A Differential Absorption Lidar (DIAL) for measurement of water vapour in the atmosphere of Mars emits light pulses at the “on” and “off” wavelengths shown in Figure 1. The recorded backscatter signals are shown in Figure 2. Use the signals to determine the average water vapour number density (molecules/m3 ) in the height range between 2.0 km and 2.5 km. The recorded signals at these heights are as follows: Non(2.0km) = 0.6 kHz ; Noff(2.0km) = 1.5 kHz Non(2.5km) = 0.27 kHz ; Noff(2.5km) = 0.96 kHz
A Differential Absorption Lidar (DIAL) for measurement of water vapour in the atmosphere of Mars emits light pulses at the “on” and “off” wavelengths shown in Figure 1. The recorded backscatter signals are shown in Figure 2. Use the signals to determine the average water vapour number density (molecules/m3 ) in the height range between 2.0 km and 2.5 km. The recorded signals at these heights are as follows: Non(2.0km) = 0.6 kHz ; Noff(2.0km) = 1.5 kHz Non(2.5km) = 0.27 kHz ; Noff(2.5km) = 0.96 kHz
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
Problem 1LR
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A Differential Absorption Lidar (DIAL) for measurement of water vapour in the atmosphere of Mars
emits light pulses at the “on” and “off” wavelengths shown in Figure 1. The recorded backscatter signals are
shown in Figure 2.
Use the signals to determine the average water vapour number density (molecules/m3
) in the height range
between 2.0 km and 2.5 km.
The recorded signals at these heights are as follows:
Non(2.0km) = 0.6 kHz ; Noff(2.0km) = 1.5 kHz
Non(2.5km) = 0.27 kHz ; Noff(2.5km) = 0.96 kHz
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