Traduction de «Courbe intensité-durée d'une précipitation » (Français → Anglais) :

depth-duration curve | rainfall intensity-duration curve

intensity-duration curve | I-D curve | strength-duration curve | S-D curve

depth–duration curve | intensity–duration curve

intensity-duration-frequency curve [ IDF curve ]

intensity–duration–frequency curve

intensity-duration curve

rainfall intensity-duration curve

rainfall intensity curve [ rainfall-intensity curve | rainfall curve ]

depth-area curve | rainfall intensity-area curve

6. Notes also that, owing to the acceleration of glacial melting especially prevalent in the Himalayas and the Andes, mountainous regions are increasingly at threat from floods and avalanches; points out, however, that glacial melt is not the only factor affecting water flows in the Himalayas, but that timing and intensity of the monsoon, other rainfall and especially land use practices such as deforestation, overgrazing, agricultural systems and settlement patterns are determinant; in particular, stresses that deforestation frequently increases the rate and speed of the flow of water into major channels, while floods arising from ‘gla ...[+++]cier lake outburst floods’ (GLOFs) are often exacerbated by unsustainable land use practices;

6. Notes also that, owing to the acceleration of glacial melting especially prevalent in the Himalayas and the Andes, mountainous regions are increasingly at threat from floods and avalanches; points out, however, that glacial melt is not the only factor affecting water flows in the Himalayas, but that timing and intensity of the monsoon, other rainfall and especially land use practices such as deforestation, overgrazing, agricultural systems and settlement patterns are determinant; in particular, stresses that deforestation frequently increases the rate and speed of the flow of water into major channels, while floods arising from ‘gla ...[+++]cier lake outburst floods’ (GLOFs) are often exacerbated by unsustainable land use practices;

6. Notes also that, owing to the acceleration of glacial melting especially prevalent in the Himalayas and the Andes, mountainous regions are increasingly at threat from floods and avalanches; points out, however, that glacial melt is not the only factor affecting water flows in the Himalayas, but that timing and intensity of the monsoon, other rainfall and especially land use practices such as deforestation, overgrazing, agricultural systems and settlement patterns are determinant; in particular, stresses that deforestation frequently increases the rate and speed of the flow of water into major channels, while floods arising from ‘gla ...[+++]cier lake outburst floods’ (GLOFs) are often exacerbated by unsustainable land use practices;