Sentences with phrase «stratospheric heights of»

Ranging from stratospheric heights of $ 20000, the price of bitcoin fell to below $ 15000 figures creating much concern amongst crypto aficionados who were rooting for the digital token to reach record heights.
Guess what the Cupertino based company is charged with — trademark infringement over the term iPad, which in turn is the biggest product that has propelled Apple to stratospheric heights of success in recent times.
Still the good doctor couldn't quite reach the stratospheric heights of «Iron Man» ($ 98.6 million), «Captain America: Civil War» ($ 179.1 million), or «Marvel's The Avengers» ($ 207.4 million).

Not exact matches

In the late 1980s, on the heels of a three - decade long «Economic Miracle,» Japan experienced its infamous «bubble economy» in which stock and real estate prices soared to stratospheric heights driven by a speculative mania.
The Dubliner's inexorable rise reached stratospheric heights in the cross-over clash which is expected to earn him in the region of # 77m — and that's before endorsement deals are considered.
«We were very much surprised to find polar stratospheric clouds down to heights of about 14 km,» Björn - Martin Sinnhuber says.
«For a period of several weeks, wide areas of the Arctic were covered by polar stratospheric clouds between about 14 and 26 kilometers height.
Recent studies have shown a doubling of stratospheric water vapour, likely from increasing atmospheric heights due to global warming, overshooting thunderstorm tops from stronger tropical cyclones and mesoscale convective systems etc...
As VW itself has helped pushed the hot hatch genre up to its stratospheric heights with the Clubsport Edition 40 and Clubsport S, it seems an inconceivable oversight not to have instilled some of the character from those (now defunct) models into this updated GTI Performance.
Adding CO2 does not (at least not before the climate response, which is generally stratospheric cooling and surface and tropospheric warming for increasing greenhouse gases) decrease the radiation to space in the central portion of the band because at those wavelengths, CO2 is so opaque that much or most radiation to space is coming from the stratosphere, and adding CO2 increases the heights from which radiation is able to reach space, and the stratospheric temperatures generally increase with increasing height.
Basically, what happens, I would argue, is that increased opacity raises the height of the «stratospheric» radiating layer.
In some rough order of certainty we can consider that the 11 year solar cycle impacts on the following are well accepted: stratospheric ozone, cosmogenic isotope production, upper atmospheric geopotential heights, stratospheric temperatures and (slightly less certain and with small magnitudes ~ 0.1 deg C) tropospheric and ocean temperatures.
The main points of that solution are to show that (1) for making temperature increase with height, it's not enough to have a stratospheric absorber; you need one with the right vertical profile, and (2) you can get stratospheric cooling in response to increased IR opacity because you get rid of more of the absorbed solar locally.
Showing how a change in CO2 amount causes different LW flux changes at different heights would show how stratospheric cooling occurs, and the spectra (overlayed for 0.5 x, 1 x, 2 x, 4 x, 8 x preindustrial CO2) would also show the origin of the logarithic proportionality for tropopause - level forcing once the center of the band is saturated.
It's not legal because of height and the fact that, even on wood buildings, the cladding has to be noncombustible; nobody in the world has done modular CLT on this scale; the cantilevers look impossible; and the monthly condo maintenance fees will be stratospheric with a wooden cladding.
«Climate models show cooler stratospheric temperatures happen when there is more water vapor present» «The stratosphere is the typically dry layer of the atmosphere above the troposphere, where temperatures increase with height
Recent changes in the location of maximum spring stratospheric ozone depletion (Evtushevsky et al. 2008) may also be contributing to the negative geopotential height trends in the South Pacific sector and to the east — west asymmetry of Antarctic climate change.
The volumes of sulphate aerosols that would need to be flown to stratospheric heights and released each year would continue to grow as humans went on burning ever more fossil fuels.
There is a choice of vertical resolutions between 38 levels extending to ~ 40 km height (of which 29 are below 18 km), 63 levels extending to ~ 40 km height (of which 50 are below 18 km), and 85 levels extending to 85 km in height (of which 50 are below 18 km), the latter allowing improved representation of stratospheric processes.
But to quantify the influences (or «forcings» in climate jargon) even further, they considered three anthropogenic forcings — well - mixed greenhouse gases, sulfate aerosols, and tropospheric and stratospheric ozone — as well as two natural forcings — changes in solar irradiance and volcanic aerosols — all of which are likely to influence tropopause height
The Acer Spin 7 follows the recent trend of scaling back display resolution from stratospheric QHD heights and limiting it to Full HD (1,920 x 1,080) resolution.
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