INTERPOLATION FORMULAS FOR DETERMINING WIND SPEED IN THE BOUNDARY LAYER OF THE ATMOSPHERE.

被引：0

|

作者：

Byzova, N.L.

机构：

来源：

Soviet meteorology and hydrology | 1986年 / 03期

关键词：

D O I：

暂无

中图分类号：

学科分类号：

摘要：

9

引用

收藏

页码：9 / 15

相关论文

共 50 条

[11] The isothermal layer of the atmosphere.
Chref, C
NATURE, 1908, 77 : 437 - 437
[12] The isothermal layer of the atmosphere.
Dines, WH
NATURE, 1909, 79 : 459 - 459
[13] The isothermal layer of the atmosphere.
Dines, WH
NATURE, 1908, 77 : 390 - 390
[14] The isothermal layer of the atmosphere.
Dines, WH
NATURE, 1908, 77 : 486 - 486
[15] The specific speed of ions in the atmosphere.
Mache, H
von Schweidler, E
PHYSIKALISCHE ZEITSCHRIFT, 1905, 6 : 71 - 73
[16] Influence of the speed of the wind on the vertical and the variations of the meteorological elements in the lower layers of the atmosphere.
Brazier, CE
COMPTES RENDUS HEBDOMADAIRES DES SEANCES DE L ACADEMIE DES SCIENCES, 1919, 168 : 179 - 182
[17] APPROXIMATE SOLUTION OF BOUNDARY PROBLEM FOR OPTICALLY INHOMOGENEOUS LAYER AND INTERPOLATION FORMULAS
MIROVITS.DI
BUDAGYAN, IF
OPTIKA I SPEKTROSKOPIYA, 1972, 33 (03): : 537 - &
[18] A new method of determining the emanation content of the atmosphere.
Messerschmidt, W
PHYSIKALISCHE ZEITSCHRIFT, 1931, 32 : 548 - 549
[19] FEATURES OF THE TEMPERATURE AND WIND DISTRIBUTIONS IN THE UPPER ATMOSPHERE.
Ryazanova, L.A.
Speranskii, K.E.
Tarasenko, D.A.
Soviet Meteorology and Hydrology (English Translation of Meteorologiya i Gidrologiya), 1976, (11): : 17 - 23
[20] Lagrange Interpolation and the Newton–Cotes Formulas on a Bakhvalov Mesh in the Presence of a Boundary Layer
A. I. Zadorin
N. A. Zadorin
Computational Mathematics and Mathematical Physics, 2022, 62 : 347 - 358

← 1 2 3 4 5 →