A method for early warning of overflow water level of glacial lake outburst and its application
A water level and overflow technology, which is applied in the fields of alarms, climate change adaptation, climate sustainability, etc., can solve the problems of low early warning accuracy, failure to consider whether the ice avalanche can reach the ice lake, poor applicability, etc., and achieve early warning. The effect of high accuracy, improved early warning accuracy, and enhanced applicability
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Embodiment 1
[0025] A method for early warning of overflow water level of a glacier lake burst, comprising the following steps:
[0026] a. Investigate and measure the thickness T of the top of the ice track dam, the width of the breach b, and the average width of the ice lake w 0 , the length-to-width ratio c of the glacial lake, the average slope β of the bank slope of the glacial lake before the outburst, and the characteristic particle size of the starting sediment d;
[0027] b. Analyze the critical water level conditions of the sediment at the overflow outlet of the ice-mark embankment when the water level rises, and obtain the critical overflow water depth H of the glacier lake outburst;
[0028]
[0029] Among them, H is the critical overflow water depth of glacial lake burst, in m; d is the characteristic particle size of starting sediment, in m; T is the thickness of ice track embankment crest, in m; b is the burst width, in m; w 0 is the average width of the glacial lake, in...
Embodiment 2
[0033] A method for early warning of overflow water level of a glacier lake burst, comprising the following steps:
[0034] a. Investigate and measure the thickness T of the top of the ice track dam, the width of the breach b, and the average width of the ice lake w 0 , the length-to-width ratio c of the glacial lake, the average slope β of the bank slope of the glacial lake before the outburst, and the characteristic particle size of the starting sediment d;
[0035] b. Analyze the critical water level conditions of the sediment at the overflow outlet of the ice-mark embankment when the water level rises, and obtain the critical overflow water depth H of the glacier lake outburst;
[0036]
[0037] Among them, H is the critical overflow water depth of glacial lake burst, in m; d is the characteristic particle size of starting sediment, in m; T is the thickness of ice track embankment crest, in m; b is the burst width, in m; w 0 is the average width of the glacial lake, in...
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