Search results for "ice crystals"

showing 10 items of 69 documents

Single-crystal I h ice surfaces unveil connection between macroscopic and molecular structure

2017

Physics and chemistry of ice surfaces are not only of fundamental interest but also have important impacts on biological and environmental processes. As ice surfaces—particularly the two prism faces—come under greater scrutiny, it is increasingly important to connect the macroscopic faces with the molecular-level structure. The microscopic structure of the ubiquitous ice Ih crystal is well-known. It consists of stacked layers of chair-form hexagonal rings referred to as molecular hexagons. Crystallographic unit cells can be assembled into a regular right hexagonal prism. The bases are labeled crystallographic hexagons. The two hexagons are rotated 30° with respect to each other. The linkage…

Hexagonal prismMultidisciplinaryMaterials sciencegenetic structures010504 meteorology & atmospheric sciencesIce crystalsbusiness.industryIce IhGeometry02 engineering and technology021001 nanoscience & nanotechnologyCorrections01 natural sciencesCrystalOpticsPhysical SciencesPrismSnowflake0210 nano-technologybusinessSingle crystal0105 earth and related environmental sciencesElectron backscatter diffractionProceedings of the National Academy of Sciences
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Dehydration potential of ultrathin clouds at the tropical tropopause

2003

[1] We report on the first simultaneous in situ and remote measurements of subvisible cirrus in the uppermost tropical troposphere. The observed cirrus, called UTTCs ( ultrathin tropical tropopause clouds), are the geometrically (200-300 m) and optically (t approximate to 10(-4)) thinnest large-scale clouds ever sampled (approximate to10(5) km(2)). UTTCs consist of only a few ice particles per liter with mean radius approximate to5 mum, containing only 1-5 % of the total water. Yet, brief adiabatic cooling events only 1-2 K below mean ambient temperature destabilize UTTCs, leading to large sedimenting particles (r approximate to 25 mm). Due to their extreme altitude above 17 km and low part…

Ice cloudMaterials scienceIce crystalsparticle micro-physicsdehydrationtropical tropopauseRadiusAtmospheric sciencesJTroposphereGeophysicsAltitudeddc:550General Earth and Planetary SciencesCirrussubvisible cirrus cloudsTropopauseStratosphere
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Cascaded adaptive-mask algorithm for twin-image removal and its application to digital holograms of ice crystals.

2009

An iterative Gerchberg-Saxton-type algorithm with a support constraint for twin-image removal from reconstructed Gabor inline holograms of single plane objects is described. It is applied to simulated holograms and to holograms of ice crystals recorded in the laboratory and in atmospheric clouds in situ. The algorithm is characterized by a distinction between object and background region and an iterative adaption of the object mask. Applying the algorithm to recorded inline holograms of atmospheric objects, the twin-image artifacts are removed successfully, for the first time allowing for a proper access to the in situ phase information on atmospheric ice crystals. It is also demonstrated t…

Ice crystalsComputer sciencebusiness.industryMaterials Science (miscellaneous)HolographyPhase (waves)Industrial and Manufacturing EngineeringPtychographylaw.inventionLight intensityOpticslawFresnel numberBusiness and International ManagementbusinessPhase retrievalAlgorithmDigital holographyApplied optics
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Partitioning of Aerosol Particles in Mixed-phase Clouds at a High Alpine Site

2007

6 German Aerospace Centre, D-82234, Wessling, Germany * Now at Institute for Atmospheric and Climate Science, ETH Zurich, 8092 Zurich, Switzerland Abstract The partitioning of aerosol particles between the cloud and the interstitial phase (i.e., unactivated aerosol) has been investigated during several Cloud and Aerosol Characterization Experiments (CLACE) conducted in winter and summer 2004 and winter 2005 at the high alpine research station Jungfraujoch (3,580 m altitude, Switzerland). Ambient air was sampled using different inlets in order to determine the scavenged fraction of aerosol particles, F Scav , and of black carbon, F Scav,BC . They denote the fraction of the aerosol volume con…

Ice crystalsParticle numberLiquid water contentPhase (matter)Ice nucleusEnvironmental scienceAtmospheric sciencescomplex mixturesMass fractionWater vaporAerosol
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Upper tropospheric water vapour and its interaction with cirrus clouds as seen from IAGOS long-term routine in-situ observations

2017

IAGOS (In-service Aircraft for a Global Observing System) performs long-term routinein situobservations of atmospheric chemical composition (O3, CO, NOx, NOy, CO2, CH4), water vapour, aerosols, clouds, and temperature on a global scale by operating compact instruments on board of passenger aircraft. The unique characteristics of the IAGOS data set originate from the global scale sampling on air traffic routes with similar instrumentation such that the observations are truly comparable and well suited for atmospheric research on a statistical basis. Here, we present the analysis of 15 months of simultaneous observations of relative humidity with respect to ice (RHice) and ice crystal number …

In situ010504 meteorology & atmospheric sciencesIce crystalsSampling (statistics)010501 environmental sciencesAtmospheric sciences01 natural sciencesGeneralLiterature_MISCELLANEOUSTroposphereddc:550Environmental scienceRelative humidityCirrusPhysical and Theoretical ChemistryTropopauseWater vapor0105 earth and related environmental sciences
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Tropical tropopause ice clouds: a dynamic approach to the mystery of low crystal numbers

2012

Abstract. The occurrence of high, persistent ice supersaturation inside and outside cold cirrus in the tropical tropopause layer (TTL) remains an enigma that is intensely debated as the "ice supersaturation puzzle". However, it was recently confirmed that observed supersaturations are consistent with very low ice crystal concentrations, which is incompatible with the idea that homogeneous freezing is the major method of ice formation in the TTL. Thus, the tropical tropopause "ice supersaturation puzzle" has become an "ice nucleation puzzle". To explain the low ice crystal concentrations, a number of mainly heterogeneous freezing methods have been proposed. Here, we reproduce in situ measure…

In situAtmospheric ScienceSupersaturationIce crystalsChemistryAtmospheric scienceslcsh:QC1-999lcsh:ChemistryCrystallcsh:QD1-999Sea ice growth processesIce nucleusddc:550CirrusClear icelcsh:Physics
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Simulations clarify when supercooled water freezes into glassy structures

2014

Although liquid water is a ubiquitous substance and its properties are crucial for all living species, the precise understanding of these properties is still a matter of active scientific research. One rather mysterious aspect concerns the conditions when undercooled water freezes not into ice crystals but into glass-like structures. Based on a rather novel type of computer simulation approach, in PNAS, Limmer and Chandler (1) propose a nonequilibrium phase diagram that attempts to clarify the conditions (temperature, pressure, cooling protocol) under which one should observe transitions from undercooled water to different forms of amorphous ice.

Phase transitionMultidisciplinaryIce crystalsLiquid waterChemistryAmorphous iceThermodynamicsNon-equilibrium thermodynamicsSupercoolingPhase diagramProceedings of the National Academy of Sciences
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Contrail Formation: Analysis of Sublimation Mechanisms

2018

We study losses of ice crystals in a persistent, soot-rich contra i l in the wake behind a medium-sized aircraft at cru i se. Constrain i n g a model covering ice nucleation, growth, and subl i m a t i o n phases with a n aircraft data set, we track the subl i m a t i o n history over two minutes of cont r a i l age and rela t e ice crystal numbers to the number of soot particles emitted by th e aircraft engines.

Physics010504 meteorology & atmospheric sciencesIce crystalscontrailsAtmosphärische SpurenstoffeCloud physicsThermodynamics010502 geochemistry & geophysics01 natural sciencesGeophysicsIce nucleusprocess modelingGeneral Earth and Planetary SciencesSublimation (phase transition)microphysicsWolkenphysikSoot particlesaircraft measurements0105 earth and related environmental sciencesGeophysical Research Letters
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HOLIMO II: a digital holographic instrument for ground-based in situ observations of microphysical properties of mixed-phase clouds

2013

Measurements of the microphysical properties of mixed-phase clouds with high spatial resolution are important to understand the processes inside these clouds. This work describes the design and characterization of the newly developed ground-based field instrument HOLIMO II (HOLographic Imager for Microscopic Objects II). HOLIMO II uses digital in-line holography to in situ image cloud particles in a well-defined sample volume. By an automated algorithm, two-dimensional images of single cloud particles between 6 and 250 μm in diameter are obtained and the size spectrum, the concentration and water content of clouds are calculated. By testing the sizing algorithm with monosized beads a system…

PhysicsAtmospheric ScienceField (physics)Ice crystals010504 meteorology & atmospheric sciencesbusiness.industrylcsh:TA715-787Resolution (electron density)lcsh:Earthwork. FoundationsHolographyCloud computing01 natural sciencesSizingCharacterization (materials science)law.inventionlcsh:Environmental engineering010309 opticslaw0103 physical scienceslcsh:TA170-171businessImage resolutionRemote sensing0105 earth and related environmental sciences
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2014

Abstract. Dynamical and microphysical processes in pyroconvective clouds in mid-latitude conditions are investigated using idealized three-dimensional simulations with the Active Tracer High resolution Atmospheric Model (ATHAM). A state-of-the-art two-moment microphysical scheme building upon a realistic parameterization of cloud condensation nuclei (CCN) activation has been implemented in order to study the influence of aerosol concentration on cloud development. The results show that aerosol concentration influences the formation of precipitation. For low aerosol concentrations (NCN = 200 cm−3), rain droplets are rapidly formed by autoconversion of cloud droplets. This also triggers the f…

PhysicsAtmospheric ScienceMeteorologyIce crystalsTRACERCloud condensation nucleiAtmospheric modelPrecipitationSnowflakeGraupelAerosolAtmospheric Chemistry and Physics
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