Space and time variations in the fine structure of the upper atmosphere according to acoustic sounding data

2016 ◽  
Vol 52 (2) ◽  
pp. 176-187 ◽  
Author(s):  
S. N. Kulichkov ◽  
I. P. Chunchuzov ◽  
G. A. Bush ◽  
A. A. Mishenin ◽  
E. V. Golikova
Symmetry ◽  
2020 ◽  
Vol 12 (3) ◽  
pp. 344
Author(s):  
T. D. Le

Astrophysical tests of current values for dimensionless constants known on Earth, such as the fine-structure constant, α , and proton-to-electron mass ratio, μ = m p / m e , are communicated using data from high-resolution quasar spectra in different regions or epochs of the universe. The symmetry wavelengths of [Fe II] lines from redshifted quasar spectra of J110325-264515 and their corresponding values in the laboratory were combined to find a new limit on space-time variations in the proton-to-electron mass ratio, ∆ μ / μ = ( 0.096 ± 0.182 ) × 10 − 7 . The results show how the indicated astrophysical observations can further improve the accuracy and space-time variations of physics constants.


1974 ◽  
Vol 36 (11) ◽  
pp. 1841-1849 ◽  
Author(s):  
Yu.D Iljichev ◽  
I.A Lysenko ◽  
A.D Orlyansky ◽  
Yu.I Portnyagin

2016 ◽  
Vol 43 (3) ◽  
pp. 438-447 ◽  
Author(s):  
L. V. Kuksina ◽  
N. I. Alekseevskii

1976 ◽  
Vol 6 (3) ◽  
pp. 247-252 ◽  
Author(s):  
Erwin R. Berglund ◽  
Arnett C. Mace Jr.

Diurnal albedo relationships were determined for black spruce (Piceamariana (Mill.) B.S.P.) and sphagnum–sedge bogs in northern Minnesota. Two opposing, cart-mounted, Kipp and Zonen pyranometers traversed a tramway to integrate space and time variations of incoming and reflected solar radiation (waveband 0.3–3.0 microns (μ)).The black spruce stand's diurnal albedo was parabolic. Albedo increased with solar altitude to a maximum at 1200 h (7–8%) and then decreased. Greatest within-season variation occurred during June and September. Canopy roughness was the dominant influence on albedo variation and differences.The sphagnum–sedge type diurnal albedo was M-shaped. A minimum albedo between two maxima occurred at 1200 h. Albedos increased from the 1200-h minimum to each maxima as a result of reported surface 'flattening' effects, increased specular reflection, and changes in solar radiation quality. Albedos before the first and after the second maxima were dominated by the microrelief roughness of the sphagnum–sedge hummocks.


2020 ◽  
Vol 47 (4) ◽  
pp. 629-640
Author(s):  
N. M. Shesterkina ◽  
V. P. Shesterkin ◽  
V. S. Talovskaya ◽  
T. D. Ri

2019 ◽  
Vol 46 (S1) ◽  
pp. S74-S84 ◽  
Author(s):  
R. G. Dzhamalov ◽  
K. G. Vlasov ◽  
K. G. Myagkova ◽  
O. S. Reshetnyak ◽  
T. I. Safronova

Sign in / Sign up

Export Citation Format

Share Document