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In Fig. 2.45.2 the dependences of Xomax on Adr are shown for Climax NM. From Fig. 2.45.2 can be seen that the region of crossings of Xo max (Adr ) for odd and even cycles is: 13 < Xomax < 16.5 , 1.7% < Ajr < 2.3%. For Huancayo/Haleakala NM this region is: 13 < Xomax < 18,0.23% < Adr < 0.43%. Thus we came to conclusion that the amplitude of the drift effect is about 2.0% for Climax NM and about 0.33% for Huancayo/Haleakala NM. It means that for primary CR with rigidity 10-15 GV a relative contribution of drift effects is about 20-25%. For CR with rigidity 35-40 GV a relative role of drift effects is about 2-3 times smaller. For Xo max we obtained for both 10-15 and 35-40 GV about 15 av. months, what corresponds ro ~ 100 AU (at average solar wind speed 400 km/s).

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Renewable Energy 101

Renewable Energy 101

Renewable energy is energy that is generated from sunlight, rain, tides, geothermal heat and wind. These sources are naturally and constantly replenished, which is why they are deemed as renewable. The usage of renewable energy sources is very important when considering the sustainability of the existing energy usage of the world. While there is currently an abundance of non-renewable energy sources, such as nuclear fuels, these energy sources are depleting. In addition to being a non-renewable supply, the non-renewable energy sources release emissions into the air, which has an adverse effect on the environment.

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