RELATIVITY…
One principal
subject of physics is relativity, the field of study that measures events
(things that happen): where and when they happen, and by how much any two
events are separated in space and time. In addition, relativity has to do with
transforming such measurement reference frame that move relative to each other.
Transformation
and moving reference frame were well understood and quite routine to physicists
in 1905. Then albert Einstein published his special theory of relativity. The
adjective special mean that the theory deals only with inertial reference
frames, which are frames in which Newtons laws are valid.
(Einstein general theory of relativity treats that more challenging situation in which reference
frames can undergo gravitational acceleration; the term relativity implies only
inertial reference frames.)
EINSTEIN
DEMONSTRATION…
In particular, Einstein demonstrated that space and time
are entangled; that is, the time between two events depends on how far apart
they occurs and vice versa. Also the entanglement is different for observer who
move relative to each other. One result is that time does not pass at a fixed
rate, as if it were ticked off with mechanical regularity on some master grandfather
clock that controls the universe. Rather, that rate is adjustable: Relative
motion can change the rate at which time passes. Prior to 1905, no one but a
few daydreamer would have thought that. Now, engineers and scientists take it
for granted because their experience with special relativity has reshaped their
common sense.
SPECIAL relativity has the reputation of being difficult.
It is not difficult mathematically, at least not here. However, it is difficult
in that we must be very careful about who measures what about an event and just
how that measurement is made and it can be difficult because it can contradict
routine experience.
Fundamental Of Physics.
By Nicholas Barber , BBC News
The new film Jason Bourne reunites Matt Damon and director Paul Greengrass after nearly a decade – but can they recreate the old magic? Nicholas Barber finds out.
Jason Bourne.
Photo Credit : www.jasonbournemovie.com
Break out the ‘Bourne again’ headlines: nearly a decade on from The Bourne Ultimatum, Matt Damon and writer-director Paul Greengrass have reunited for Jason Bourne, another propulsive yarn about the CIA’s memory-impaired rogue super-spy. The character was born in a Robert Ludlum novel, and his big-screen debut, The Bourne Identity, was directed by Doug Liman, but the series is now associated so closely with Damon and Greengrass that if someone else makes a Bourne film - eg, The Bourne Legacy, with Jeremy Renner - it feels like a karaoke version of a classic song. Jason Bourne, on the other hand, is the sound of the band getting back together.
Since we last saw him, Bourne has been living off the grid as a bare-knuckle boxer. It’s disappointing that he hasn’t made more productive use of his phenomenal skills, but the idea is that he was traumatised by his time as a brainwashed black-ops killer. The fact that the viewer gets to see an alarmingly muscular Damon with his top off is, I’m sure, an unintended bonus.
At any rate, Bourne’s anonymous existence is interrupted when his old CIA buddy Nicky Parsons (Julia Stiles) tracks him down to share some new information about his murky past. Bourne is intrigued enough to investigate further, but his enquiries upset the CIA’s director (Tommy Lee Jones, providing the air of elder-statesman gravitas and deviousness that Brian Cox, Chris Cooper, David Strathairn and Albert Finney brought to prior instalments). He believes that Bourne should be dispatched by an assassin known only as The Asset (Vincent Cassel, who is an asset indeed), whereas his shrewd lieutenant (Alicia Vikander) argues that Bourne can be persuaded to rejoin the Agency.
No one else can construct a fight sequence that is so head-spinningly fast, but which is also possible to follow
It’s just like old times. Once again, Bourne hurtles from one grey and gritty European metropolis to another at breathtaking speed. Once again, he is never more than half-a-step ahead of his enemies. And once again, Greengrass stages the action with bone-jarring immediacy, using wobbly handheld cameras and rat-a-tat editing to make the viewer feel as if they could be hit by a stray fist or bullet at any moment. Greengrass’s hectic, immersive style has been much imitated since The Bourne Supremacy rewrote the rules of the secret-agent genre in 2004, but no one else has his ability to construct a fight sequence that is so head-spinningly fast and fragmentary, but which is also possible to follow.
Just to show the copycats how it’s done, he puts the film’s first extended set piece in the middle of an anti-government demonstration in Athens - and the confidence with which he orchestrates the chaos is astounding. Once you’ve seen Bourne barrelling through crowds of protesters and riot police in a city choked by smoke and tear gas, you’ll never be able to rewatch 007’s daft car chase in Spectre, through a conveniently deserted Rome, without smirking.
Bourne, Jason Bourne
But even when Jason Bourne has you on the edge of your seat, it’s still hard to shake the feeling that it isn’t as satisfying as the earlier films. Partly, it’s a simple matter of the law of diminishing returns. Greengrass and Damon (and, to a lesser extent, Liman), have done a positively scientific job of refining the Bourne-movie formula. They know exactly which elements it has to have in order to distinguish it from every other espionage thriller on the market. The downside of this precision, though, is that they haven’t left themselves much room for manoeuvre.
It’s not as if they can let Bourne ski-jump off a cliff, or hop on a space shuttle, or acquire a taste for vodka Martinis and risque one-liners. They can’t let him do anything that he didn’t do in The Bourne Supremacy and The Bourne Ultimatum - and there’s no way he can it any more electrifyingly than he did in those. After two films which deserved to have “supreme” and “ultimate” in their titles - more or less - any follow-up will inevitably seem like a slightly less impressive retread of what we’ve seen before.
Perhaps the film should have been called “Chasin’ Bourne” instead
Sometimes, the repetition makes you roll your eyes. Isn’t it ridiculous, for instance, that the CIA is still hunting down Bourne, a task they first had a crack at in The Bourne Identity 14 years ago? Considering how much money, man-power and futuristic technology they have at their disposal in the film, you’d think they would have caught him by now - and yet here they are spending a fortune and mowing down countless innocent bystanders in the attempt. What a palaver. Wouldn’t it make more sense if they concentrated on catching terrorists instead?
But the problems with Jason Bourne aren’t all to do with familiarity breeding contempt. There are a few other off-key notes which suggest that, having reunited, the band isn’t quite playing in tune. For one thing, Greengrass resorts to more spy-movie hokum than he used to: more jargon, more absurdly quick computer uploads, more scenes in which someone looks at a photo on a screen, and barks, “enhance!” and the blurry picture magically comes into pin-sharp focus.
For another thing, it seems as if Greengrass is trying to make two films at once. One of them is about Bourne and his identity, just as the previous ones were. But the other is about a high-tech cyber-conspiracy which has nothing to do with him. It’s strange that Jason Bourne should have that full name as its title, because Bourne himself is almost a supporting character, with less screen time, less depth, and less dialogue than ever. Perhaps the film should have been called “Chasin’ Bourne” instead.
The non-Bourne plot concerns the CIA’s shady dealings with a Silicon Valley entrepreneur (Riz Ahmed) whose social networking service is more popular than Facebook, Instagram and Twitter put together. Inspired by Wikileaks and Edward Snowden, it’s a storyline that’s turned up in too many films already. After all, the villain’s scheme involves “full-spectrum surveillance - watching everyone, all the time.” But wasn’t that what Blofeld had planned in Spectre? You know something’s wrong with a Bourne film when it lags a year behind Bond.
The potential future effects of global climate change include more frequent wildfires, longer periods of drought in some regions and an increase in the number, duration and intensity of tropical storms. Credit: Left - Mellimage/Shutterstock.com, center - Montree Hanlue/Shutterstock.com.
Global climate change has already had observable effects on the environment. Glaciers have shrunk, ice on rivers and lakes is breaking up earlier, plant and animal ranges have shifted and trees are flowering sooner.
Effects that scientists had predicted in the past would result from global climate change are now occurring: loss of sea ice, accelerated sea level rise and longer, more intense heat waves.
Taken as a whole, the range of published evidence indicates that the net damage costs of climate change are likely to be significant and to increase over time.
- Intergovernmental Panel on Climate Change
Scientists have high confidence that global temperatures will continue to rise for decades to come, largely due to greenhouse gases produced by human activities. The Intergovernmental Panel on Climate Change (IPCC), which includes more than 1,300 scientists from the United States and other countries, forecasts a temperature rise of 2.5 to 10 degrees Fahrenheit over the next century.
According to the IPCC, the extent of climate change effects on individual regions will vary over time and with the ability of different societal and environmental systems to mitigate or adapt to change.
The IPCC predicts that increases in global mean temperature of less than 1.8 to 5.4 degrees Fahrenheit (1 to 3 degrees Celsius) above 1990 levels will produce beneficial impacts in some regions and harmful ones in others. Net annual costs will increase over time as global temperatures increase.
"Taken as a whole," the IPCC states, "the range of published evidence indicates that the net damage costs of climate change are likely to be significant and to increase over time." 1
Future effects
Some of the long-term effects of global climate change in the United States are as follows, according to the Third National Climate Assessment Report:
Change will continue through this century and beyond
Global climate is projected to continue to change over this century and beyond.
Global climate is projected to continue to change over this century and beyond. The magnitude of climate change beyond the next few decades depends primarily on the amount of heat-trapping gases emitted globally, and how sensitive the Earth’s climate is to those emissions.
Temperatures will continue to rise
Because human-induced warming is superimposed on a naturally varying climate, the temperature rise has not been, and will not be, uniform or smooth across the country or over time.
Because human-induced warming is superimposed on a naturally varying climate, the temperature rise has not been, and will not be, uniform or smooth across the country or over time.
Frost-free season (and growing season) will lengthen
The length of the frost-free season (and the corresponding growing season) has been increasing nationally since the 1980s, with the largest increases occurring in the western United States, affecting ecosystems and agriculture
The length of the frost-free season (and the corresponding growing season) has been increasing nationally since the 1980s, with the largest increases occurring in the western United States, affecting ecosystems and agriculture. Across the United States, the growing season is projected to continue to lengthen.
In a future in which heat-trapping gas emissions continue to grow, increases of a month or more in the lengths of the frost-free and growing seasons are projected across most of the U.S. by the end of the century, with slightly smaller increases in the northern Great Plains. The largest increases in the frost-free season (more than eight weeks) are projected for the western U.S., particularly in high elevation and coastal areas. The increases will be considerably smaller if heat-trapping gas emissions are reduced.
Changes in precipitation patterns
Average U.S. precipitation has increased since 1900, but some areas have had increases greater than the national average, and some areas have had decreases
Average U.S. precipitation has increased since 1900, but some areas have had increases greater than the national average, and some areas have had decreases. More winter and spring precipitation is projected for the northern United States, and less for the Southwest, over this century.
Projections of future climate over the U.S. suggest that the recent trend towards increased heavy precipitation events will continue. This trend is projected to occur even in regions where total precipitation is expected to decrease, such as the Southwest.
More droughts and heat waves
Droughts in the Southwest and heat waves (periods of abnormally hot weather lasting days to weeks) everywhere are projected to become more intense, and cold waves less intense everywhere.
Droughts in the Southwest and heat waves (periods of abnormally hot weather lasting days to weeks) everywhere are projected to become more intense, and cold waves less intense everywhere.
Summer temperatures are projected to continue rising, and a reduction of soil moisture, which exacerbates heat waves, is projected for much of the western and central U.S. in summer. By the end of this century, what have been once-in-20-year extreme heat days (one-day events) are projected to occur every two or three years over most of the nation.
Hurricanes will become stronger and more intense
The intensity, frequency and duration of North Atlantic hurricanes, as well as the frequency of the strongest (Category 4 and 5) hurricanes, have all increased since the early 1980s
The intensity, frequency and duration of North Atlantic hurricanes, as well as the frequency of the strongest (Category 4 and 5) hurricanes, have all increased since the early 1980s. The relative contributions of human and natural causes to these increases are still uncertain. Hurricane-associated storm intensity and rainfall rates are projected to increase as the climate continues to warm.
Sea level will rise 1-4 feet by 2100
Global sea level has risen by about 8 inches since reliable record keeping began in 1880. It is projected to rise another 1 to 4 feet by 2100
Global sea level has risen by about 8 inches since reliable record keeping began in 1880. It is projected to rise another 1 to 4 feet by 2100. This is the result of added water from melting land ice and the expansion of seawater as it warms.
In the next several decades, storm surges and high tides could combine with sea level rise and land subsidence to further increase flooding in many of these regions. Sea level rise will not stop in 2100 because the oceans take a very long time to respond to warmer conditions at the Earth’s surface. Ocean waters will therefore continue to warm and sea level will continue to rise for many centuries at rates equal to or higher than that of the current century.
Arctic likely to become ice-free
The Arctic Ocean is expected to become essentially ice free in summer before mid-century.
The Arctic Ocean is expected to become essentially ice free in summer before mid-century.
U.S. regional effects
Below are some of the impacts that are currently visible throughout the U.S. and will continue to affect these regions, according to the Third National Climate Assessment Report2, released by the U.S. Global Change Research Program:
Northeast. Heat waves, heavy downpours and sea level rise pose growing challenges to many aspects of life in the Northeast. Infrastructure, agriculture, fisheries and ecosystems will be increasingly compromised. Many states and cities are beginning to incorporate climate change into their planning.
Northwest. Changes in the timing of streamflow reduce water supplies for competing demands. Sea level rise, erosion, inundation, risks to infrastructure and increasing ocean acidity pose major threats. Increasing wildfire, insect outbreaks and tree diseases are causing widespread tree die-off.
Southeast. Sea level rise poses widespread and continuing threats to the region’s economy and environment. Extreme heat will affect health, energy, agriculture and more. Decreased water availability will have economic and environmental impacts.
Midwest. Extreme heat, heavy downpours and flooding will affect infrastructure, health, agriculture, forestry, transportation, air and water quality, and more. Climate change will also exacerbate a range of risks to the Great Lakes.
Southwest. Increased heat, drought and insect outbreaks, all linked to climate change, have increased wildfires. Declining water supplies, reduced agricultural yields, health impacts in cities due to heat, and flooding and erosion in coastal areas are additional concerns.
IPCC 2007, Summary for Policymakers, in Climate Change 2007: Impacts, Adaptation and Vulnerability. Contribution of Working Group II to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, Cambridge University Press, Cambridge, UK, p. 17.
USGCRP 2014, Third Climate Assessment.
Source : climate.nasa.gov
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