F3 Layers Research Articles

Variability of an additional layer in the equatorial ionosphere over Fortaleza

The day‐to‐day variations (or the weather) of an additional layer, called the F3 layer, that has been predicted to exist at altitudes above the F2 peak in the equatorial ionosphere are studied through ionosonde observations and theoretical modeling. The ionograms recorded in 1995 at the equatorial station Fortaleza (4°S, 38°W; dip angle 9°S) in Brazil show the occurrence of the F3 layer during daytime from 0800 to 1630 LT, with the duration of occurrence ranging from 15 min to 6 hours. Although the layer occurs most frequently (75% of the days) in local summer as previously predicted, there are consecutive and individual magnetically quiet and disturbed days when the layer does not occur. There are also days when the layer reoccurs. The model results, obtained using the Sheffield University plasmasphere‐ionosphere model, show that the day‐to‐day variations of the F3 layer arise from the corresponding variations of the vertical plasma velocity. The layer occurs when the time‐cumulative vertical velocity displaces the daytime F2 peak to high altitudes, to form the F3 layer, while the normal F2 layer develops at low altitudes. Sudden displacements result in more distinct F3 layers than gradual displacements. Model results also show that the plasma temperature within the F3 layer decreases as the plasma density increases, and, like the plasma density, the plasma temperature also undergoes large day‐to‐day variations.

Steroid concentrations in isolated theca and granulosa layers of preovulatory follicles during the ovulatory cycle of the domestic hen.

The purpose of the present investigation was to measure the concentrations of progesterone (P4), testosterone (T) and estradiol-17 beta (E2) in isolated theca and granulosa layers of the five preovulatory follicles of the domestic hen. The largest follicle (F1), the second largest (F2), third largest (F3), fourth largest (F4) and fifth largest (F5) follicles were removed at 24, 18, 12, 6 and 2 h before the expected ovulation. Theca and granulosa layers were isolated and P4, T, E2 and protein concentrations determined. Protein concentrations of the granulosa and theca layers increased 5- and 15-fold, respectively, during the five ovulatory cycles prior to ovulation. As the follicle approached ovulation, there was a linear decrease in E2 concentration of the theca layer with the most significant decrease (P less than 0.001) occurring between 24 and 18 h of the ovulatory cycle. In the F3 and F4 theca layers, there was a significant increase (P less than 0.005) in E2 at 6 h of the ovulatory cycle. Fluctuations in T concentrations in theca and granulosa layers were similar. There was a significant increase (P less than 0.05) in T in both layers of the F2, F3 and F4 follicles at 6 h followed by a decrease (P less than 0.005) in the theca layers at 2 h of the ovulatory cycle. The P4 concentration of the granulosa layer increased gradually during follicular maturation, with the greatest increase occurring in the F2 and F1 granulosa layers between 18 and 12 h of the ovulatory cycle.(ABSTRACT TRUNCATED AT 250 WORDS)