Polar Biology

2013 ◽  
Keyword(s):  
Polar Biology

scholarly journals Antarctic Genomics

2004 ◽  
Vol 5 (3) ◽  
pp. 230-238 ◽  
Author(s):  
Melody S. Clark ◽  
Andrew Clarke ◽  
Charles S. Cockell ◽  
Peter Convey ◽  
H. William Detrich III ◽  
...  
Keyword(s):  
Extreme Environments ◽  
Genomic Analysis ◽  
The Novel ◽  
Global Context ◽  
Polar Ecosystems ◽  
Recent Developments ◽  
Genomic Science ◽  
Polar Biology

With the development of genomic science and its battery of technologies, polar biology stands on the threshold of a revolution, one that will enable the investigation of important questions of unprecedented scope and with extraordinary depth and precision. The exotic organisms of polar ecosystems are ideal candidates for genomic analysis. Through such analyses, it will be possible to learn not only the novel features that enable polar organisms to survive, and indeed thrive, in their extreme environments, but also fundamental biological principles that are common to most, if not all, organisms. This article aims to review recent developments in Antarctic genomics and to demonstrate the global context of such studies.

A “Polar Biology Publication” that prevailed: forces at work when Penguins Poo

Polar Biology ◽  
2006 ◽  
Vol 29 (7) ◽  
pp. 541-542
Author(s):  
V. B. Meyer-Rochow ◽  
J. Gal
Keyword(s):  
Polar Biology

scholarly journals A network model for fluid transport through sea ice

2006 ◽  
Vol 44 ◽  
pp. 129-133 ◽  
Author(s):  
J. Zhu ◽  
A. Jabini ◽  
K.M. Golden ◽  
H. Eicken ◽  
M. Morris
Keyword(s):  
Sea Ice ◽  
Fluid Transport ◽  
Laboratory Data ◽  
Grid Method ◽  
Two Dimensions ◽  
Cross Sectional ◽  
Fluid Permeability ◽  
Porous Microstructure ◽  
Polar Biology ◽  
Fully Connected

AbstractThe flow of liquid through porous sea ice is a fundamental process affecting problems in polar biology, oceanography and geophysics. The geometry and connectedness of the pore microstructure of sea ice determine its fluid permeability, which depends strongly on temperature. Here we analyze a simple pipe network as a basis for modeling fluid flow through the complex porous microstructure, and for numerical approximations of the fluid permeability of sea ice as a function of temperature. For slow flow the fluid system is equivalent to an electrical resistor network, and the network is solved using a fast multi-grid method. The radii of the pipes in the network are chosen randomly from distributions describing measured cross-sectional areas of brine inclusions in sea ice. At this stage, the model reflects only the most general features of brine microstructure and its evolution with temperature. Preliminary results for a basic implementation in two dimensions are presented. They are consistent with theoretical bounds on the vertical fluid permeability of sea ice found recently. Moreover, the results agree roughly with laboratory data for higher porosities. For lower porosities and colder temperatures, the fully connected network of pipes in the model, albeit with smaller radii, overestimates observed values. This finding provides evidence that the brine network becomes more disconnected with lower temperatures, which is consistent with transitional behavior near a percolation threshold.

scholarly journals As time goes by: Polar Biology over the years 1982–2008

Polar Biology ◽  
2008 ◽  
Vol 32 (1) ◽  
pp. 3-7 ◽  
Author(s):  
Dieter Piepenburg
Keyword(s):  
Polar Biology
Sign in / Sign up

Export Citation Format

Share Document