Sentences with phrase «intensity scale changes»

Intensity Scale Changes with Viewing Angle: There is essentially no change in the Intensity Scale for the LG OLED TV with Viewing Angle but a very large change for the Samsung LCD TV, which is shown in this Figure.

Not exact matches

These particular freshwater Microcystis blooms (and toxins) are increasing in estuaries and coastal waters around the world and are expected to expand in scale and intensity with global climate change.

The records document that the Laschamp Excursion was characterized locally by (1) declination changes of ± 120 °, (2) inclination changes of more than 140 °, (3) ~ 1200 - year oscillations in both inclination and declination, (4) near 90 ° out - of - phase relationships between inclinations and declinations that produced two clockwise loops in directions and virtual geomagnetic poles (VGPs) followed by a counterclockwise loop, (5) excursional VGPs during both intervals of clockwise looping, (6) magnetic field intensities less than 10 % of normal that persisted for almost 2000 years, (7) marked similarity in excursional directions over ~ 5000 km spatial scale length, and (8) secular variation rates comparable to historic field behavior but persisting in sign for hundreds of years.

This is addressed by evaluating change in global or large - scale patterns in the frequency or intensity of extremes (e.g., observed widespread intensification of precipitation extremes attributed to human influence, increase in frequency and intensity of hot extremes) and by event attribution methods.

It's also easy to scale this one to your abilities — it will still burn, but you can add or subtract weight to change up the intensity.

The key will be in enlarging the native Color Gamut and then dynamically changing the display's color management and intensity scales with the measured Ambient Light level in order to automatically compensate for reflected glare and image wash out from Ambient Light as discussed in our 2014 Innovative Displays and Display Technology and SID Display Technology Shoot - Out articles.

There is essentially no change in the Intensity Scale for the LG OLED TV with Viewing Angle but a very large change for the Samsung LCD TV, which is shown in this Figure.

For all other LCD technologies like VA there is a large change in the Intensity Scale with Viewing Angle

Even at a 45 degree Viewing Angle the LG OLED TV shows relatively small changes in both Color and Brightness, and no changes in the Black Level, Contrast Ratio, and Intensity Scale.

The Intensity Scale on the iPhone 5 should be changed to match the excellent calibration of the new iPad.

The biggest improvements for mobile displays will come from dynamically changing the display Color Gamuts and Intensity Scales to automatically compensate and correct for reflected glare and image wash out from ambient light.

The key will be in dynamically changing the display's color management and intensity scales with the measured Ambient Light in order to automatically compensate for reflected glare and image wash out from ambient light as discussed in our 2014 Innovative Displays and Display Technology and SID Display Technology Shoot - Out articles.

The galleries respond to the evolving character of Still's art, changing scale and proportion, while varying the intensity of light.

Most of these variations are given changes in scale and tonal intensity from painting to painting within a series.

Refraction, specifically the real component of refraction n (describes bending of rays, wavelength changes relative to a vacuum, affects blackbody fluxes and intensities — as opposed to the imaginary component, which is related to absorption and emission) is relatively unimportant to shaping radiant fluxes through the atmosphere on Earth (except on the small scale processes where it (along with difraction, reflection) gives rise to scattering, particularly of solar radiation — in that case, the effect on the larger scale can be described by scattering properties, the emergent behavior).

Another complication in looking at long - term tornado intensity trends is the fact that the «damage indicators» used to rate tornadoes have recently changed with the adoption of the EF scale, making it dubious to compare tornadoes of the past with those of the present.

``... it is now very likely that anthropogenic forcing has contributed to the observed changes in the frequency and intensity of daily temperature extremes on the global scale since the mid-20th century.

For the entire Northern Hemisphere, there is evidence of an increase in both storm frequency and intensity during the cold season since 1950,1 with storm tracks having shifted slightly towards the poles.2, 3 Extremely heavy snowstorms increased in number during the last century in northern and eastern parts of the United States, but have been less frequent since 2000.11,15 Total seasonal snowfall has generally decreased in southern and some western areas, 16 increased in the northern Great Plains and Great Lakes region, 16,17 and not changed in other areas, such as the Sierra Nevada, although snow is melting earlier in the year and more precipitation is falling as rain versus snow.18 Very snowy winters have generally been decreasing in frequency in most regions over the last 10 to 20 years, although the Northeast has been seeing a normal number of such winters.19 Heavier - than - normal snowfalls recently observed in the Midwest and Northeast U.S. in some years, with little snow in other years, are consistent with indications of increased blocking (a large scale pressure pattern with little or no movement) of the wintertime circulation of the Northern Hemisphere.5 However, conclusions about trends in blocking have been found to depend on the method of analysis, 6 so the assessment and attribution of trends in blocking remains an active research area.

Their work encompasses a range of problems and time scales: from five - day model predictions of hurricane track and intensity, to understanding the causes of changes in extremes over the past century, to building new climate prediction models for seamless predictions out to the next several years, to earth system model projections of human - caused changes in various extremes (heat waves, hurricanes, droughts, etc.) over the coming century.

The research contributes to building an improved understanding of 1) how different intensities of disaster affect children in different contexts and 2) the structures needed to realise the benefits of engaging children as active citizens and agents of change at the sub-national and local scale.

However, on climate time scales there has not been detection (much less attribution) of increasing disasters (intensity or frequency) to human - caused climate change

The table that accompanies the above passage from the IPCC's report, captioned «Extreme weather and climate events: global - scale assessment of recent observed changes, human contribution to the changes, and projected further changes for the early (2016 — 2035) and late (2081 — 2100) 21 st century `'» has the following entries for «Increases in intensity and / or duration of drought»: under changes observed since 1950, «low confidence on a global scale, likely changes in some regions `'» [emphasis added]; and under projected changes for the late 21 st century, «likely (medium confidence) on a regional to global scale».

Lin expects that a lot of consensus building will be needed for the storm intensity scale to change.

Further, «confidence in large - scale changes in the intensity of extreme extratropical cyclones [such as «Superstorm» Sandy] since 1900 is low.»

Rather, the regime shifts in the HCS are related to 3D habitat changes driven by changes in upwelling intensity from both regional and large ‐ scale forcing.

«Over the time - scale of millions of years, the change in solar intensity is a critical factor influencing climate (e.g., ice ages).

The cosmogenic radionuclide records have been low - pass filtered by a rectangular function in the frequency domain with different cut - off frequencies in order to minimise the solar influence and to investigate the time scales on which we see common changes in the radionuclide production rates and the geomagnetic field intensity reconstructions.

Also, in another complication in assessing long - term tornado intensity trends, the «damage indicators» used to rate tornadoes recently have changed with the adoption of the EF scale, making it dubious to compare tornadoes of the past with those of the present.

In summary, confidence in large scale changes in the intensity of extreme extratropical cyclones since 1900 is low.

«There is no compelling evidence to indicate that the characteristics of tropical and extratropical storms have changed... Owing to incomplete data and limited and conflicting analyses, it is uncertain as to whether there have been any long - term and large - scale increases in the intensity and frequency of extra-tropical cyclones in the Northern Hemisphere.

The records document that the Laschamp Excursion was characterized locally by (1) declination changes of ± 120 °, (2) inclination changes of more than 140 °, (3) ~ 1200 - year oscillations in both inclination and declination, (4) near 90 ° out - of - phase relationships between inclinations and declinations that produced two clockwise loops in directions and virtual geomagnetic poles (VGPs) followed by a counterclockwise loop, (5) excursional VGPs during both intervals of clockwise looping, (6) magnetic field intensities less than 10 % of normal that persisted for almost 2000 years, (7) marked similarity in excursional directions over ~ 5000 km spatial scale length, and (8) secular variation rates comparable to historic field behavior but persisting in sign for hundreds of years.

Differences between conditions at follow - up displayed precisely the same pattern of results noted here, with the following exceptions: (1) change in ECBI Intensity Scale score from baseline to the 6 - month follow - up was statistically significant between WL and PTG, but the ECBI Problem Scale score was not, and (2) change in the DPICS - CII child disruptive behavior at posttreament was significant in the NR - PTG condition.

At 12 months significant change (p < 0.05) in a positive direction was observed for intervention group children on the intensity scale of the ECBI, and the total, conduct, and hyperactivity scales of the SDQ.

Grouped t tests were used to compare the mean change in scores in the control and intervention groups where the differences were normally distributed (ECBI intensity score, SDQ total score, PSI parent child interaction, and parent domains), and Mann - Whitney U tests for the mean change in scores in the two groups where the differences were not normally distributed (ECBI problem score, SDQ conduct, hyperactivity, emotional, peer and prosocial scales, GHQ somatic anxiety, social, depression and total scores, PSI difficult child domain and total score, and SES).

Figures 2 — 4 show the plotted change over time in mean scores for the outcome measures that showed a significantly greater change in the intervention than control group at either 6 or 12 months: ECBI intensity scale, SDQ conduct subscale, and GHQ depression scale.

This pattern was present for internalizing disorders as a predictor of change on the Eyberg intensity scale, difficult child temperament as a predictor of change on the Eyberg intensity scale, and the CGAS as a predictor of change on the CBCL externalizing scale.

This may have discouraged participants from adjusting the scale upwards or downwards until pronounced changes in emotional intensity were detected.

Items are rated on a 4 - point scale ranging from 0 to 3 in terms of intensity of symptoms (e.g., change in appetite) and attitudes (e.g., pessimism) during the past 2 weeks.