Sentences with phrase «for vertical force»

There was no significant difference between sprinters for vertical force production during the second half of the stance phase.

Not exact matches

But wait, there's even more: The vertical and lateral G - force loads for a NASCAR driver average between three and five Gs in banked turns.

That mistake, a few short free kicks and a missed pass or two was all I could find in the negative for this guy, who was completely dominant as the vertical driving force of the offense.

We OTs love getting kids to work on vertical surfaces (think: easel or chalkboard) because of how it forces them to bend their wrists back (called «extension») as they play, something that is critical for good handwriting skills.

More commonly, deformational plagiocephaly occurs postnatally and is associated with congenital torticollis, vertebral anomalies, neurologic impairment, or forced sleeping position.3 — 5 Few reports document any late effects of deformational plagiocephaly other than potential cosmetic concerns and the potential for strabismus, especially involving vertical eye movements.6,, 7 Plagiocephaly may be morphometrically evident in as many as 14 % of adults, but it is rarely recognized.8

Our species is prone to back pain, for example, because our ancestors» imperfect transition to upright walking essentially took a spine similar to that of our nearest living relatives, knuckle - walking chimpanzees, and forced it vertical with piecemeal adaptations.

They found that for an open wheeled racing car weighing around 700 kg, the force of gravity would be 8571N less than the frictional force, meaning the car would easily be able to stay on the vertical banking.

Kelly could reduce the downward force for particularly delicate objects by making the vertical part of her trunk shorter — and increase the force by making the vertical section longer.

Instead, imagine you're pulling the bar down toward your chest in a controlled manner because it will help you maintain the proper body position for generating maximum vertical force.

The end result of this course of thinking was that I essentially disregarded vertical force production and placed far more emphasis on horizontally orientated specialised strength development exercises in the programmes I use for my players and clients.

Comparing the use of a barbell or a barbell plus chains for the clean, using 75 % or 80 % of 1RM with 5 % of chains replacing the same weight of barbell, Berning et al. (2008) found that there was no difference between conditions in relation to peak vertical displacement, peak velocity or rate of force production in the first - pull, transition, or second - pull phases of the clean.

For a person running at a typical casual runner's pace of 2.5 meters per second (9 km / hr, or 5.6 mph) it can be shown, based on data collected by LG Pugh for the study titled «The influence of wind resistance in running and walking and the mechanical efficiency of work against horizontal or vertical forces,» that the energy cost of air resistance while running on solid ground is roughly 0.84 calories per kilometer (this is equivalent to approximately an extra 1.2 % calorie burn relative to a runner on a treadmilFor a person running at a typical casual runner's pace of 2.5 meters per second (9 km / hr, or 5.6 mph) it can be shown, based on data collected by LG Pugh for the study titled «The influence of wind resistance in running and walking and the mechanical efficiency of work against horizontal or vertical forces,» that the energy cost of air resistance while running on solid ground is roughly 0.84 calories per kilometer (this is equivalent to approximately an extra 1.2 % calorie burn relative to a runner on a treadmilfor the study titled «The influence of wind resistance in running and walking and the mechanical efficiency of work against horizontal or vertical forces,» that the energy cost of air resistance while running on solid ground is roughly 0.84 calories per kilometer (this is equivalent to approximately an extra 1.2 % calorie burn relative to a runner on a treadmill).

Very recent research has identified that for any given athlete, it is possible to establish a force - velocity profile in the vertical squat jump (Samazino et al. 2012; 2014) and countermovement jump (Jiménez - Reyes et al. 2014).

For any athlete, it is possible to establish a force - velocity profile (FV) during the vertical jumping movement.

Since strength is velocity - specific, not everyone automatically has an optimal force - velocity profile for producing peak power output in a vertical jump.

Getting back to «body neutral» begins with aligning your skeleton with the vertical force of gravity so that your muscles have the opportunity for their full range of motion.

In a highly niched industry that often forces providers into vertical silos, we've managed to stay «horizontal» on two levels: 1) Delivering an elegant UI / UX for consumers who are trying to make sense of the noise, and 2) Providing an API for developers and analysts seeking a faster path to underlying data that drives their business.

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At the side we find a new set of lower sills, again in clear carbon fiber but with a small red pinstripe... a detail inspired by the Veneno Rosso naturally, at the front the horizontal styling will increase down force while in front of the rear wheel DMC uses another vertical fin... this not only directs more air onto the rear brakes but it also doubles as a stabilizer for straight line high speed driving.

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It allows for changes in vertical loads, and hence optimizes control of braking force the instant load returns to the tires after jumping a crest.

Automatic tailgate opening, BMW emergency call, BMW Online services, BMW teleservices, Brake pad wear indicator warning light, Check control system, Door / boot open warning, Front / rear Parking distance control, Lights on warning, Oil temperature gauge, On board computer, Outside temperature display, Run flat indicator, Service interval indicator, Stop / start button, Bluetooth audio streaming, BMW professional radio / CD / MP3, DAB Digital radio, 2 speed adjustable intermittent wipers with wash / wipe function, Auto dimming rear view mirror, Body colour bumpers, Body colour door handles, Body colour door mirrors, Body colour roof mouldings, Chrome kidney grille with black vertical slats, Door sill finishers, Dual chrome exhaust, Electric adjustable heated door mirrors, Electric front and rear windows with fingertip open / close + anti-trap all round, Follow me home headlights, Headlight range control, Heat insulating tinted glass, Heated windscreen washer jets, High gloss shadow line, LED daytime running lights, LED front fog lights, LED tail lights, M aerodynamic bodystyling, Rain sensor including auto headlights activation, Windscreen with grey shadeband, 12V sockets in front centre console and passenger footwell, 3 spoke leather M multifunction sports steering wheel, 4 grab handles, Anthracite headlining, Anthracite Velour floor mats, Dual zone climate control, Folding front centre armrest with storage compartment, Folding storage compartment with glasses holder + coin tray, Front cupholders x 2, Front door storage with bottle holder, Front head restraints, Front sports seats with electric side bolster adjustment, Front / rear armrests within door panels, Glovebox with lid, Heated front seats, Integrated rear head restraints, ISOFIX child seat preparation + airbag deactivation, Lashing eyelets in boot, Leather gearknob, Leather handbrake grip, Reach + rake adjustable steering column, Rear centre armrest with 2 cupholders, Toolkit located in luggage compartment, Welcome lighting, Extended lights package - 4 Series, 3 point seatbelts on all seats, ABS / EBD, Automatic Stability Control (ASC), Brake assist, CBC -(Cornering brake control), Crash Sensor - activates hazard / interior lighting + unlocks doors, Driver seatbelt warning indicator, Driver / Front Passenger airbags, DSC +, Dynamic brake control, Dynamic Traction Control - DTC, Front seatbelt force limiters, Front seatbelt pretensioner, Front side airbags, Hill start assist, ITS head airbags for front / rear, Side impact protection, Tyre pressure monitor, Warning triangle and first aid kit, Drive away door locking, Electronic immobiliser, Remote central locking, Remote control Thatcham category 1 alarm, Diesel particulate filter, Drive Performance Control, Electronic differential lock, Sports function on gearbox with steering wheel mounted gearshift paddles, Run flat tyres

BMW emergency call, BMW teleservices, Brake pad wear indicator warning light, Check control system, Cruise control with brake function, Door / boot open warning, Lights on warning, Oil temperature gauge, On board computer, Outside temperature display, Run flat indicator, Service interval indicator, Stop / start button, Auxiliary point for auxiliary devices, Bluetooth audio streaming, BMW professional radio / CD / MP3, DAB Digital radio, 2 speed adjustable intermittent wipers with wash / wipe function, Auto dimming rear view mirror, Body colour bumpers, Body colour door handles, Body colour door mirrors, Body colour roof mouldings, Chrome kidney grille with black vertical slats, Daytime running lights, Door sill finishers, Dual chrome exhaust, Electric front and rear windows with fingertip open / close + anti-trap all round, Follow me home headlights, Front fog lights, Headlight washers, Heat insulating tinted glass, Heated windscreen washer jets, Rain sensor including auto headlights activation, Windscreen with grey shadeband, 12V sockets in front centre console and passenger footwell, 3 spoke leather multifunction sports steering wheel, Anthracite Velour floor mats, Dakota leather upholstery, Dual zone climate control, Electrically adjustable front seats - driver seat with memory, Front cupholders x 2, Front door storage with bottle holder, Front head restraints, Front / rear armrests within door panels, Glovebox with lid, Heated front seats, Height adjustable front seats, Integrated rear head restraints, ISOFIX child seat preparation + airbag deactivation, Lashing eyelets in boot, Leather gearknob and handbrake lever, Reach + rake adjustable steering column, Rear centre armrest, Storage compartment behind rear seat, Storage compartment in rear centre console, Storage compartment in rear seat base, Sunvisors with vanity mirrors, Toolkit located in luggage compartment, Extended lights package - 4 Series, ABS / EBD, Automatic Stability Control (ASC), CBC -(Cornering brake control), Crash Sensor - activates hazard / interior lighting + unlocks doors, Driver seatbelt warning indicator, Driver / Front Passenger airbags, DSC +, Dynamic brake control, Dynamic Traction Control - DTC, Front passenger airbag deactivation, Front seatbelt force limiters, Front seatbelt pretensioner, Front side airbags, Hill start assist, Roll over protection, Tyre pressure monitor, Warning triangle and first aid kit, Drive away door locking, Electronic immobiliser, Remote central locking, Remote control Thatcham category 1 alarm, Drive Performance Control, Run flat tyres

That said, there are two visual elements I'd like to adjust in the Kindle app, but can't: There's no control for tweaking line spacing (the vertical height between successive rows of text), and there's no option to disable forced justification.

The muscular forces transferred from the thigh muscles to the lower leg utilise the kneecap as a pulley system, and if these forces are not completely vertical, there is a tendency for a pull on the patella to the medial or inner side of the knee, which causes the instability.

The vertical shoot»em up Sky Force was originally released for Symbian - operated smartphones in 2004.

Battle in the vertical environments of the Underhive, use raised walkways to push a high ground advantage, set traps for unwitting victims, and ambush your foes to force them into bloody melee engagements.

Originally executed for Baxter Travenol Laboratories» newly built corporate headquarters in Deerfield, Illinois, Valentine had conceived of two immense vertical columns standing side by side, but because of architectural modifications (the ceiling in the company's reception area was lowered at a late stage of construction), Valentine was forced to install the two slabs on their sides.

In this case, there has been an identification of a host of small issues (and, in truth, there are always small issues in any complex field) that have involved the fidelity of the observations (the spatial coverage, the corrections for known biases), the fidelity of the models (issues with the forcings, examinations of the variability in ocean vertical transports etc.), and the coherence of the model - data comparisons.

There also should be a vertical line indicating when the forcing adjusted hindcast ends and where the forecast begins for this figure.

First, for changing just CO2 forcing (or CH4, etc, or for a non-GHE forcing, such as a change in incident solar radiation, volcanic aerosols, etc.), there will be other GHE radiative «forcings» (feedbacks, though in the context of measuring their radiative effect, they can be described as having radiative forcings of x W / m2 per change in surface T), such as water vapor feedback, LW cloud feedback, and also, because GHE depends on the vertical temperature distribution, the lapse rate feedback (this generally refers to the tropospheric lapse rate, though changes in the position of the tropopause and changes in the stratospheric temperature could also be considered lapse - rate feedbacks for forcing at TOA; forcing at the tropopause with stratospheric adjustment takes some of that into account; sensitivity to forcing at the tropopause with stratospheric adjustment will generally be different from sensitivity to forcing without stratospheric adjustment and both will generally be different from forcing at TOA before stratospheric adjustment; forcing at TOA after stratospehric adjustment is identical to forcing at the tropopause after stratospheric adjustment).

The hydrostatic equation is the vertical component of the momentum equation (Newton's equation of motion) for the fluid parcel when the forces are in perfect balance and the net acceleration = 0.»

For higher stability, there's a stronger restoring force on any vertical displacement of air (assuming no latent heating occurs), which speeds up the motion associated with the wave causing the wave to propagate faster (i.e. faster phase speed).

Since there are virtually no temperature changes in Lake Tanganyika, there are no driving forces for vertical currents.

The corresponding working quasilinear wave equation for the barotropic azonal stream function Ψm ′ of the forced waves with m = 6, 7, and 8 (m waves) with nonzero right - hand side (forcing + eddy friction) yields (34) u˜ ∂ ∂ x (∂ 2Ψm ′ ∂ x2 + ∂ 2Ψm ′ ∂ y2) + β˜ ∂ Ψm ′ ∂ x = 2Ω sin ϕ cos2 ϕT˜u˜ ∂ Tm ′ ∂ x − 2Ω sin ϕcos2 ϕHκu˜ ∂ hor, m ∂ x − (kha2 + kzH2)(∂ 2Ψm ′ ∂ x2 + ∂ 2Ψm ′ ∂ y2), [S3] where x = aλ and y = a ln -LSB-(1 + sin ϕ) / cos ϕ] are the coordinates of the Mercator projection of Earth's sphere, with λ as the longitude, H is the characteristic value of the atmospheric density vertical scale, T˜ is a constant reference temperature at the EBL, Tm ′ is the m component of azonal temperature at this level, u˜ = u ¯ / cos ϕ, κ is the ratio of the zonally averaged module of the geostrophic wind at the top of the PBL to that at the EBL (53), hor, m is the m component of the large - scale orography height, and kh and kz are the horizontal and vertical eddy diffusion coefficients.

This was because they only had the, now outdated, Clausius statement which physicists now realise is only strictly correct for heat transfers in a horizontal plane, not for conduction, diffusion and convection in a vertical plane when subjected to the force of gravity.

Winds and waves are the major forcing factors for vertical mixing; the degree of mixing depends on the vertical density structure.

Compared to, say, CO2 change, the stratospheric O3 forcing is not global in extent, being very small in the tropics and increasing from mid - to high latitudes; the O3 forcing also differs in its vertical structure, since the radiative forcings for CO2 change in both the troposphere and surface are of the same sign (WMO, 1986).

This is further substantiated by Christiansen (1999) who shows that the higher climate sensitivity for upper stratospheric O3 losses relative to lower stratospheric depletion is related to the vertical partitioning of the forcing, in particular the relative roles of short - wave and long - wave radiation in the surface - troposphere system.

However, even without the actual results from the models for the past 30 years, I think we can surmise that driven by changes in anthropogenic forcings alone, the models simulations of the past 30 years would be trending in a similar direction as the model projections for the future, that is, vertical stability and wind shear should be increasing, at least over the tropical Atlantic.

Those waves dominate the vertical velocity field in the mixed layer (vortex Rossby waves) and below the first hundred meters (near inertial waves) and they are responsible for the differences in the vertical transport properties under the various forcing fields as quantified by frequency spectra, vertical velocity profiles and vertical dispersion of Lagrangian tracers.

The set - up of the numerical experiments suggests that the temporal resolution of the atmospheric forcing field is responsible for the significant increase in vertical velocities, in agreement with previous studies (Danioux et al., 2008; Komori et al., 2008).

It needs to be expanded to account for the vertical and regional structure of radiative forcing and also for nonradiative climate forcings.

When the domain is forced by monthly winds, the vertical velocities over flat bathymetry are extremely small most of the time; however, in simulations forced by daily and six - hourly winds and heat fluxes, the magnitude of the vertical velocities is several times larger than for monthly winds throughout the water column.

For a given percentage change in the vertical structure of ozone, the largest dependence of the radiative forcing is in the upper troposphere and ozone layer regions (e.g., TAR, Figure 6.1).