The Radiation Balance of Alpine Tundra, Plateau Mountain, Alberta, Canada

1989 ◽  
Vol 21 (2) ◽  
pp. 126 ◽  
Author(s):  
W. G. Bailey ◽  
E. J. Weick ◽  
J. D. Bowers
1997 ◽  
Vol 29 (3) ◽  
pp. 339 ◽  
Author(s):  
Beth-Renee Babrauckas ◽  
Thomas W. Schmidlin

Agrometeoros ◽  
2020 ◽  
Vol 26 (2) ◽  
Author(s):  
Felipe Gustavo Pilau ◽  
Luiz Roberto Angelocci

1969 ◽  
Vol 1 (4) ◽  
pp. 247 ◽  
Author(s):  
Werner H. Terjung ◽  
Ronald N. Kickert ◽  
Gerald L. Potter ◽  
Stanley W. Swarts
Keyword(s):  

1992 ◽  
Vol 56 (5) ◽  
pp. 1379-1384 ◽  
Author(s):  
B. S. Sharratt ◽  
M. J. Schwarzer ◽  
G. S. Campbell ◽  
R. I. Papendick

Molecules ◽  
2021 ◽  
Vol 26 (2) ◽  
pp. 392
Author(s):  
Nobuo Maeda

The nucleation of ice is vital in cloud physics and impacts on a broad range of matters from the cryopreservation of food, tissues, organs, and stem cells to the prevention of icing on aircraft wings, bridge cables, wind turbines, and other structures. Ice nucleation thus has broad implications in medicine, food engineering, mineralogy, biology, and other fields. Nowadays, the growing threat of global warming has led to intense research activities on the feasibility of artificially modifying clouds to shift the Earth’s radiation balance. For these reasons, nucleation of ice has been extensively studied over many decades and rightfully so. It is thus not quite possible to cover the whole subject of ice nucleation in a single review. Rather, this feature article provides a brief overview of ice nucleation that focuses on several major outstanding fundamental issues. The author’s wish is to aid early researchers in ice nucleation and those who wish to get into the field of ice nucleation from other disciplines by concisely summarizing the outstanding issues in this important field. Two unresolved challenges stood out from the review, namely the lack of a molecular-level picture of ice nucleation at an interface and the limitations of classical nucleation theory.


2007 ◽  
Vol 28 (12) ◽  
pp. 2695-2712 ◽  
Author(s):  
C. M. Frey ◽  
G. Rigo ◽  
E. Parlow

Polar Record ◽  
2000 ◽  
Vol 36 (196) ◽  
pp. 3-18 ◽  
Author(s):  
P. Prosek ◽  
M. Janouch ◽  
K. Láska

AbstractThis article presents the results of measurements of the components of ground-surface energy balance (radiation balance, sensible heat flux, latent heat flux, and ground heat flux) taken during the 1994/95 summer season at Poland's Henryk Arctowski Station, King George Island, South Shetland Islands (62°09'42”S, 58°28'10”W). This was the first time that these complex measurements had been taken in the central part of the South Shetlands archipelago. The results are evaluated at the level of daily and seasonal fluctuations. The consequences of energy balance on the temperature conditions of the soil substrata are highlighted. The verification of the degree of influence of a subset of energy-balance components on soil temperature allowed analysis of the relationships among soil temperature, radiation balance, and sensible heat flux. This analysis leads to the conclusion that there is a rapid reaction of the soil temperature to the radiation balance and sensible heat flux to a depth of 5 cm. The boundary atmosphere and soil substrate represent the basic components of the ecotops of the Antarctic vegetation oasis, so these results are interpreted in pedological or botanical studies in the search for environmental influences on the vegetation.


Sign in / Sign up

Export Citation Format

Share Document