Nov. 9 Artificial Modification of Clouds and Precip

Slides:



Advertisements
Similar presentations
Cloud Development and Precipitation
Advertisements

Precipitation Cloud particles are so small that they are easily kept afloat by even the weakest updrafts. This is why most clouds do not produce rain.
What’s Up With That Weather? Why Does It Rain? When rain clouds are pushed up into cold air the rain drops form and become heavy enough to be pulled.
Cloud Seeding in the Walker River Basin Arlen Huggins Desert Research Institute Scientific basis for wintertime cloud seeding Determining the potential.
Weather Review Battleship!. Air Basics As the temperature of a gas increases what happens to its volume? Increases.
MICHELLE WILSON LIGHTNING. BACKGROUND- LIGHTNING Separation of charges within the thunderstorm Ice particles tend to be positively charged Mix of water.
Project STORMFURY and Hurricane Modification NHRP 50 th 23MAY06 H. E. Willoughby, Dept of Earth Sciences, FIU, 21FEB07.
Warm cloud microstructures
G O D D A R D S P A C E F L I G H T C E N T E R How Is Urbanization Affecting Earth’s Weather, Climate and Water Cycle? Dr. J. Marshall Shepherd Deputy.
Chapter 5 Atmospheric Water and Weather
Class #4: Stability, cloud development, and precipitation Chapters 6 and 7 1Class #4 Monday, July 12, 2010.
Choose a category. You will be given the answer. You must give the correct question. Click to begin.
Welcome to Weather Science Jeopardy GeneralKnowledge Weather Factors I Weather Factors II ForecastingTools Final Jeopardy.
Chapter 5 Atmospheric Water and Weather
Hail and More. Today Hail How to stop hail? Hail Precipitation in the form of balls or irregular lumps of ice, only produced by convective clouds, usually.
Chapter 5: Cloud Development and Precipitation Atmospheric Stability Atmospheric Stability Determining stability Determining stability Cloud development.
The importance of clouds. The Global Climate System
Cloud Seeding §Examples of man's desire to modify weather are as old as recorded history. § The modern era of weather modification began in the late 1940s.
Robert W. Christopherson Charlie Thomsen Chapter 7 Water and Atmospheric Moisture.
5. Formation and Growth of Ice Crystals
Chapter 7 – Precipitation Processes
AOS 101 Weather and Climate Lisha M. Roubert University of Wisconsin-Madison Department of Atmospheric & Oceanic Sciences.
Fire Weather: Clouds & T-Storms. Physical structure of a cloud Minute water droplets Ice crystals Combination of both Why are clouds important for fire.
Hurricane Cloud Physics
Lecture 6: The Hydrologic Cycle EarthsClimate_Web_Chapter.pdfEarthsClimate_Web_Chapter.pdf, p. 10, 16-17, 21, 31-32, 34.
Moisture and Clouds Weather Unit When you see this megaphone, Click it for audio information Weather Unit When you see this megaphone, Click it for audio.
Clouds, Aerosols and Precipitation GRP Meeting August 2011 Susan C van den Heever Department of Atmospheric Science Colorado State University Fort Collins,
〉 When fronts move through an area, the result is usually precipitation and a change in wind direction and temperature. air mass: a large body of air.
Chapter 5: Cloud development and precipitation Atmospheric Stability Atmospheric Stability Determining stability Determining stability Cloud development.
Weather Instruments WindsMoistureStorms Weather Maps.
Hail. What is hail? Hail is a ball or irregular clump of ice Hail is different from winter precipitation! –Not sleet (raindrops that have frozen) –Not.
Lightning: Charge Separation Mechanisms, Detection and Applications Kaitlyn Suski May 29, 2009 SIO 209
Section 3.2: Weather Factors
WEATHER.
Lightning Outbreaks in the Eyewall MET 614 Seminar Antti Pessi.
Atmospheric Technology Division Rain In Cumulus over the Ocean Jorgen Jensen, Jeff Stith, Teresa Campos, Mary Barth, Dave Rogers NCAR science to complement.
Scott Rudlosky Characteristics of Positive Cloud-to-Ground Lightning Motivation and Goals Florida Power and Light Corporation dispatchers have observed.
Nature of Storms Chapter 13.
Precipitation Chapter 16 Section 5 Pages Chapter 16 Section 5 Pages
Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Section 3 Precipitation Chapter 23 Objectives Identify the four forms.
SCIENCE NEWS.
Edward Mansell National Severe Storms Laboratory Donald MacGorman and Conrad Ziegler National Severe Storms Laboratory, Norman, OK Funding sources in the.
The Thunderstorm: Ultimate Instability
Possible Aerosol Effects on Lightning Activity and Structure of Hurricanes Khain, A., N. Cohen, B. Lynn, and A. Pokrovsky, 2008: Possible aerosol effects.
Water in the Atmosphere Section 3 Section 3: Precipitation Preview Key Ideas Forms of Precipitation Causes of Precipitation Measuring Precipitation Weather.
Chapter 24 Water in the Atmosphere Section 3 Precipitation Notes 24-4.
Moist Processes SOEE1400: Lecture 11. SOEE1400 : Meteorology and Forecasting2 Water in the Atmosphere Almost all the water in the atmosphere is contained.
Weather. Atmosphere and Air Temperature insolation – the amount of the Sun’s energy that reaches Earth at a given time and place insolation – the amount.
Distribution of Liquid Water in Orographic Mixed-Phase Clouds Diana Thatcher Mentor: Linnea Avallone LASP REU 2011.
The AtmosphereSection 3 Fronts and Severe Weather 〉 How do fronts affect the weather? 〉 When fronts move through an area, the result is usually precipitation.
Fronts Mountains Heat Capacity Latent Heat “The Weather”
Severe Weather Weather Dynamics Science 10. Today we will learn about: Thunderstorms Updrafts Downdrafts Tornados Hurricanes Typhoons Tropical Cyclones.
Chien Wang Massachusetts Institute of Technology A Close Look at the Aerosol-Cloud Interaction in Tropical Deep Convection.
Background – Building their Case “continental” – polluted, aerosol laden “maritime” – clean, pristine Polluted concentrations are 1-2 orders of magnitude.
Weather. Atmosphere and Air Temperature insolation – the amount of the Sun’s energy that reaches Earth at a given time and place insolation – the amount.
Fog The result of the condensation of water vapor in the air. Difference between fog and clouds is that fog forms very near the surface of the earth–
What are the factors which affect the Uk climate?.
Water in the Atmosphere Section 3 Section 3: Precipitation Preview Key Ideas Forms of Precipitation Causes of Precipitation Measuring Precipitation Weather.
Microphysical-dynamical interactions in an idealized tropical cyclone simulation Stephen R. Herbener and William R. Cotton Colorado State University, Fort.
Deep Convective Clouds and Chemistry (DC3) Field Program.
THUNDERSTORMS.
Chapter 5: Cloud Development and Precipitation
THUNDERSTORMS.
Lecture 6: The Hydrologic Cycle
Thunderstorms – 13.1 The Nature of Storms.
PRECIPITATION & WEATHER MODIFICATION
Hurricanes This chapter discusses:
Chapter 5 Weather.
Review of Roesenfeld et al
Thunderstorms.
Presentation transcript:

Nov. 9 Artificial Modification of Clouds and Precip Thunderstorm Electrification Cloud and Precipitation Chemistry Additional problems due next Wednesday: 6.28, 6.34 (explain), 6.35, 6.36

Artificial Modification of Clouds, or, “Cloud Seeding”: Why ? improve conditions for aircraft encourage rain (for agriculture) Focus has been on cold clouds (T<0C) Idea: ice concetrations limited by ice nuclei number => Increase IN

“dry ice” - frozen CO2, thus T= -78 C Encourages homogeneous nucleation in its wake 1cm diameter => 1011 ice crystals! Supercooled liquid =>small ice crystals=>evaporation Used at airports (non-US, I think) Note stability

Artificial IN: silver iodide most common Works best when cloudtops ~ -14 C (why?) Who ? Israel, South Africa,Australia, US, more recently, China, Thailand 11/4/05

Though done to enhance precip, after much $$$, unclear results cloud seeding arguably most successful in mountaineous Areas Orographic lifiting produces large amounts of supercooled Water, at predictable locations Airflow patterns also important But: regions with little rain, also have variable rain anyway

Under the right conditions (weak stable layer cap), Can release further cloud buoyancy Picture from either Caribbean or Florida. More recent experiments in Texas show less dramatic cloud changes

Diffusing hurricanes through seeding: STORMFURY: Willoughby et al., BAMS, 1985 Seeding moves all freezing to 0C level,lower level of latent Heat release strengthens updrafts, intensifying hurricane, Ultimately widening eyewall & reducing wind speed. STORMFURY Could not prove hypothesis; hurricane seeding abandonned.

Urban island effects on precipitation Plenty of IN Aerosols found to decrease Droplet spectra, Leading to greater Separation of charge In mixed-phase regions, Increased lightning But Also increased precipitation

Lightning: Why care ? damage to property, life, aerospace indicator of convective dynamics, strength Technological advances have recently fostered field

Updrafts separate charges + + + - graupell - - - - + Graupel becomes negatively charged, lighter ice particles Are positive. Thought to reflect relative ease of movement Of positive ions in ice.

A ground-based lightning detection network detects Cloud-to-ground lightning. Satellites detect all lightning. In Tropics: all lightning/CG lightning ~ 10 In midlatitudes: all lightning/CG lightning ~ 2 Occasionally CG is positive. More violent. Mostly along Rocky Mountains satellite Detection at ground

Lightning detection from space: FORTE, LIS on TRMM LIS annual climatology Most lightning over land; FL highest incidence in US

High FL lightning frequency related to ocean-land breezes On both sides + lake breeze Maximum in July, next is August

FPL commissioned FSU to characterize lightning for Miami-Dade

Lightning also of interest for hurricane studies

Cloud and Precipitation Chemistry Clouds react to aerosols, but also modify them, By type and number Clouds transport gases and particles scavenge aerosols dissolve aerosols foster aqueous-phase chemical reactions scavenge through precipitation. Either diffusional, Or inertial

Transport of aerosols Possibly a large contributor to aerosol concs in marine subtropics