An early identification method of glacial lake outburst and its application
An early identification and glacier technology, applied in special data processing applications, design optimization/simulation, etc., can solve the problems of low early warning accuracy, poor applicability, and failure to consider whether ice avalanches can reach the ice lake, etc., and achieve early identification accuracy , high applicability effect
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Embodiment 1
[0045] An early identification method of a glacier lake outburst, comprising the following steps:
[0046] a. Determine the basic glacier data of the collapsing glacier lake and the surrounding unbursting glacier lake through Google Earth, including the ice tongue slope α at the back edge of the glacier lake, the slope aspect θ of the glacier, the vertical height H from the center of mass of the potential glacier body to the glacier lake, and the potential glacier The straight-line distance L from the mass center of the collapse mass to the ice lake, the width of the breach b, the thickness T of the breach, and the width w of the ice lake before the collapse 0 , the length-to-width ratio C of the glacial lake before the outburst, the slope β on the bank of the glacial lake before the outburst, and the area F of the continuous glacier;
[0047] b. There are two prerequisites for determining the occurrence of a glacier lake collapse. One is the ratio of the vertical height H fro...
Embodiment 2
[0062] An early identification method of a glacier lake outburst, comprising the following steps:
[0063] a. Determine the basic glacier data of the collapsing glacier lake and the surrounding unbursting glacier lake through Google Earth, including the ice tongue slope α at the back edge of the glacier lake, the slope aspect θ of the glacier, the vertical height H from the center of mass of the potential glacier body to the glacier lake, and the potential glacier The straight-line distance L from the mass center of the collapse mass to the ice lake, the width of the breach b, the thickness T of the breach, and the width w of the ice lake before the collapse 0 , the length-to-width ratio C of the glacial lake before the outburst, the slope β on the bank of the glacial lake before the outburst, and the area F of the continuous glacier;
[0064] b. There are two prerequisites for determining the occurrence of a glacier lake collapse. One is the ratio of the vertical height H fro...
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