Not exact matches
Exhibitor: Magnum Powers Superchargers Phone: 520-971-1888 Fax: 520-468-2464 Email:
[email protected] Website: http://magnumpowers.com/ Booth Number: 38063 Customizer / Builder: SPS Autosport, ES Tuned, Larry's Engine and
Marine, Tucson, Arizona Powertrain / Drivetrain: Jeep 4.0 L bored and stroked to 5.0 L; Magnum Powers Mx90 1,500 cc supercharger kit, 85 mm throttle body,
air intake upgrade and intercooler; Bosch injectors; Snow methanol injection; ceramic - coated intake manifold; Banks headers; braided header heat shield; SPS Autosport exhaust; MagnaFlow muffler; Spal electric fan; RaceTec custom pistons; Comp Cam hydraulic lifters, camshaft and roller rockers; Mishimoto radiator, radiator hoses, catch can and oil
cooler; silicon couplers for supercharger and
air intake; XS Power battery; Evan's coolant Chassis: Centerline wheels; Rusty's Offroad 5.5 - in.
Frequently, particularly during the «May gray / June gloom» period, a thick «
marine layer» cloud cover keeps the
air cool and damp within a few miles of the coast, but yields to bright cloudless sunshine approximately 5 — 10 miles (8.0 — 16.1 km) inland.
The area is annually affected by a
marine layer caused by the
cool air of the Pacific Ocean meeting the warm
air over the land.
A sea breeze, which is caused by the temperature and pressure difference between warm areas inland and the
cool air over the ocean, often develops on warm summer days as well, increasing the on - shore flow pattern and maintaining a constant flow of
marine stratus clouds onto the coastal areas.
However, the moderating influence of
cool,
marine air, combined with daily fog, extends activity throughout the summer.
When temperatures rise, so does the
air, pulling
cool, moist
marine air inland onto the beaches like a foggy blanket.
Marine air temperatures and lower troposphere temperatures
cool in response because the tropical Pacific is releasing less heat than normal through evaporation as a result of the
cooler surface waters.