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Artigos de revistas sobre o tema "Atmospheric microlidar"

Autor: Grafiati
Publicado: 3 de agosto de 2024
Última modificação: 31 de julho de 2025

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1

Arumov, G. P., and A. V. Bukharin. "Miniaturization of elastic scattering lidars: determination of the microstructure of the surface layer of the atmosphere." Izmeritel`naya Tekhnika, no. 4 (June 26, 2024): 32–38. http://dx.doi.org/10.32446/0368-1025it.2024-4-32-38.

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Miniature elastic scattering lidars with similar schemes for determining the microstructure of the surface layer of the atmosphere are considered. In the considered microlidar model, it is assumed that in the limiting case there may be no particles in a small probed volume. In this case, the minimum value of the return signal corresponds to molecular scattering. The excess of the signal above this level is associated with the presence of a particle. The molecular component of the backscatter signal is constant and can be compared to a tabulated value of the backscatter coefficient using an opt
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2

Krichbaumer, W. "Airborne Cloud Measurements with the DLR Microlidar during the CLEOPATRA Campaign." Journal of Atmospheric and Oceanic Technology 13, no. 1 (1996): 54–57. http://dx.doi.org/10.1175/1520-0426(1996)013<0054:acmwtd>2.0.co;2.

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3

Mariage, Vincent, Jacques Pelon, Frédéric Blouzon, et al. "IAOOS microlidar-on-buoy development and first atmospheric observations obtained during 2014 and 2015 arctic drifts." Optics Express 25, no. 4 (2017): A73. http://dx.doi.org/10.1364/oe.25.000a73.

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4

Fierli, F., G. Di Donfrancesco, F. Cairo, et al. "Variability of cirrus clouds in a convective outflow during the Hibiscus campaign." Atmospheric Chemistry and Physics 8, no. 16 (2008): 4547–58. http://dx.doi.org/10.5194/acp-8-4547-2008.

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Abstract. Light-weight microlidar and water vapour measurements were taken on-board a stratospheric balloon during the HIBISCUS 2004 campaign, held in Bauru, Brazil (49° W, 22° S). Cirrus clouds were observed throughout the flight between 12 and 15 km height with a high mesoscale variability in optical and microphysical properties. It was found that the cirrus clouds were composed of different layers characterized by marked differences in height, thickness and optical properties. Simultaneous water vapour observations show that the different layers are characterized by different values of the
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5

Chen, Lee Chuin, Tsubasa Naito, Satoshi Ninomiya, and Kenzo Hiraoka. "Hyphenation of high-temperature liquid chromatography with high-pressure electrospray ionization for subcritical water LC-ESI-MS." Analyst 143, no. 22 (2018): 5552–58. http://dx.doi.org/10.1039/c8an01113c.

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6

Budke, C., and T. Koop. "BINARY: an optical freezing array for assessing temperature and time dependence of heterogeneous ice nucleation." Atmospheric Measurement Techniques 8, no. 2 (2015): 689–703. http://dx.doi.org/10.5194/amt-8-689-2015.

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Abstract. A new optical freezing array for the study of heterogeneous ice nucleation in microliter-sized droplets is introduced, tested and applied to the study of immersion freezing in aqueous Snomax® suspensions. In the Bielefeld Ice Nucleation ARraY (BINARY) ice nucleation can be studied simultaneously in 36 droplets at temperatures down to −40 °C (233 K) and at cooling rates between 0.1 and 10 K min−1. The droplets are separated from each other in individual compartments, thus preventing a Wegener–Bergeron–Findeisen type water vapor transfer between droplets as well as avoiding the seeding
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7

Ma, Chang-Jin, Cheol-Soo Lim, and Takuro Sakai. "Preliminary Study on the Elemental Quantification of in Ambient Liquid Samples of Microliter Volume Using the In-air Micro-PIXE Technique." Asian Journal of Atmospheric Environment 11, no. 1 (2017): 54–60. http://dx.doi.org/10.5572/ajae.2017.11.1.054.

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8

Budke, C., and T. Koop. "BINARY: an optical freezing array for assessing temperature and time dependence of heterogeneous ice nucleation." Atmospheric Measurement Techniques Discussions 7, no. 9 (2014): 9137–72. http://dx.doi.org/10.5194/amtd-7-9137-2014.

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Abstract. A new optical freezing array for the study of heterogeneous ice nucleation in microliter-sized droplets is introduced, tested and applied to the study of immersion freezing in aqueous Snomax® suspensions. In the Bielefeld Ice Nucleation ARraY (BINARY) ice nucleation can be studied simultaneously in 36 droplets at temperatures down to −40 °C (233 K) and at cooling rates between 0.1 K min−1 and 10 K min−1. The droplets are separated from each other in individual compartments, thus preventing a Wegener–Bergeron–Findeisen type water vapor transfer between droplets as well as avoiding the
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9

Kunert, Anna T., Mark Lamneck, Frank Helleis, Ulrich Pöschl, Mira L. Pöhlker, and Janine Fröhlich-Nowoisky. "Twin-plate Ice Nucleation Assay (TINA) with infrared detection for high-throughput droplet freezing experiments with biological ice nuclei in laboratory and field samples." Atmospheric Measurement Techniques 11, no. 11 (2018): 6327–37. http://dx.doi.org/10.5194/amt-11-6327-2018.

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Abstract. For efficient analysis and characterization of biological ice nuclei under immersion freezing conditions, we developed the Twin-plate Ice Nucleation Assay (TINA) for high-throughput droplet freezing experiments, in which the temperature profile and freezing of each droplet is tracked by an infrared detector. In the fully automated setup, a couple of independently cooled aluminum blocks carrying two 96-well plates and two 384-well plates, respectively, are available to study ice nucleation and freezing events simultaneously in hundreds of microliter-range droplets (0.1–40 µL). A cooli
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10

Hawkins, Lelia Nahid, Hannah G. Welsh, and Matthew V. Alexander. "Evidence for pyrazine-based chromophores in cloud water mimics containing methylglyoxal and ammonium sulfate." Atmospheric Chemistry and Physics 18, no. 16 (2018): 12413–31. http://dx.doi.org/10.5194/acp-18-12413-2018.

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Abstract. Simulating aqueous brown carbon (aqBrC) formation from small molecule amines and aldehydes in cloud water mimics provides insight into potential humic-like substance (HULIS) contributors and their effect on local and global aerosol radiative forcing. Previous work has shown that these (Maillard type) reactions generate products that are chemically, physically, and optically similar to atmospheric HULIS in many significant ways, including in their complexity. Despite numerous characterization studies, attribution of the intense brown color of many aqBrC systems to specific compounds r
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11

Grawe, Sarah, Stefanie Augustin-Bauditz, Hans-Christian Clemen, et al. "Coal fly ash: linking immersion freezing behavior and physicochemical particle properties." Atmospheric Chemistry and Physics 18, no. 19 (2018): 13903–23. http://dx.doi.org/10.5194/acp-18-13903-2018.

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Abstract. To date, only a few studies have investigated the potential of coal fly ash particles to trigger heterogeneous ice nucleation in cloud droplets. The presented measurements aim at expanding the sparse dataset and improving process understanding of how physicochemical particle properties can influence the freezing behavior of coal fly ash particles immersed in water. Firstly, immersion freezing measurements were performed with two single particle techniques, i.e., the Leipzig Aerosol Cloud Interaction Simulator (LACIS) and the SPectrometer for Ice Nuclei (SPIN). The effect of suspensio
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12

Gabel, J. C., K. D. Fallon, G. A. Laine, and R. E. Drake. "Lung lymph flow during volume infusions." Journal of Applied Physiology 60, no. 2 (1986): 623–29. http://dx.doi.org/10.1152/jappl.1986.60.2.623.

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We investigated the effect of intravenous isotonic crystalloid solution infusion on lung lymph flow. Tracheobronchial lung lymph vessels were cannulated in 13 anesthetized dogs. The lymph flow rate was measured 1) with the lymph flowing against atmospheric pressure (QL), and 2) with the pressure at the outflow end of the lymph cannula equal to systemic venous pressure (QLV). QL and QLV were measured alternately in each lymph vessel. In one group of nine dogs, the base-line QL and QLV were 18 +/- 9 and 13 +/- 6 (SD) microliter/min, respectively (P less than 0.05). QL increased by 4.8 +/- 1.4-fo
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13

Huang, Shuquan, Jessica Connolly, Andrei Khlystov, and Richard B. Fair. "Digital Microfluidics for the Detection of Selected Inorganic Ions in Aerosols." Sensors 20, no. 5 (2020): 1281. http://dx.doi.org/10.3390/s20051281.

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A prototype aerosol detection system is presented that is designed to accurately and quickly measure the concentration of selected inorganic ions in the atmosphere. The aerosol detection system combines digital microfluidics technology, aerosol impaction and chemical detection integrated on the same chip. Target compounds are the major inorganic aerosol constituents: sulfate, nitrate and ammonium. The digital microfluidic system consists of top and bottom plates that sandwich a fluid layer. Nozzles for an inertial impactor are built into the top plate according to known, scaling principles. Th
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14

Pelon, J., M. Mallet, A. Mariscal, et al. "Microlidar observations of biomass burning aerosol over Djougou (Benin) during African Monsoon Multidisciplinary Analysis Special Observation Period 0: Dust and Biomass-Burning Experiment." Journal of Geophysical Research 113 (December 13, 2008). http://dx.doi.org/10.1029/2008jd009976.

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15

Shao, Fangchi, Kuangwen Hsieh, Pengfei Zhang, Aniruddha M. Kaushik, and Tza-Huei Wang. "Facile and scalable tubing-free sample loading for droplet microfluidics." Scientific Reports 12, no. 1 (2022). http://dx.doi.org/10.1038/s41598-022-17352-3.

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AbstractDroplet microfluidics has in recent years found a wide range of analytical and bioanalytical applications. In droplet microfluidics, the samples that are discretized into droplets within the devices are predominantly loaded through tubings, but such tubing-based sample loading has drawbacks such as limited scalability for processing many samples, difficulty for automation, and sample wastage. While advances in autosamplers have alleviated some of these drawbacks, sample loading that can instead obviate tubings offers a potentially promising alternative but has been underexplored. To fi
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