𝔖 Bobbio Scriptorium
✦   LIBER   ✦

Dependence of the correlation of small scale photospheric structures upon resolution

✍ Scribed by R. G. Teske; G. H. Elste


Publisher
Springer
Year
1979
Tongue
English
Weight
596 KB
Volume
62
Category
Article
ISSN
0038-0938

No coin nor oath required. For personal study only.

✦ Synopsis


Correlations between continuum intensity, velocity, and equivalent widths of two Mn I lines as observed with two different entrance apertures tend to deteriorate with improvement in spatial resolution. The KPNO muitichannel magnetograph was used to make area scans at the center of the disk with entrance apertures 3.5" β€’ 2.5" arc and 1" β€’ 1" arc. A coherence analysis shows that this effect is caused by marked differences of fluctuations in temperature and temperature gradients as well as in the velocity structure of photospheric elements of various sizes.


πŸ“œ SIMILAR VOLUMES


The use of the Goldberg-Unno method for
✍ E. Gurtovenko; V. Troyan πŸ“‚ Article πŸ“… 1971 πŸ› Springer 🌐 English βš– 478 KB

The Goldberg-Unno method is analysed. Accounting for the instrumental profile correction reduces the derived microturbulent velocities only slightly. A similar effect may be caused by an unresolved macroturbulence. The method of accounting for the damping effect is considered. The correction for the

Dependence of dissolved carbohydrate con
✍ C. M. Burney; P. G. Davis; K. M. Johnson; J. Mc N. Sieburth πŸ“‚ Article πŸ“… 1981 πŸ› Springer-Verlag 🌐 English βš– 718 KB

Significant correlations between trophic components of the <20/~m microbial plankton and the concentrations of total dissolved carbohydrate (TCHO) and polysaccharide (PCHO) have been found at two drogued buoy stations which were sampled at 3 or 4-h intervals over diel cycles. An attempt was made to

The temperature dependence of small-scal
✍ G. ZΓ€ngl πŸ“‚ Article πŸ“… 2008 πŸ› John Wiley and Sons 🌐 English βš– 757 KB

## Abstract This study presents idealized numerical simulations to analyze the temperature dependence of small‐scale orographic precipitation enhancement in a non‐convective environment for a variety of mountain heights. The investigation is motivated by a climatological analysis of several rain‐ga