According to research by the dating represented when you look at the Figure cuatro, the fresh calculate the quantity of damaging ton will likely be projected

According to research by the dating represented when you look at the Figure cuatro, the fresh calculate the quantity of damaging ton will likely be projected

The new instances in the list above show that the fresh new estimate of dangers in exposure to glacier flooding can not be made on such basis as one to factor by yourself (e.g. the outside part of a good glacial river (Post and you may Mayo 1971)). Instead, the combination out of discharge volumes, rupture systems, peak-discharge thinking, lithology and you can preference in the arrived at of one’s glacier load features getting analyzed. Outbursts of specialist-glacial ponds having moraine dams which includes stagnant frost are, regardless, hazardous and you can warrant precautionary action, because they usually enable it to be big rain occurrences. Hence the discharge may be superimposed on to flood considering precipitation. Peak-release thinking having outbursts because of modern enlargement off frost channels are computed making use of the completely empirical Clague-Mathews formula:

For years and years, of a lot slope towns was basically dependent in which they truly are impacted of the for example events and that, toward one-hand, are very unusual, and on additional, may enjoys big outcomes down the road

where V is the outburst frequency when you look at the cubic yards (Clague and you may Matthews 1973). Thinking calculated in this way is actually quite higher than the highest observed top discharge opinions (Table II).

The formula is, therefore, admirably suitable for estimates in such cases. However, much higher peak-discharge values are expected in the event of sudden ruptures of ice barriers (Table III). For such events, with the exclusion of the minimal outburst at Glacier Bas d’Arolla, the following formula has to be applied: Q max (sudden break (m 3 s ?1 )) = V/tw

where V is again the outburst volume in cubic metres and tw is an empirical time constant [about 1 000 to 2 000 s, cf. Table III). In Figure 4, the average slope between the place of rupture and the outermost limit of the recorded area of damage, as a measure of the potential area of damage in the valley, is plotted as a function of the expected value of the peak-discharge. Since the spatial extent of populated areas in the Swiss Alps has not changed significantly over the centuries under consideration, the historical records of events causing damage can be used as a first approximation to appropriate standards. On the other hand, the extent of the damage in comparable cases today and in the future may well be considerably greater because of the expansion of cultivated land in the interim. The most extensive damage occurs when there is relatively small debris content. Peak-discharge values below 20 m 3 s ?1 are dangerous only for slopes over 10 to 12° and when there is, in addition, readily eroded loose material. The relationship given in Figure 4 also takes into account a few (known to the author), well-documented, non-Swiss glacier floods in the Alps, especially the catastrophe on Glacier de la Tete Rousse 1892, French Alps (sudden waterpocket rupture, many people killed in St Gervais (Mougin and Bernard 1922)), and at Vernagtferner, Austrian Alps (repeated sudden dumping of the Rofen lake, dammed-up during and after the surges of Vernagtferner, damages right into the Inntal: Reference Lanser Lanser 1959, Reference Hoinkes Hoinkes 1969). These are, however, extreme events historically. Many glacier floods take place and terminate well within the indicated extremes. These extremes have to be taken as standards, however, until the reasons are known why it is that, in some cases, the limits are not being reached.

Fig. 4. Extent regarding damage along side glacier stream to possess sufficiently noted glacier flooding from the Swiss Alps, ?crit = mediocre mountain amongst the host to rupture (often the glacier terminus) and the outermost maximum of your own recorded ruin naughty el salvador chat room. Occurrences is labelled given that “dirt flow” in the event that region from the pounds out of dust exceeds the new region from the lbs of h2o.


Problems in connection with glacier flooding continue to be to-be asked on the Swiss Alps down the road, but from the haven out-of glaciers plus the structure away from reservoirs having electricity manufacturing, it can generally become an issue of outbursts away from relatively short liquids people for the effortlessly eroded, shed sediments. To the estimation of such glacier hazards, which happen to be constantly local, one has to turn to sense off historical situations. Peak-release philosophy will be computed just as much as, making use of the Clague-Matthews algorithm, for as long as the new sudden crack out of an ice dam is actually not guessed; this might occur following surge out-of an excellent glacier, a frost avalanche or a temporary blockage of an effective subglacial release channel. If this sounds like the truth, then the release for every second is started to 1/1000 of your outburst regularity and you can a flooding wave of numerous yards tall get ensue. If hill is steep, actually quick outburst quantities and you may more compact height-release philosophy may result in the synthesis of hazardous debris circulates. In appropriate procedure (20 so you’re able to 30° high moraine slopes, scree hills or rock-glacier fronts), erosional streams which have a combination-sectional part of doing five hundred meters dos could form. The biggest, erratic top-discharge opinions off glacierized parts are observed to the drinking water-wallet ruptures, due to progressive enhancement from intra- and subglacial channels to the big rain, as well as have away from abrupt h2o-pouch ruptures immediately after short-term blockage from release channels. Such as for example thinking was of purchase out of one hundred to 150 meters step 3 s _1 .


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