distribution data collected at a background station in southern Sweden between February 2001 and May 2004. Events occurred on about 36% of all days and were favoured by high global radiation values. The clearest events (class I, 20% of all days) were observed when the formation rate of activated hypothetical clusters around 1 nm diameter, J1 was higher than 10(180*CondS-0.60), where CondS is the condensation sink (in s-1). The median condensable vapour concentration, observed formation rate at 3 nm, and growth rate during class I events were 3.0 × 107 cm-3, 1.1 cm-3 s-1 and 2.1 nm h-1, respectively. On 7% of all days, it was possible to observe growth of the newly formed particles exceeding 30 nm geometric mean diameter during event days in the evening, which is important for the regional particle population, and thereby the climate. A trajectory analysis revealed that cleaner air masses were relatively more important for the contribution of Aitken mode particles than polluted ones. Class I events were registered on 36% of all days when trajectories had passed over the open sea, indicating that ship traffic can contribute to particle formation and growth.


Journal of Physical Chemistry A | 2010

Cloud Droplet Activation of Amino Acid Aerosol Particles.

Adam Kristensson; Thomas Rosenørn; Merete Bilde

In this work we investigated the ability of a series of amino acids to act as cloud condensation nuclei using a static thermal gradient diffusion type cloud condensation nucleus counter. Particles of pure dry l-glycine, glycyl-glycine, l-serine, l-methionine, l-glutamic acid, l-aspartic acid, and l-tyrosine were studied as well as internally mixed dry particles containing ammonium sulfate and one or two of the following amino acids: l-methionine, l-aspartic acid, or l-tyrosine. The amino acids ranged in water solubility from high (>100 g/L), intermediate (10-100 g/L), low (3-10 g/L), to very low (<3 g/L). With the exception of l-methionine and l-tyrosine, all the studied pure amino acid particles activated as though they were fully soluble, although Kohler theory modified to account for limited solubility suggests that the activation of the intermediate and low solubility amino acids l-serine, l-glutamic acid, and l-aspartic acid should be limited by solubility. Activation of mixed particles containing at least 60% dry mass of l-tyrosine was limited by solubility, but the activation of the other investigated mixed particles behaved as if fully soluble. In general, the results show that particles containing amino acids at atmospherically relevant mixture ratios are good cloud condensation nuclei.


Journal of Geophysical Research | 2010

Examination of laboratory-generated coated soot particles: An overview of the LACIS Experiment in November (LExNo) campaign

Frank Stratmann; Merete Bilde; U. Dusek; Göran Frank; T. Hennig; S. Henning; Astrid Kiendler-Scharr; A. Kiselev; Adam Kristensson; Ingo Lieberwirth; Thomas F. Mentel; Ulrich Pöschl; D. Rose; J. Schneider; Jefferson R. Snider; R. Tillmann; S. Walter; Heike Wex

In the suite of laboratory measurements described here and in companion articles we deal with the hygroscopic growth and activation behavior of coated soot particles synthesized to mimic those of an atmospheric aerosol originating from biomass combustion. The investigations were performed during the measurement campaign LACIS Experiment in November (LExNo) which took place at the Leipzig Aerosol Cloud Interaction Simulator (LACIS). The specific goals of this campaign were (1) to perform a critical supersaturation measurement intercomparison using data sets from three different cloud condensation nucleus (CCN) instruments (two static thermal gradient type, one stream-wise thermal gradient type) and LACIS, (2) to examine particle hygroscopic growth (hydrated particle size as function of relative humidity) for particle characteristics such as aerosol mass spectrometer (AMS) measured soluble mass and particle morphology, and (3) to relate critical supersaturations derived from both measurements of soluble mass and high humidity tandem differential mobility analyzer (HH-TDMA) determined growth factors to critical supersaturations measured by means of the CCN instruments. This paper provides information on the particle synthesis techniques used during LExNo, an overview concerning the particle characterization measurements performed, and, by proving relations between measured composition, hygroscopic growth, and activation data, lay the foundations for the detailed investigations described in the companion studies. In the context of the present paper, excellent agreement of the critical supersaturations measured with three different CCN instruments and LACIS was observed. Furthermore, clear relations between coating masses determined with AMS and both hygroscopic growth factors at 98% RH and measured critical supersaturations could be seen. Also, a strong correlation between measured hygroscopic growth (growth factors at 98%) and measured critical supersaturation for all of the differently coated soot particles (coating substances being levoglucosan and/or ammonium (hydrogen) sulfate) was found. This is clearly indicative of the possibility of predicting the critical supersaturation of coated soot particles based on hygroscopic growth measurements using Kohler theory. (Less)


Tellus B | 2016

Coupling an aerosol box model with one-dimensional flow: a tool for understanding observations of new particle formation events

Niku Kivekäs; Jimmie Carpman; Pontus Roldin; Johannes Leppä; Ewan J. O'Connor; Adam Kristensson; Eija Asmi

Field observations of new particle formation and the subsequent particle growth are typically only possible at a fixed measurement location, and hence do not follow the temporal evolution of an air parcel in a Lagrangian sense. Standard analysis for determining formation and growth rates requires that the time-dependent formation rate and growth rate of the particles are spatially invariant; air parcel advection means that the observed temporal evolution of the particle size distribution at a fixed measurement location may not represent the true evolution if there are spatial variations in the formation and growth rates. Here we present a zero-dimensional aerosol box model coupled with one-dimensional atmospheric flow to describe the impact of advection on the evolution of simulated new particle formation events. Wind speed, particle formation rates and growth rates are input parameters that can vary as a function of time and location, using wind speed to connect location to time. The output simulates measurements at a fixed location; formation and growth rates of the particle mode can then be calculated from the simulated observations at a stationary point for different scenarios and be compared with the ‘true’ input parameters. Hence, we can investigate how spatial variations in the formation and growth rates of new particles would appear in observations of particle number size distributions at a fixed measurement site. We show that the particle size distribution and growth rate at a fixed location is dependent on the formation and growth parameters upwind, even if local conditions do not vary. We also show that different input parameters used may result in very similar simulated measurements. Erroneous interpretation of observations in terms of particle formation and growth rates, and the time span and areal extent of new particle formation, is possible if the spatial effects are not accounted for.


Atmospheric Chemistry and Physics | 2010

Aerosol ageing in an urban plume – implications for climate and health

Pontus Roldin; Erik Swietlicki; A. Massling; Adam Kristensson; Jakob Löndahl; Axel Eriksson; Joakim Pagels; S. Gustafsson

This paper presents an application of the ADCHEM air-trajectory model with online chemistry, aerosol microphysics and radiative transfer. The authors investigate the aging of air masses after they pass over Malmö, Sweden, and model predictions are tested using a field station 50 km downwind of Malmö. They estimate the effect of Malmö on the aerosol radiative forcing and a proxy for aerosol health effects.


Scientific Data | 2018

Collocated observations of cloud condensation nuclei, particle size distributions, and chemical composition

Julia Schmale; S. Henning; Bas Henzing; Helmi Keskinen; K. Sellegri; Jurgita Ovadnevaite; A. Bougiatioti; N. Kalivitis; Iasonas Stavroulas; Anne Jefferson; Minsu Park; P. Schlag; Adam Kristensson; Yoko Iwamoto; K. J. Pringle; C. L. Reddington; Pasi Aalto; Mikko Äijälä; Urs Baltensperger; Jakub Bialek; Wolfram Birmili; Nicolas Bukowiecki; Mikael Ehn; A. M. Fjaeraa; Markus Fiebig; Göran Frank; Roman Fröhlich; Arnoud Frumau; Masaki Furuya; E. Hammer

Cloud condensation nuclei (CCN) number concentrations alongside with submicrometer particle number size distributions and particle chemical composition have been measured at atmospheric observatories of the Aerosols, Clouds, and Trace gases Research InfraStructure (ACTRIS) as well as other international sites over multiple years. Here, harmonized data records from 11 observatories are summarized, spanning 98,677 instrument hours for CCN data, 157,880 for particle number size distributions, and 70,817 for chemical composition data. The observatories represent nine different environments, e.g., Arctic, Atlantic, Pacific and Mediterranean maritime, boreal forest, or high alpine atmospheric conditions. This is a unique collection of aerosol particle properties most relevant for studying aerosol-cloud interactions which constitute the largest uncertainty in anthropogenic radiative forcing of the climate. The dataset is appropriate for comprehensive aerosol characterization (e.g., closure studies of CCN), model-measurement intercomparison and satellite retrieval method evaluation, among others. Data have been acquired and processed following international recommendations for quality assurance and have undergone multiple stages of quality assessment.


Atmospheric Environment | 2004

Real-world traffic emission factors of gases and particles measured in a road tunnel in Stockholm, Sweden

Adam Kristensson; Christer Johansson; Roger Westerholm; Erik Swietlicki; Lars Gidhagen; Ulla Wideqvist; Vaclav Vesely

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Pasi Aalto

University of Helsinki

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Niku Kivekäs

Finnish Meteorological Institute

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Heikki Lihavainen

Finnish Meteorological Institute

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