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Exam Title : Riverbed Certified Solutions Associate - Network Performance Management
Exam ID : 201-01
Exam Duration : 90 mins
Questions in test : 50
Passing Score : 60%
Official Training : NPM200 Performance Monitoring Essentials
APM200 Application Performance Monitoring Essentials
Exam Center : Pearson VUE
Real Questions : Riverbed RCSA-NPM Real Questions
VCE Practice Test : Riverbed 201-01 Certification VCE Practice Test

Subject Area
Approximate Number of Questions from this area
AppResponse 13
NetProfiler 21
Packet Analyzer 9
Transaction Analyzer 1
NetShark 1
Portal 5

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When the levees destroy | 201-01 real questions and Real test Questions

Researchers are studying the place, when, and why rivers jump from their channels in deadly avulsions.

After a 2008 avulsion on the Kosi River, floodwaters overran the Indian state of Bihar, displacing hundreds of thousands of people.


Rumors that the Kosi River changed into about to burst have been spreading quickly in Kusaha, a Nepalese village on the border with India. The river's levees, towering over the village, were being eroded without delay by means of the cresting waters. At 2 p.m. on 18 August 2008, the east financial institution ruptured. people ran for his or her lives as the breach grew. quickly, the total river, some of the largest tributaries of the Ganges River, had overrun Kusaha and become spilling into India, drowning farm after farm in search of a sooner direction to the ocean.

eventually, the rampaging river discovered an extended-deserted channel, the place it flowed for 4 months earlier than engineers wrenched it lower back to its historical route. within the conclusion, the flood destroyed some 800 farming villages, killed greater than four hundred people, and displaced an additional 3 million. At one aspect, half of the Indian state of Bihar became underwater.

at the time, executive officers and scientists blamed the deluge on heavy monsoon rains and poor protection of the levees. each performed a job, but this adventure changed into brought on by something else, says Rajiv Sinha, a river morphologist at the Indian Institute of technology, Kanpur, who has studied it in detail.

The Kosi is without doubt one of the siltiest rivers on earth, carrying an annual load of some one hundred million lots of sediment eroded from its catchment within the Himalayas. near Kusaha the river hits the flat undeniable on the foot of the mountains, where it slows, dropping a whole lot of its load within the riverbed. as the channel's carrying potential diminishes over time, the river ultimately seeks a brand new route. for hundreds of years, the Kosi has burst its banks during this location each few decades—a phenomenon accepted to geographers as an avulsion.

Avulsions are often known as the “earthquakes of rivers,” as a result of they are so unexpected and catastrophic. but over the past decade, research has published that they are additionally just a little predictable. laptop analyses and laboratory models of rivers and deltas have yielded insights into where major rivers are likely to avulse—and when. “Ten years ago, they failed to comprehend what became using avulsions,” says Vamsi Ganti, a geomorphologist on the institution of California, Santa Barbara (united states). “Now they can model the approaches and begin to determine scorching spots.”

Yet simply as researchers are gaining foresight into these rhythmic cataclysms, human exercise is undermining it. Upstream deforestation and development is including silt to rivers in unpredictable methods. Levees and dams are altering flows and paths, from time to time worsening the risk. After the Kosi flood, for example, Bihar begun to build even more flood insurance plan levees. however levees force a river to drop silt within a limited channel, hastening the subsequent avulsion, Sinha says. “If [engineers] don't take into account the underlying dynamics,” he says, “they're doomed to fail.”

local weather trade is one other wild card: Rising seas are shifting avulsion sizzling spots that turn up on coastal deltas, one more place where rivers decelerate, drop silt, and raise riverbeds, “people are now the huge instigators of avulsions on rivers,” says Jaia Syvitski, a hydrogeologist at the tuition of Colorado, Boulder.

FOR ALL THEIR destructiveness, avulsions bring merits to each nature and society. They unleash regular floods that nourish lots of the world's first rate wetlands. as an instance, the enormous Pantanal, in the coronary heart of South america, is saved rich and muddy by means of the avulsing Taquari River.

And by using smearing sparkling sediment throughout flood plains and deltas, avulsions fertilize lands that have nurtured probably the most planet's fantastic civilizations. The interlinked flood plains of the Tigris and Euphrates rivers in Iraq endure the imprints of 11 most important avulsions over the last 7000 years. historic Mesopotamians converted some deserted channels into irrigation canals; at other times the rivers themselves took over irrigation canals.

It isn't any shock that to this present day, avulsion zones are among the many most densely populated locations on the earth. River deltas, where avulsions are conventional, occupy simply 0.5% of the realm's land, however are domestic to four.5% of its inhabitants. those dense populations, drawn via the fertility that avulsions foster, are additionally in the route of their destructive drive. not for nothing are amazing avulsing rivers such because the Kosi or the Yellow River (Huang He) in China called their peoples' “joy and sorrow.”

Avulsions don't seem to be just infrequent catastrophes. An unpublished analysis of satellite tv for pc pictures with the aid of Sam Brooke of america has identified about a hundred abrupt river jumps during the past 50 years: about 40 on coastal deltas and 60 on inland alluvial enthusiasts where rivers exit mountain valleys. Many avulsions cluster on rainy, mountainous islands in the tropics that erode straight away, equivalent to Madagascar and Java—whatever Brooke says the evaluation, the first of its kind, drew attention to.

within the aftermath of the Kosi catastrophe, Douglas Jerolmack, a sedimentologist at the college of Pennsylvania, changed into one of a handful of researchers to look greater carefully at the dynamics of avulsions. frequently during the past, researchers had claimed avulsions were brought on with the aid of earthquakes or severe floods. but Jerolmack's experiments confirmed a growing suspicion that avulsions took place naturally—and predictably. “Rivers are perturbed all of the time however simplest avulse in the event that they are deploy by satisfactory deposition,” he says. typically, he says, this occurs as soon as the riverbed rises above the land outdoor its banks or levees, so the entire volume of the river is “perched,” as happened with the Kosi.

Jerolmack and his colleagues used a humble laboratory tool for mimicking river avulsions: a flow desk, in reality a large tank stuffed with sand and water. At one conclusion of the move table, the researchers could turn a “river” faucet on and off and change the concentrations of sediment in the circulate. by varying the steepness of the desk, they created miniature mountain streams disgorging into fan-formed flood plains and fowl's-foot deltas.

Geographers had already noticed that rivers are inclined to avulse at the foot of mountains, the place slopes trade dramatically and sediment settles out, silting up the bed. The miniature rivers of the circulate desk allowed the group to quantify how commonly the avulsions happened. “The time scale became actually the time it took the channel to fill with sediment,” Jerolmack says.

He and his colleagues also found that the river saved reoccupying a small variety of channels. “historical channel paths remained topographically clean, and so low-resistance pathways to the sea,” Jerolmack says. So if an avulsing river encounters an old channel, he says, it is likely to colonize it.

while Jerolmack changed into researching concerning the periodicity and quasi-predictability of avulsions inland, Michael Lamb, a geomorphologist at the California Institute of expertise, wanted to remember the mystery of recurrent avulsions downstream, in river deltas. In deltas, unlike at the foot of mountains, there is very nearly no slope alternate to gradual a river and cause sediment to construct up.

Lamb and his colleagues investigated via establishing now not a steep move table, but a languid laboratory delta, with a gradient of only 1 in a hundred,000 and a river spilling right into a three-meter-extensive “ocean.” In cycles of floods and delicate flows, they despatched water and sediment—low-density beaten walnut shells—into the basin. They once more found that the river spontaneously switched pathways to the ocean, and that the avulsions almost always happened at the head of the delta.

Why that was happening grew to become out to be extra complex than expected. Tides, by way of slowing the river in order that it unloads sediment as it enters the delta, are one ingredient. but in deltas, scouring from floods is very nearly as vital as deposition in growing avulsion situations. Floods are inclined to flush sediment faraway from the lower part of the delta, Lamb says, fighting avulsions from happening there. This leads to an avulsion-inclined spot one “backwater length” from the mouth of the delta—a distance that can also be calculated from fundamental river parameters.

The theory suggested that on the Mississippi River, an avulsion aspect should still fall some 500 kilometers upstream from its delta mouth. The precise world concurs: The Mississippi has avulsed in significant Louisiana about once every 1400 years, developing big delta lobes across the Gulf Coast. The researchers additionally found proof for repeated avulsions one backwater size up from the mouth of the Yellow, Rhine, Danube, Orinoco, and Nile rivers. “The found out tie between avulsion area and backwater hydrodynamics has been a online game changer,” Jerolmack says.

Some rivers are much less predictable, however. remaining yr, Lamb and colleagues published an investigation into a cluster of contemporary avulsions on short, steep, and sediment-rich streams in Madagascar. They found avulsions going on as an awful lot as 20 times farther upstream than envisioned through the backwater length by myself. They concluded that scouring from floods penetrates farther upstream on these streams as a result of they deposit strangely first-class sediments, which floods can sweep away more easily. “it be a special case, however still conforms to the conception that scour size is picking avulsion area,” Lamb says.

credit: (image) V. ALTOUNIAN/SCIENCE; (photos) NASA WORLDVIEW

although AVULSIONS will not ever be fully predictable, the day is nearing the place engineers can comprehend the place and when the risks are at their top-quality. Adrian Hartley, a rivers researcher on the tuition of Aberdeen, is happy with how some distance the container has come. “We are getting an awful lot nearer to figuring out avulsions.” however he warns that just as researchers start to draw close these natural river cycles, human influences are altering them. “Few river methods are without giant human have an impact on anymore, so basic usual fashions, besides the fact that children decent they are, won't do the entire job mandatory to predict avulsions.”

Some anthropogenic results are unsurprising. for instance, deforestation and soil erosion could make rivers siltier. That raises the tempo at which they refill their channels and reach the element of avulsion. but different components are much less obvious. Dams can lure sediment, combating its move downstream—and they also would seem to cut back the possibility of avulsions. but Ganti says dams selectively capture coarse sediment, whereas enabling finer silt to proceed downstream. ironically, the resulting rivers “can lift specifically high volumes of sediment,” Ganti says. these loads, eventually dropped, should enhance the frequency of avulsions, he predicts.

in the meantime, coastal deltas are facing rising seas. by eroding the shoreline and pushing tides farther upstream, they cause rivers to dump extra sediment farther inland, transferring the total backwater reach upstream, along with the avulsion scorching spot. Ganti says their frequency raises as smartly, since the invading tides ensure that much less of the sediment reaches. As tides push farther into deltas, they slow down rivers; less of the sediment receives into the ocean and more results in the delta the place it factors avulsions. “we are turning the knob the wrong way,” Ganti says. “We should brace ourselves for extra avulsions.”

If fashions are to keep up with such a quick-changing atmosphere, they need more and more desirable container statistics to exhibit when and where tipping aspects are drawing near, Lamb says. “accumulating data on the world's riverbeds is greater essential than ever.” but that tips is complicated to acquire remotely and painstaking to bring together in grownup or through boat, Lamb says. “for many of the realm's rivers, they lack any statistics set for river bottom elevations,” he says. “or not it's truly a massive hole in their knowing of the geography of the Earth.”

blind to what is going on underwater, many river engineers proceed to make bad instances worse by sticking with widely wide-spread methods of attempting to grasp returned floods. For them, ever better levees are the solution, whereas river scientists say they're the difficulty.

at the herbal avulsion aspect some 500 kilometers up from the mouth of the Mississippi delta, the U.S. army Corps of Engineers has for a century fought the river's urge to movement into the Atchafalaya River, which turned into the Mississippi's leading channel unless a couple of thousand years ago. In 1963, the Corps acted to steer clear of a full-scale avulsion. It accomplished a floodgate device, normal because the ancient River control constitution, that kept many of the river's stream—and sediment—mainly channel. “without this engineering, the Atchafalaya would have captured the majority of the flow from the Mississippi via now,” Ganti says.

but half a century on, the ancient River control structure's effectiveness is dwindling. It allows the Mississippi to ship 30% of its water into the Atchafalaya while holding onto most of its sediment. as a result, the riverbed just downstream of old River control has risen through about 1.5 meters, in response to Bo Wang, a fluvial geomorphologist now at Brown tuition. The sediment buildup raises the possibility that a future flood will again up, weigh down ancient River manage, and surge down the Atchafalaya. Such an avulsion could be catastrophic for trade on the Mississippi River, and could overrun many low-lying areas of the Atchafalaya. but Lamb says the frenzy of sediment would be an ecological boon for the delta areas of coastal Louisiana now sinking to the ocean. “Many can be nourished promptly if the river went down the Atchafalaya,” he says (Science, 23 April, p. 334).

To prevent avulsions, China has established discharging water from the Yellow River reservoirs to flush sediment from the riverbed downstream and send it to the ocean.

picture: XINHUA/LI AN/GETTY images

The stakes could be even better in northern China, where some ninety million people are living in a flood zone downstream of an avulsion hot spot on the Yellow River. but China is taking a more subtle strategy to mitigating the possibility, which it is aware of neatly from recent, tragic heritage.

On the right bank of the river, close to the city of Zhengzhou, is a modest stone plaque. It commemorates movements on the morning of 9 June 1938, when the great river burst its banks, flooded the nation's breadbasket, and located a brand new outlet to the sea, 650 kilometers south of the river's former mouth. think about the Mississippi heading east to enter the Atlantic Ocean in Georgia. The significant avulsion killed as much as 1 million individuals and made refugees of up to 10 million greater. It took engineers 9 years to coerce the river lower back to its former path.

This changed into no natural avulsion, youngsters. The river's banks have been dynamited on the orders of the nation's chief Chiang Kai-shek, to hang returned eastern invaders all over the 2nd Sino-jap battle. it is reckoned to be humanity's single most lethal act of war, besides the fact that children lots of the useless have been chinese language, and the eastern troops have been held up for less than a month.

some thing the militia folly, the engineers knew what they had been doing. They breached the financial institution at Huayuankou, a commonly used avulsion scorching spot where the river slackens as it emerges from the Loess Plateau and dumps its sediment. For the past 2500 years, the Yellow River has changed route right here roughly as soon as a century. If it were to occur again, “it will be a disaster of international importance, via affecting the chinese language financial system,” Syvitski warns.

these days, as the river rises as a whole lot as 10 meters above the encircling flood simple, China is trying out out new strategies in the vigil to avoid an avulsion. It has reduced sediment loads via soil conservation initiatives on the Loess Plateau. And it demonstrated the usage of quick flows of sediment-depleted water from dammed reservoirs to flush out sediment from the riverbed downstream and convey it to the ocean, says Jeff Nittrouer, a hydrologist whose crew at Rice school has been discovering China's efforts to tame the Yellow River.

In 1938, China brought on an avulsion on the Yellow River to repel eastern invaders—idea to be humanity's deadliest act of battle.


chinese engineers are also intervening on the 2d avulsion point downstream, at the head of the Yellow River delta, the place seven avulsions have took place between 1855 and 1930. considering that then, engineers have stopped attempting to avoid channel switches. in its place, they set off them with dynamite and digging. apart from making avulsions greater predictable, the idea is to circulate sediment deposition to components of the delta where the created land can be economically advantageous, reminiscent of for aquaculture or exploiting oil and fuel reserves, Nittrouer says.

the first fundamental diversion was in 1976. Then in 1996, workers blocked the 20-yr-ancient Qingshuigou channel as it crammed with sediment, and compelled the river down an historical natural channel to enter the ocean 20 kilometers from its former mouth. Nature took the lead once more in 2005, when the river cut a crevasse into its left bank, forming a brand new channel that has now taken over.

“The Yellow River delta is not any longer by any stretch a herbal delta,” Syvitski says. even so, the river's urge to shift its path to the ocean not ever abates. The expense of protection on its banks is eternal vigilance.

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