Welcome de KL7J
Soldotna - Alaska.

The indexes now.

From Space WX : "When Bz is south (Bz -), that is, opposite Earth's magnetic field, the two fields link up," explains Christopher Russell, a Professor of Geophysics and Space Physics at UCLA. "You can then follow a field line from Earth directly into the solar wind" -- or from the solar wind to Earth. South-pointing Bz's open a door through which energy from the solar wind can reach Earth's atmosphere! Southward (-Bz) often heralds widespread auroras, triggered by solar wind gusts or coronal mass ejections that are able to inject energy into our planet's magnetosphere." [-Bz]. The HF propagation is usually negatively impacted during these events. Even during +Bz, the AK conditions can be difficult.

What might occur or recent history.

Possible storm Pre and Post Enhancements

(Auroral Zone in the center row of chart represents South Central AK)


DX openings at higher MUF's during the increasing ionization before the upset magnetic field impacts the bands, or on the down side with the magnetic field back normal before ionization decreases substantially.
This is usually called pre-enhancement or post-enhancement and is somewhat intuitive.

High levels of geomagnetic activity degrade the ability of the ionosphere to propagate HF radio signals.

The above estimates what can be seen visually, HF radio propagation is affected even further south.

Below an index forecast and a table for interpetation. The farther north, the more pronounced the upsets and possible aurora.

27 day forecast Link

Nasa long range forecast Link to interesting details

Propagation characteristics in the north.

The farther North or South of the equator is significant.
* Central and South-Central Alaska do not get the
higher band openings (MUF) as often or as long *

The daytime F region frequencies peak not at the magnetic equator, but around 15 to 20 degrees north and south of it. This is called the equatorial anomaly. At night, frequencies reach a minimum around 60 degrees latitude north and south of the geomagnetic equator. This is called the mid-latitude trough. Large tilts can occur in the vicinity of these phenomena which may lead to variations in the range of sky waves that have reflection points nearby.
The ionosphere becomes quite variable in the polar regions due to the variable energy input from the solar wind. The near-vertical magnetic field funnels particles into this region and changes in energy input can trigger atmospheric waves and dramatic changes in the electron profile over short time scales. Link to details and source.

This graph shows highest frequencies refracted vertically from the E and F2 region at noon (Day hemisphere) and midnight (Night hemisphere).
high latitude issues

Note from The high-latitude ionosphere and its effects on radio propagation by: R.D.Hunsucker, J.K. Hargreaves, 2003.

The low-latitude zone, spanning 20 or 30 deg either side of the magnetic equator, is strongly influenced by electromagnet forces that arise because the geomagnetic field runs horizontally over the magnetic equator. The primary consequence is that the electrical conductivity is abnormally large over the equator…
At high latitudes we find the opposite situation. Here the geomagnetic field runs nearly vertical, and this simple fact of nature leads to the existence of an ionosphere that is considerably more complex than that in either the middle or the low-latitude zones. "This happens because the magnetic field-lines connect the high latitudes to the outer part of the magnetosphere which is driven by the solar wind, whereas the ionosphere at middle latitude is connected to the inner magnetosphere which essentially rotates with the Earth and so is less sensitive to external influence."


The Magnetic North Pole is close to Alaska compared to most DX countries.
This geatly impacts propagation on the high and low bands MUF and absorption.
Near polar paths are very impacted.

Magnetic North
Link Link2

More information here.

The above chart illustrates the global contours and different levels of ionization real time.
You can examine latitude and in darkness and daylight locations.

This is a K=4 index level according to Univ of Alaska, Geophysical Institute.

Link to other K levels