3. In a storm of 90 minutes duration, the incremental rainfall at various time intervals is given below. a. Maximum incremental depth (in mm) b. Maximum intensity (in mm/hr). TIME (minutes) 0 232SR 88 ID 20 30 40 50 60 70 80 90 CUMULATIVE (mm) C 6.2 8.5 14.5 21.7 27.9 33.0 35.1 36.2 37.0

Q: 9.15. The IDF function for 10- yr storms in Atlanta, Georgia, is given by i 1628 (t + 8.16)0.76…

A: maximum rainfall intensity occurs at 38% of the rainfall durationDuration= 40-min

Q: CE 141-2 HW2-A The mass curve of rainfall in a storm of total duration 90 minutes is given below.…

A:

Q: 10. Problema 9.16 The precipitation resulting storm in Miami, Florida is estimated to be…

A:

Q: 10. Problema 9.22 (Chin, edited) The precipitation resulting from a 25-year 24-hour storm in Miami,…

A:

Q: Q2) The hourly rainfall intensity data during a storm are as follows 01 2 3 45 6 7 89 10 Time (hrs)…

A:

Q: Q2) Use the 1-h Unit Hydrograph tabulated below to predict the total flood hydrograph that would be…

A: It is required to find the flood hydrograph from the resulting DRH.

Q: 9.16. The IDF function for 10- yr storms in Santa Fe, New Mexico, is given by 818 (t + 8.54)0.76…

A: Solving question firstGiven data,IDF function function for 10 yr given by maximum intensity occurs…

Q: Time (hrs) Depth (mm) of rainfall 1 5.86 2 1313 3068 4 16.79 10.53 13

A:

Sediment transport

Sediment transport or Soil transport is the movement of solid particles, usually due to the combination of gravitational forces acting on the sediment, and the movement of the liquid at which the sediment enters. Soil erosion occurs in natural systems where the particles are sandstones (sand, rocks), mud, or clay; the liquid is air, water, or ice; and the gravitational force that works to move particles to the landing surface. Sediment transportation or soil migration due to the movement of liquids occurs in rivers, lakes, lakes, oceans, and other bodies of water as a result of currents and waves. Transportation is also caused by glaciers as they flow, and to places on earth under the influence of wind. Soil erosion due to gravity alone is possible in most sloping areas, including hills, scarves, cliffs, and the continental shelf — the continental boundary of the slope.