–DOX
发表于 2025-3-27 00:38:08
Principles of Aerosol LIDAR Systemsic aerosols..The first part illustrates the classical representation of the LIDAR technique: monitoring coherent and undistinguishable photons travelling in and interacting with the non-homogeneous medium atmosphere. Then, it is given an overview of the architecture of LIDAR instruments that are mai
混沌
发表于 2025-3-27 02:09:32
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CLAM
发表于 2025-3-27 07:49:58
An Introduction to Rain Gauges and Disdrometerses will be briefly described to provide a useful overview of the local in situ measurement techniques. The measurements of drop size distribution provide a powerful opportunity to investigate the storm microphysics to be used in synergy with ground-based remote sensing instrument like radars. For th
观点
发表于 2025-3-27 09:51:19
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评论性
发表于 2025-3-27 14:27:45
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钳子
发表于 2025-3-27 19:34:51
Observing Microphysical Properties of Cloud and Rain relationship with atmospheric aerosols. The role of clouds and aerosols into the climate system and models is briefly discussed, with an emphasis on the associated uncertainty and the current level of understanding. Potential feedback effects of an increasing aerosols load are discussed. The chapte
偶像
发表于 2025-3-27 22:31:27
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Coeval
发表于 2025-3-28 03:33:37
Ground-Based Observing Systems for Atmospheric Aerosol Chemistry and Compositioncs of atmospheric aerosols, spanning a continuum size spectrum from 10. to 10. m and varying chemical compositions, mixing state, physical properties cause an infinite number of degrees of freedom which are not fully measurable by the existing instrumentation. This chapter introduces the most import
galley
发表于 2025-3-28 09:42:34
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小臼
发表于 2025-3-28 12:01:07
An Integrated Observing System for Boundary Layer Monitoring at Concordia Station, Antarcticaordia during 2004–2005. Concordia station is located over the Antarctic plateau at Dome C (Lat. 75° 06.06 S, Long. 123° 20.74 E, 3250 m a.s.l.) An observing system was set to during the field experiment to study the processes occurring in the long-lived stable, and in the weak convective atmospheric