Source emission characterization of residential wood-burning stoves and fireplaces: fine particle methyl chloride ratios for use in chemical mass balance modeling

1986 ◽  
Vol 20 (8) ◽  
pp. 803-807 ◽  
Author(s):  
S. A. Edgerton ◽  
M. A. K. Khalil ◽  
R. A. Rasmussen
2008 ◽  
Vol 116 (4) ◽  
pp. 459-466 ◽  
Author(s):  
Jeremy A. Sarnat ◽  
Amit Marmur ◽  
Mitchel Klein ◽  
Eugene Kim ◽  
Armistead G. Russell ◽  
...  

2006 ◽  
Author(s):  
W. Heitbrink ◽  
T. Peters ◽  
D. Evans ◽  
T. Slavin

2001 ◽  
Vol 47 (159) ◽  
pp. 659-664 ◽  
Author(s):  
W. D. Harrison ◽  
D. H. Elsberg ◽  
K. A. Echelmeyer ◽  
R. M. Krimmel

AbstractGlacier response to climate can be characterized by a single time-scale when the glacier changes sufficiently slowly. Then the derivative of volume with respect to area defines a thickness scale similar to that of Jóhannesson and others, and the time-scale follows from it. Our version of the time-scale is different from theirs because it explicitly includes the effect of surface elevation on mass-balance rate, which can cause a major increase in the time-scale or even lead to unstable response. The time constant has a dual role, controlling both the rate and magnitude of response to a given climate change. Data from South Cascade Glacier, Washington, U.S.A., illustrate the ideas, some of the difficulty in obtaining accurate values for the thickness and time-scales, and the susceptibility of all response models to potentially large errors.


2001 ◽  
Vol 35 (25) ◽  
pp. 4347-4355 ◽  
Author(s):  
D Temesi ◽  
A Molnár ◽  
E Mészáros ◽  
T Feczkó ◽  
A Gelencsér ◽  
...  

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