BROWSE - VOLUME LIST
- A - Physics of the Earth's Interior
- B - Seismology
-
C - Geomagnetism
C-118, C-117, C-116, C-115, C-114, C-113, C-112, C-111, C-110, C-109, C-108, C-107, C-106, C-105, C-104, C-103, C-102, C-101, C-100, C-99, C-98, C-97, C-96, C-95, C-94, C-93, C-92, C-91, C-90, C-89, C-88, C-87, C-86, C-85, C-84, C-83, C-82, C-81, C-80, C-79, C-78, C-77, C-76, C-75, C-74, C-73, C-72, C-71, C-70, C-69, C-68, C-67, C-66, C-65, C-64, C-63, C-62, C-61, C-60, C-59, C-58, C-57, C-56, C-55, C-54, C-53, C-52, C-51, C-50, C-49, C-48, C-47, C-46, C-45, C-44, C-43, C-42, C-41, C-40, C-39, C-38, C-37, C-36, C-35, C-33, C-32, C-31, C-30, C-29, C-28, C-27, C-26, C-25, C-24, C-23, C-22, C-21, C-20, C-19, C-18, C-17, C-16, C-15, C-14, C-13, C-12, C-11, C-10, C-9, C-8, C-7, C-6, C-5, C-4, C-3, C-2, C-1
-
D - Physics of the Atmosphere
D-79, D-78, D-77, D-76, D-75, D-74, D-73, D-72, D-71, D-70, D-69, D-68, D-67, D-66, D-65, D-64, D-63, D-62, D-61, D-60, D-59, D-58, D-57, D-56, D-55, D-54, D-53, D-52, D-51, D-50, D-49, D-48, D-47, D-46, D-44, D-45, D-43, D-42, D-41, D-40, D-39, D-38, D-37, D-35, D-34, D-33, D-32, D-31, D-30, D-28, D-27, D-26, D-25, D-24, D-23, D-22, D-21, D-20, D-19, D-18, D-17, D-16, D-15, D-14, D-13, D-12, D-11, D-10, D-9, D-8, D-7, D-6, D-5, D-4, D-3, D-2, D-1
- E - Hydrology
- P - Polar Research
- M - Miscellanea
-
Online First
D - Physics of the Atmosphere
Atmospheric Ozone, Solar Radiation, 1984
Author(s):
Volume: 189
Series: D-22
Volume: 189
Series: D-22
Ozone observations have been made by means of Dobson spectrophotometer No. 84 in the Geophysical Observatory at Belsk since March 1963. This publication presents all total ozone values and vertical distribution of ozone over Belsk in 1984 obtained from the conventional Umkehr observations.
The Structure of Turbulence in the Surface Layer of the Atmosphere
Author(s): Borkowski J.
Volume: 183
Series: D-21
Volume: 183
Series: D-21
In the paper a model of turbulence is developed and applied to predict surface layer characteristics. The model contains equations for Reynolds stresses, turbulent heat flux, temperature variance, and turbulence energy dissipation rate. The closure is achieved by applying the gradient type hypothesis for diffusive terms, and modeling pressure terms, expressing them in terms of second order moments. The form adopted for pressure terms included also correction accounting for proximity of the underlying surface. Numerical solutions of the model equations are presented and compared with experimental data and similarity predictions. In most cases the model predictions agree with the data reasonably well.
Atmospheric Ozone, Solar Radiation, 1983
Author(s):
Volume: 178
Series: D-20
Volume: 178
Series: D-20
Ozone observations have been made by means of Dobson spectrophotometer No. 84 in the Geophysical Observatory at Belsk since March 1963. This publication presents all total ozone values and vertical distribution of ozone over Belsk in 1983 obtained from the conventional Umkehr observations. Ozone profiles obtained from the short and multi-wavelength Umkehr observations taken in 1982 and 1983 are presented in this issue.
Électricité Atmosphérique et Météorologie Observatoire Géophysique de S. Kalinowski à Świder 1983
Author(s):
Volume: 177
Series: D-19
Volume: 177
Series: D-19
This volume contains the results of recordings of some elements of atmospheric electricity and daily observations of major meteorological factors, noted at the S. Kalinowski Geophysical Observatory of the Polish Academy of Sciences at Świder in 1983.
Atmospheric Ozone 1982 and 1963-1981, Solar Radiation 1982
Author(s):
Volume: 169
Series: D-18
Volume: 169
Series: D-18
Ozone observations have been made by means of Dobson spectrophotometer No. 84 in the Geophysical Observatory at Belsk since March 1963. This publication presents all total ozone values and vertical distribution of ozone over station Belsk in 1982 as well as the revised 19-year total ozone data.