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ford fusion evaporator discharge air temperature sensor


Vinyl windows are a great replacement option because they are easy to install. Moreover these widows prove to be energy efficient fixtures that regulate the room temperature well as well as are a cost effective interior decor option.

Brake Booster Market - Freescale Semiconductor

PERFOMANCE BOOST The Freescale* MPXV4115V pressure sensor is the ideal part for automotive vacuum sensing needs such as those found in the brake booster application. Prepared by Marc Osajda Automotive Sensor Marketing Motorola – Toulouse, France Advanced braking systems are becoming increasingly common in today’s automobiles. Higher level systems and technology now being used in “brake assist systems” (BAS) in several European cars, have made it possible for more efficient and intelligent braking systems. A key functional application block found in these braking systems that has advanced with this technology surge, is the vacuum brake booster function. Here are a few driving factors behind the need and use of the brake booster, which helps ensure a safer braking system. Independent Systems: In current gasoline engine cars, the engine’s intake manifold generates the vacuum for the brake booster. This system works fine with one exception. The amount of vacuum in the brake booster is unknown by the braking system. Thus the amount of amplification is also unknown. If heavy braking is needed, there is no possibility for the brake system to interact with the intake manifold if additional amplification is required. The manufacturer’s interest for having the vacuum generated by an auxiliary vacuum pump is that the brake system can manage the amount of vacuum as required, on demand. This in turns gives it the ability to perform amplification on its own, giving it complete independent from the engine’s operating condition. The auxiliary pump is also able to provide higher amounts of vacuum whenever necessary. In situations calling for heavy braking, the pressure will naturally decrease in the brake booster, also causing a decrease in the amplification during braking. With an external pump it is possible to maintain, or even increase the amplification during a heavy braking phase. Smart Safety: Wheel blocking due to high-braking force is controlled by the Anti-Lock Brake System (ABS). However, it has been observed that in many cases, drivers do not...

Excelon RNT Clear Flexible PVC Tubing Specifications

Clear Flexible PVC Tubing • Clear material, with a dense, smooth bore • Resistant to oxidation, chemicals and bacteria • Chemical or thermal bonding • Can be gas or radiation sterilized Physical Properties** • Extreme flexibility permits easy set-ups RNT Hardness, Shore A Tensile Strength, psi Elongation at Break, % Brittle Temperature, °F Specific Gravit y 68 2000 400 -41 1.20 • Available in transparent or opaque colors • Flushes clean with most conventional cleaners and sanitizers ** Values listed are typical and are meant only as a guide to aid in design. Field testing should be performed to find the actual values for your application. RNT ID OD SIZE NO. WALL LBS./FT. MAX.WKG. PSI AT 68°F STD. LENGTHS PART NO. 1/16 3/32 0.120 1/8 1/8 5/32 5/32 0.170 3/16 3/16 3/16 3/16 1/4 1/4 1/4 5/16 5/16 5/16 3/8 3/8 3/8 3/8 3/8 7/16 7/16 7/16 1/8 5/32 0.170 3/16 1/4 7/32 11/32 1/4 5/16 1/4 3/8 7/16 3/8 7/16 1/2 7/16 1/2 9/16 1/2 3/4 7/8 9/16 5/8 9/16 5/8 11/16

2009 Hayabusa - PCV - MPS Racing
by nkono 0 Comments favorite 4 Viewed Download 0 Times

Parts List Power Commander USB Cable CD-ROM Installation Guide Power Commander Decals Dynojet Decals Velcro® Strip Alcohol Swab Wire tap O2 eliminator The ignition MUST be turned OFF before installation! YOU CAN ALSO DOWNLOAD THE POWER COMMANDER SOFTWARE AND LATEST MAPS FROM OUR WEB SITE AT: WWW.POWERCOMMANDER.COM PLEASE READ ALL DIRECTIONS BEFORE STARTING INSTALLATION 2191 Mendenhall Drive 20-008 North Las Vegas, NV 89081 (800) 992-4993 2009 Suzuki Hayabusa PCV - 1 POWER COMMANDER V INPUT ACCESSORY GUIDE A C C E S S O RY I N P U T S Map - The PCV has the ability to hold 2 different base maps. You can switch on the fly between these two base maps when you hook up a switch to the MAP inputs. You can use any open/close type switch. The polarity of the wires is not important. When using the Autotune kit one position will hold a base map and the other position will let you activate the learning mode. When the switch is “CLOSED” Autotune will be activated. Shifter- These inputs are for use with the Dynojet quickshifter. Insert the wires from the Dynojet quickshifter into the SHIFTER inputs. The polarity of the wires is not important. Speed- If your application has a speed sensor then you can tap into the signal side of the sensor and run a wire into this input. This will allow you to calculate gear position in the Control Center Software. Once gear position is setup you can alter your map based on gear position and setup gear dependent kill times when using a quickshifter. USB CONNECTION CRANK ANALOG EXPANSION PORTS 1 & 2 Optional Accessories such as Color LCD unit or Auto tune kit.

RCC Turbos - Stage 1 Turbo Install - Suzuki Hayabusa - Gen 1

RCC Turbos - Stage 1 Turbo Install: Suzuki Hayabusa (Gen 1) • Preparation/Disassembly: Remove the seat. Disconnect negative terminal on the battery. Drain the fuel tank. Remove the fuel tank. Remove the stock fuel pump from the tank. Remove the air box. Remove the MAP sensor and temperature sensor from the air box. Remove left and right side fairings. Drain engine oil. Drain engine coolant. Remove the oil filter Remove the oil restrictor, behind the filter. Remove the oil cooler lines. Remove the radiator and oil cooler, as one unit, leaving only the bracket/support for radiator (before reinstalling the radiator please remove all the tabs along the bottom of the radiator). Remove the entire exhaust system. Remove the PAIR system. Remove the oil pan from the engine. • Sensor Bracket Modification: On the left hand side of bike, on the inside of the frame, you will see a bracket, with a plastic vacuum canister, vacuum control solenoid valve, atmospheric pressure sensor, and some vacuum lines, with a check valve in the vacuum line. Please remove this entire bracket, eliminate all the vacuum lines, the plastic canister, and the control solenoid valve, and also cut off the metal tab that held the vacuum canister. Then reinstall this bracket with only the atmospheric pressure sensor, and plug the wires back in. • Tap/plug PAIR System Holes: Tap the four small PAIR system holes, above the exhaust ports, with an M6 x 1.0 tap. Install the four small M6 screws into the exhaust holes after tapping them. • Modify the Oil Pan: Drill a ¾” hole on the left side of the oil pan. Use thread sealant on the washer, and red Loctite on the threads. Make sure the sealing washer is against the inside of pan, then the stainless flat washer, then the nut. Once the fitting is installed, reinstall the oil pan. • Install Header/Turbo/Oil Lines/Exhaust: Install the header and turbo as a unit, but with the bolts loose. Use four of your original header bolts on the top of the turbo header (Allen head). Use the four new bolts on the bottom row of the header (M8, 10mm flange head). PLEASE NOTE! After installing the dump pipes and waste gate, the nipple on the top of the waste gate remains open, and no hose gets installed on the top fitting. The top fitting is used for boost control on Stage 2 and higher end kits. It is not used on Stage 1 kits.

Savage Gulf Trail Map - Friends of South Cumberland State ...

GREETER TRAIL General Description: This short trail connects the Alum Gap Camp Area with the Greeter Falls Area. The first mile is an easy plateau top walk with the last half mile a moderate gorge walk. The falls are sometimes dry but there is always a cool water hole at the bottom. Miles Trail Description: 0.0 Trail begins at Alum Gap, 1 mile down Big Creek Gulf Trail from camping area. Big Bluff Overlook to left. 0.2 1.0 Suspension Bridge across Boardtree Creek, junction of Greeter Falls Loop Trail. 1.3 Trail splits—left is Lower Falls (50’ high) and plunge pool; right is Upper Falls (15’ high) Greeter Falls. 1.4 General Description: This long, difficult trail is designed to accommodate extended trips. Half the length is the Collins River Gorge and the other half is along the east rim. The gorge section has many beautiful geological features. Trail is closed during part of winter due to dangerous ice buildup at 6.3. Miles Trail Description: Trail begins atop Peak Mountain at the end of the South Rim Trail and the Stage 0.0 Road Historic Trail. 0.5 Blue Branch Overlook to the right, an outstanding view of a short tributary gorge and the main gulf. Ford of Blue Branch; thick Rhododendron growth. 1.1 Horsepound Point Overlook to right. 1.8 2.4 Standing Rock Overlook to right. 2.6 Collins River Overlook to right. 3.0 A small stream is forded with the remains of an old moonshine still visible to the left. Another still site to the left on a larger stream. 4.7 4.9 Collins East Camp Area to left. 5.3 Collins River is crossed on a 100’ suspension bridge, above huge boulders. 6.2 Collins West Camp Area on trail straight ahead; main trail to right. Camp area is on the mountaintop and has the best overlook along the trail—Rocky Point. There is also a parking area from 55th AVE off HWY 108, 1/4th mile out access trail from campsite. 6.3 The spectacular triple waterfall of Rocky Mountain Creek, a huge overhang, and creek ford. A large mound of fallen rocks and exceptionally large Chestnut Oak Tree to trail 6.8 right; start of descent.....

Pressure Sensor Market by 2017
by mnmdylan 0 Comments favorite 26 Viewed Download 0 Times

Recent report published by MarketsandMarkets forecast that the value of pressure sensor market was $5.11 billion in 2011 and is expected to reach $7.34 billion in 2017, at an estimated CAGR of 6.3% from 2012 to 2017.

Panasonic Lumix DMC-GX7 Mirrorless Micro Four Thirds Digital Camera Body Only - Black

Panasonic Lumix DMC-GX7 Mirrorless Micro Four Thirds Digital Camera Body Only - Black available for just £509.00 from Tip Top Electronics UK with fast shipping.It is a compact digital camera that features a 16 megapixel Micro Four Thirds Digital Live MOS sensor and Venus Engine image processor to produce high resolution imagery with notable low-light sensitivity to ISO 25600.

Overestimated global warming over the past 20 years

G lobal mean surface temperature over the past 20 years (1993–2012) rose at a rate of 0.14 ± 0.06 °C per decade (95% confidence interval)1. This rate of warming is significantly slower than that simulated by the climate models participating in Phase 5 of the Coupled Model Intercomparison Project (CMIP5). To illustrate this, we considered trends in global mean surface temperature computed from 117 simulations of the climate by 37 CMIP5 models (see Supplementary Information). These models generally simulate natural variability — including that associated with the El Niño–Southern Oscillation and explosive volcanic eruptions — as well as estimate the combined response of climate to changes in greenhouse gas concentrations, aerosol abundance (of sulphate, black carbon and organic carbon, for example), ozone concentrations (tropospheric and stratospheric), land use (for example, deforestation) and solar variability. By averaging simulated temperatures only at locations where corresponding observations exist, we find an average simulated rise in global mean surface temperature of 0.30 ± 0.02 °C per decade (using 95% confidence intervals on the model average). The observed rate of warming given above is less than half of this simulated rate, and only a few simulations provide warming trends within the range of observational uncertainty (Fig. 1a). The inconsistency between observed and simulated global warming is even more striking for temperature trends computed over the past fifteen years (1998–2012). For this period, the observed trend of 0.05 ± 0.08 °C per decade is more than four times smaller than the average simulated trend of 0.21 ± 0.03 °C per decade (Fig. 1b). It is worth noting that the observed trend over this period — not significantly...

European and Global Climate Change Projections - ClimateCost

2.4°C to 3.4°C rise in global temperature by the period 2071-2100 (A1B)1 • nalysis of the future impacts and economic costs of climate change A requires climate models. These models require inputs of future greenhouse gas emissions, based on modelled global socio-economic scenarios, to make projections of future changes in temperature, precipitation and other meteorological variables. • he ClimateCost project has considered three emissions scenarios: T a medium-high non-mitigation baseline scenario (A1B); a mitigation scenario (E1), which stabilises global temperature change at about 2°C above pre-industrial levels; and a high-emission scenario (RCP8.5). • Under a medium-high emission baseline (A1B), with no mitigation, the climate models considered in ClimateCost show that global average temperatures could rise by between 1.6°C and 2.3°C by 2041-2070, and 2.4°C and 3.4°C by 2071-2100, relative to the modelled baseline period used in the project of 1961-1990. However, the models project much larger temperature increases for Europe in summer, and strong regional differences across countries, for example, the Iberian Peninsula has a mean projected increase of up to 5°C by 2071-2100. 1.5°C rise in global temperature with mitigation (E1)1 Uncertainty in the climate projections between emissions scenarios and climate models for Europe is considerable These values are reported for a future average time period over 30 years, relative to a 1961-1990 baseline. They report the Ensembles Project results used in the ClimateCost project, not the full IPCC AR4 range. 1 02/03 2/2 European and Global Climate Change Projections • The differences in the precipitation projections between the models are much greater and the distributional patterns across Europe are more pronounced than for temperature. Nonetheless, there are some robust patterns of change. There are wetter winters projected for Western and Northern Europe. By contrast, there are drier conditions projected all year for Southern Europe, where summer precipitation could be reduced by 50% by the end of the century. In other parts of Europe, the changes are more uncertain, and the models even project differences in the direction of change (i.e. whether increases or decreases will occur).

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