Sentences with phrase «force feedback strength»

The amount of trigger rumble is controlled together with Force Feedback strength via the Force Feedback slider.

Not exact matches

Some workers believe that the strength of the orbital forcing is too small to trigger glaciations, but feedback mechanisms like CO2 may explain this mismatch.

However, mat Pilates can actually be the most difficult form of Pilates training, because you are forced to find all the work from your own muscular strength without the feedback of the apparatus.

The margin of error in various «forcings» and feedback loop strengths is so big that there is a reasonable probability that global climate will cool in the next decade.

«By comparing the response of clouds and water vapor to ENSO forcing in nature with that in AMIP simulations by some leading climate models, an earlier evaluation of tropical cloud and water vapor feedbacks has revealed two common biases in the models: (1) an underestimate of the strength of the negative cloud albedo feedback and (2) an overestimate of the positive feedback from the greenhouse effect of water vapor.

Polar amplication is of global concern due to the potential effects of future warming on ice sheet stability and, therefore, global sea level (see Sections 5.6.1, 5.8.1 and Chapter 13) and carbon cycle feedbacks such as those linked with permafrost melting (see Chapter 6)... The magnitude of polar amplification depends on the relative strength and duration of different climate feedbacks, which determine the transient and equilibrium response to external forcings.

Andrew Lacis wrote: (3) Water vapor and clouds account for about 75 % the strength of the terrestrial greenhouse effect, but are feedback effects that require sustained radiative forcing to maintain their atmospheric distribution.

(3) Water vapor and clouds account for about 75 % the strength of the terrestrial greenhouse effect, but are feedback effects that require sustained radiative forcing to maintain their atmospheric distribution.

The main reasons are that (i) other forcing and feedback factors may co-vary in a statistically dependent way with CO2 and can not be separated, (ii) the operation of some climate feedbacks depends on the time scale considered, and (iii) the strength of climate feedbacks depends on the mean climate.

Now the sun's strength is currently about 340 watts / m2, so this means the unknown feedback is capable of offsetting a forcing of 30 % times 340 watts / m2, or about 100 watts / m2.

It is a measure of the strengths of the climate feedbacks at a particular time and may vary with forcing history and climate state.

Incorporating new findings on the radiative forcing of black carbon (BC) aerosols, the magnitude of the climate sensitivity, and the strength of the climate / carbon cycle feedbacks into a simple upwelling diffusion / energy balance model similar to the one that was used in the TAR, we find that the range of projected warming for the 1990 - 2100 period is reduced to 1.1 - 2.8 °C.

Things like assumptions about linearity (which means more or less, they make the mistake of assuming that all forcings and feedbacks operate at similar ratios and strengths when the planet is an iceball as they do when Earth hits a rare warm phase).