| wuwuoupr | Date: Friday, 15.11.2013, 23:49 | Message # 1 |
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Sergeant
Group: User
Messages: 24
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| Many an diesel RV have manifold heaters installed in them. These run off the battery. They perform the same function as a heating blanket in your bed, but for the fuel lines in your RV. Lower end RVs, on the other hand, usually do not have such heaters. If you have one of these, you can usually get a local tow truck company to come out and apply a heater to area. You do not need an RV specialist. In colder areas, most tow companies perform this service for regular cars when their radiators freeze over.
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This study utilizes a novel technique to map the Defense Meteorological Satellite Program (DMSP) data across the two hemispheres to learn about the morphology and plasma composition of the topside ionosphere, and the underlying ionospheric dynamics. In the southern winter hemisphere, the regional maps tracked a heavy ion (Ni O+) trough,aurora zone, polar hole, and large plasma density depletion. The latter appeared in the region of the South Atlantic Magnetic Anomaly (SAMA). The electron temperature (Te) map detected the thermal characteristics of these features, while the plasma drifts and flux maps tracked their dynamics. Results show that there were special electrodynamic effects in the SAMA region due to the low magnetic field and high conductivity. These increased the vertical downward (VZ) and the westward (VY) drifts. Independently, the VZ and VY maps registered the affected area that was depleted in heavy ions and rich in light ions. Some field aligned profiles tracked the impact of these SAMA effects on the heavy ion trough, which was a stagnation trough and appeared markedly differently at different longitudes. At trough latitudes ((56 4)S (geomagnetic) when Dstav = 0 nT), the elevated electron temperatures forming a Te peak indicated subauroral heating effects. A statistical study modeled the magnetic activity dependence of the Te peak's magnitude and location and revealed their linear correlation with the activity level. Statistically, the Te peak increased <>0.226 1.355]K and moved equatorward <>.051 0.009] (geomagnetic) per 1 nT decrease in the averaged Dst index. Per 1 nT increase in the averaged AE index, its magnitude increased <>.315 0.444]K and the equatorward movement was <>.014 0.003].
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