Interface growth with a shadow instability

1991 ◽  
Vol 66 (16) ◽  
pp. 2104-2107 ◽  
Author(s):  
Christopher Roland ◽  
Hong Guo
Keyword(s):  
Interface Growth

scholarly journals Interface growth driven by a single active particle

2019 ◽  
Vol 100 (5) ◽  
Author(s):  
Prachi Bisht ◽  
Mustansir Barma
Keyword(s):  
Active Particle ◽  
Interface Growth

Amorphous molybdenum silicide layers and Mo/Si(100) interface growth: Local structure and preparation dependence

1990 ◽  
Vol 41 (9) ◽  
pp. 5871-5880 ◽  
Author(s):  
H. L. Meyerheim ◽  
U. Döbler ◽  
A. Puschmann ◽  
K. Baberschke
Keyword(s):  
Local Structure ◽  
Molybdenum Silicide ◽  
Interface Growth

Nonlocal Kardar-Parisi-Zhang equation to model interface growth

2001 ◽  
Vol 64 (1) ◽  
Author(s):  
Persefoni Kechagia ◽  
Yanis C. Yortsos ◽  
Peter Lichtner
Keyword(s):  
Interface Growth

Phase conversion and interface growth in phase-separatedHe3−He4liquid mixtures

2005 ◽  
Vol 72 (14) ◽  
Author(s):  
Haruka Abe ◽  
Takeo Satoh ◽  
Serguei N. Burmistrov
Keyword(s):  
Phase Conversion ◽  
Interface Growth

Kinetic self-stabilization of a stepped interface: growth into a supercooled melt

1995 ◽  
Vol 149 (1-2) ◽  
pp. 120-130 ◽  
Author(s):  
A.A. Chernov ◽  
S.R. Coriell ◽  
B.T. Murray
Keyword(s):  
Interface Growth ◽  
Supercooled Melt ◽  
Self Stabilization

scholarly journals Factors delaying spring runoff in the upper Ürümqi River basin, China

1992 ◽  
Vol 16 ◽  
pp. 225-230 ◽  
Author(s):  
Richard Kattelmann ◽  
Yang Daqing
Keyword(s):  
Snow Cover ◽  
River Basin ◽  
Early Spring ◽  
Ice Formation ◽  
Stream Channels ◽  
Spring Runoff ◽  
Basal Ice ◽  
Interface Growth ◽  
Streamflow Generation ◽  
Soil Interface

Although less than 100 mm of precipitation generally falls during the winter months in the upper Ürümqi River basin, an uneven snowpack of 20 to 100 cm depth is present in early spring. When the surface of this snow cover begins to melt in April, the meltwater is not immediately transformed into streamflow. Several processes are responsible for the five to 15 days of delay in streamflow generation: refreezing in the snow cover itself, creation of a basal ice layer at the snow-soil interface, growth of superimposed ice on the glaciers of the basin, ice formation in stream channels and restoration of high albedo by snowstorms that occur about once a week in spring.

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