PPT-Precipitation

Double immunodiffusion Radial immunodiffusion Precipitation Is a secondary serological test where Ag is soluble not a particulate cell A precipitation line appears at optimal proportions of Ag and Ab not equal proportions. Cloud Naming. Prefix indicates height. Cirro. .  high, 5-13 km. Alto  middle, 2-5 km. (none)  low, 0-2 km. Name for appearance. Cirrus .  wispy strands. Stratus  layered, uniform. Cumulus puffy with vertical structure. Precipitation. We’ve studied the water cycle, and last week we focused on the “Condensation”. part. Now, we are going to discuss the precipitation part of the water cycle.. Let’s watch this video on Precipitation!. . Photograph: Tony Clarke, VOCALS . REx. flight RF07. Robert Wood. University of Washington. Dave Leon and Jeff Snider, University of Wyoming. Radiative. impact of cloud droplet concentration variations. Learning objectives. Be able to estimate area average precipitation from point measurements using a variety of methods. Estimate design rainfall amounts and intensities. Develop ArcGIS skills for analysis . CBRFC Stakeholder Forum. July 31, 2012. PRECIPITATION DATA. – . WHY IS THIS IMPORTANT ?. Primary Impacts:. Immediate runoff from rainfall events. Affects soil moisture conditions and seasonal volume forecasts. Read and study each page of this PowerPoint with your table group.. Each group member should take notes about each type of precipitation. . You are looking for information that describes:. How the different types of precipitation form. in Hainan Island. Lei Zhu. Paul . Markowski. , . Zhiyong. . Meng. and . Fuqing. Zhang. Research purpose. T. ry to understand the climatology . of . diurnal. . precipitation cycle in Hainan Island. Water vapor, droplets of water suspended in the air, builds up in the Earth's atmosphere. . Water vapor in the atmosphere is visible as clouds and fog. . Water vapor collects with other materials, such as dust, in clouds. Precipitation condenses, or forms, around these tiny pieces of material, called cloud condensation nuclei (CCN).. Water vapor, droplets of water suspended in the air, builds up in the Earth's atmosphere. . Water vapor in the atmosphere is visible as clouds and fog. . Water vapor collects with other materials, such as dust, in clouds. Precipitation condenses, or forms, around these tiny pieces of material, called cloud condensation nuclei (CCN).. Relief. There are three reasons why air is forced upward also forming three types of precipitation.. Relief . Precipitation- caused by winds carrying air up over a mountain barrier.. Convectional Precipitation. Observations. Brian A. Colle. 1. . and Aaron Naeger. 2. 1. School . of Marine and Atmospheric Sciences, Stony Brook University, Stony . Brook, NY. 2. University of Alabama at Huntsville. This work is supported by NASA PMM #. Acid Precipitation. Acid Precipitation. Acid precipitation. includes all forms of precipitation . (rain, sleet, snow. ). with a high concentration of acids present. . Acid precipitation forms when water vapor and droplets in the atmosphere combine with sulfuric and nitric oxides. This forms sulfuric and nitric acids, which have a lower pH than typical rainfall.. LECTURE 5. PRECIPITATION GAUGE NETWORK. To have an idea of areal distribution of precipitation there should be adequately planned rain gauge network. There are two reasons to plan a network:. Catch area of a precipitation gauge is very small. Mountains Experiment (OLYMPEX). Lynn McMurdie . University of Washington. (co-authors: Angela Rowe, Joe . Zagrodnik. ,. Stacy . Brodzik. , . Thomas . Schuldt. , Robert . Houze. . and. , . Jamin. .