Significant alterations in anisotropic ice growth rate induced by the ice nucleation-active bacteria Xanthomonas campestris

2010 ◽  
Vol 498 (1-3) ◽  
pp. 101-106 ◽  
Author(s):  
Hiroki Nada ◽  
Salvador Zepeda ◽  
Hitoshi Miura ◽  
Yoshinori Furukawa
Cryobiology ◽  
2009 ◽  
Vol 59 (3) ◽  
pp. 373-374
Author(s):  
Hiroki Nada ◽  
Salvador Zepeda ◽  
Yoshinori Furukawa

2011 ◽  
Vol 68 (11) ◽  
pp. 2628-2654 ◽  
Author(s):  
Andrew J. Heymsfield ◽  
Paul R. Field ◽  
Matt Bailey ◽  
Dave Rogers ◽  
Jeffrey Stith ◽  
...  

Abstract Lenticular wave clouds are used as a natural laboratory to estimate the linear and mass growth rates of ice particles at temperatures from −20° to −32°C and to characterize the apparent rate of ice nucleation at water saturation at a nearly constant temperature. Data are acquired from 139 liquid cloud penetrations flown approximately along or against the wind direction. A mean linear ice growth rate of about 1.4 μm s−1, relatively independent of particle size (in the range 100–400 μm) and temperature is deduced. Using the particle size distributions measured along the wind direction, the rate of increase in the ice water content (IWC) is calculated from the measured particle size distributions using theory and from those distributions by assuming different ice particle densities; the IWC is too small to be measured. Very low ice effective densities, <0.1 g cm−3, are needed to account for the observed rate of increase in the IWC and the unexpectedly high linear growth rate. Using data from multiple penetrations through a narrow (along wind) and thin wave cloud with relatively flat airflow streamlines, growth rate calculations are used to estimate where the ice particles originate and whether the ice is nucleated in a narrow band or over an extended period of time. The calculations are consistent with the expectation that the ice formation occurs near the leading cloud edge, presumably through a condensation–freezing process. The observed ice concentration increase along the wind is more likely due to a variation in ice growth rates than to prolonged ice nucleation.


Cryobiology ◽  
2018 ◽  
Vol 85 ◽  
pp. 120-121
Author(s):  
Katharina Dreischmeier ◽  
Lukas Eickhoff ◽  
Carsten Budke ◽  
Thomas Koop
Keyword(s):  

2013 ◽  
Vol 80 (4) ◽  
pp. 1256-1267 ◽  
Author(s):  
Thomas C. J. Hill ◽  
Bruce F. Moffett ◽  
Paul J. DeMott ◽  
Dimitrios G. Georgakopoulos ◽  
William L. Stump ◽  
...  

ABSTRACTIce nucleation-active (INA) bacteria may function as high-temperature ice-nucleating particles (INP) in clouds, but their effective contribution to atmospheric processes, i.e., their potential to trigger glaciation and precipitation, remains uncertain. We know little about their abundance on natural vegetation, factors that trigger their release, or persistence of their ice nucleation activity once airborne. To facilitate these investigations, we developed two quantitative PCR (qPCR) tests of theinagene to directly count INA bacteria in environmental samples. Each of two primer pairs amplified most alleles of theinagene and, taken together, they should amplify all known alleles. To aid primer design, we collected many new INA isolates. Alignment of their partialinasequences revealed new and deeply branching clades, including sequences fromPseudomonas syringaepv.atropurpurea,Ps. viridiflava,Pantoea agglomerans,Xanthomonas campestris, and possiblyPs. putida,Ps. auricularis, andPs. poae. qPCR of leaf washings recorded ∼108inagenes g−1fresh weight of foliage on cereals and 105to 107g−1on broadleaf crops. Much lower populations were found on most naturally occurring vegetation. In fresh snow,inagenes from various INA bacteria were detected in about half the samples but at abundances that could have accounted for only a minor proportion of INP at −10°C (assuming oneinagene per INA bacterium). Despite this, an apparent biological source contributed an average of ∼85% of INP active at −10°C in snow samples. In contrast, a thunderstorm hail sample contained 0.3 INA bacteria per INP active at −10°C, suggesting a significant contribution to this sample.


1993 ◽  
Vol 59 (5) ◽  
pp. 535-543 ◽  
Author(s):  
Masao GOTO ◽  
Masahiko KOMABA ◽  
Tomohiro HORIKAWA ◽  
Noriyuki NAKAMURA

1990 ◽  
Vol 56 (4) ◽  
pp. 515-522
Author(s):  
Masao GOTO ◽  
Kazumu KODAMA ◽  
Ben-Li HUANG

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