Make It Rain: the Science Behind Altering the Weather

Total Page:16

File Type:pdf, Size:1020Kb

Make It Rain: the Science Behind Altering the Weather MAKE IT RAIN: THE SCIENCE BEHIND ALTERING THE WEATHER DARREL BAUMGARDNER MAKE IT RAIN: THE SCIENCE BEHIND ALTERING THE WEATHER WHENEVER HUMANKIND BELIEVES IT HAS CONTROL OVER THE NATURAL WORLD, THE WEATHER LIKES TO PROVE US WRONG. STORMS, FLOODS AND DROUGHTS ARE JUST SOME OF THE WEATHER PATTERNS THAT CAN COMPLICATE OR EVEN THREATEN HUMAN LIFE. WE HAVE INCREASINGLY SOPHISTICATED TECHNIQUES FOR WEATHER FORECASTING, BUT NOW SCIENTISTS ARE LOOKING EVEN FURTHER: TOWARDS DARREL BAUMGARDNER, OF THE DIRECTLY MODIFYING THE WEATHER ITSELF. AND DROPLET MEASUREMENT NATIONAL AUTONOMOUS UNIVERSITY OF MEXICO TECHNOLOGIES, RESEARCHES THE INTRIGUING TECHNIQUE OF CLOUD SEEDING TALK LIKE AN ATMOSPHERIC SCIENTIST GEOENGINEERING – deliberate, large-scale intervention in the Earth’s climate system, usually to mitigate climate change. CLIMATE – the general weather conditions over a long period. ICE NUCLEI (IN) – similar to CCN, particles in the atmosphere that ice crystals form around. CLOUD CONDENSATION NUCLEI (CCN) – small particles around which water vapour condenses and ultimately forms clouds. PRECIPITATION – water that falls from clouds to the ground, such as rain, hail, snow or sleet. CLOUD SEEDING – intentionally adding CCN to the atmosphere to change precipitation patterns. SPECTROMETER – an instrument that measures spectral properties, such as the reflective properties of cloud particles. DISDROMETER – a ground-based instrument to measure precipitation properties. WEATHER – the state of the atmosphere of a particular area at a particular time. Rain, or the lack of it, can cause problems. of investigating clouds, not only how they vapour in the atmosphere condenses into Too little rain can lead to droughts, which form but also how humans can influence clouds, but this process can only occur carries risks of crop failure and scarcity of their formation. As well as working with the presence of cloud condensation drinking water. Too much rain can cause within academia, he is the founder and nuclei (CCN). These are essentially small flooding and other forms of precipitation, Chief Scientist at Droplet Measurement particles of any number of substances, such such as hail, can cause physical damage to Technologies, which provides scientific as dust, soot or salt. To transition from a gas crops and property. Being able to influence instruments and expertise to researchers to a liquid, water molecules have to have when, where and how much rain falls could investigating aspects of cloud formation. something to cling onto, and CCN fulfil help prevent these negative effects. this function. Ice nuclei (IN) are the CCN WHAT IS CLOUD SEEDING? equivalent for the formation of ice crystals in Darrel Baumgardner has made a career A key step in the water cycle is when water the atmosphere. DARREL BAUMGARDNER National Autonomous University of Mexico and Chief Scientist at Droplet Measurement Technologies, Longmont, Colorado, USA FIELD OF RESEARCH Cloud seeding is a human-made technique that how they will respond to seeding, there are Atmospheric Science adds extra CCN or IN into the atmosphere, many factors to take into account, and at which can either enhance or suppress many different scales. For instance, the precipitation, depending on how, when and nucleation of cloud droplets around a CCN RESEARCH PROJECT where it’s done. This technique was famously happens at the microscopic level and in a used to keep the 2008 Beijing Olympics dry: matter of milliseconds, whereas the time to Investigating how clouds form, rockets containing silver iodide particles (a grow to visible raindrops (and eventually entire and how we can influence type of IN) were fired into the atmosphere, clouds) can take minutes to hours. When this their formation. intercepting incoming rainclouds and triggering is expanded to include the interconnected premature showers before they could reach cloud formation over entire regions, it gets the capital. complicated very fast. HOW CAN YOU MEASURE SUCH A However, this complexity is not COMPLEX SYSTEM? insurmountable. “Modern computers have Atmospheric science is very complex, and provided cloud modellers with the tools needed scientists simply don’t have all the information to create such models,” says Darrel. Model required to guarantee that cloud seeding will inputs include temperature, pressure, relative news for coral reefs and other underwater have the intended effect. In some instances, humidity, CCN and IN specific to a certain ecosystems. One project is looking into cloud seeding can even lead to the opposite time and area, and then different seeding seeding stratus clouds over the Great Barrier effect to that intended. There is also a certain scenarios are run to see how they affect cloud Reef, which would deflect sunlight away from lack of control. “Once the seeding material properties. As with any model, it remains a the sea’s surface and mitigate warming in that is released, there is nothing more that can be simplified representation of the real world, so area. In theory, this practice could be carried done,” says Darrel. results aren’t perfect, but are getting more out worldwide. precise all the time. Measuring cloud properties, and how they However, given the complex nature of react to different conditions, is essential. THE BIGGER PICTURE atmospheric science, geoengineering efforts “There are two general types of instruments Cloud seeding could help mitigate against on a global scale pose many challenges for used to measure cloud properties,” says droughts, floods and even air pollution, but scientists. For example, stimulating rainfall Darrel. The first are called disdrometers, and there are, perhaps, even bigger and more long- to alleviate drought in one area could lead to measure precipitation at the ground, including term applications. Geoengineering is the name extreme monsoons in another. Experts in this variables such as drop size, velocity and type of given to techniques that aim not just to alter field are mindful that they need to consider precipitation. The second type measures the the weather but also the climate, to attempt the intricacies of the bigger picture. As Darrel properties of clouds themselves and are called to counteract the effects of climate change. explains, with processes such as cloud seeding, spectrometers. By fixing a spectrometer to an When carried out at a global scale, cloud there is always the, “Goldilocks conundrum” aircraft or drone and flying it through a cloud, seeding and similar techniques are the most and the challenge is in getting things ‘just scientists can record cloud water content significant of these proposed measures. right’. He adds, “As atmospheric scientists, we and a number of other variables. Similar know that climate change is real.” Scientists measurements can also be taken from a great “Geoengineering has the potential to offset like Darrel can make a huge difference to our distance, using radar or even satellites. the negative impacts of climate change,” says world – will you be one of them? Darrel. For instance, one effect of climate HOW CAN SCIENTISTS MODEL CLOUD change is the absorption of the sun’s heat by PROPERTIES? the oceans, which raises marine temperatures When it comes to modelling clouds to predict and can lead to ocean acidification – bad ABOUT ATMOSPHERIC SCIENCE WHAT IS ATMOSPHERIC SCIENCE? instruments,” says Darrel. “We can also run know that climate change is real and is the Atmospheric science studies the layers of gas computers hundreds of times more powerful greatest danger that the world faces today,” that surround the planet, specifically their than just a few decades ago.” These huge says Darrel. Not only does atmospheric chemistry and their dynamics. This includes advancements mean that understanding of science provide us with much of the data interactions within the atmosphere, and atmospheric science is accelerating. “We about climate change – its predicted evolution between the atmosphere and other entities, know so much more about how clouds evolve and effects –, it also suggests ways we could such as the ocean or human activity. than we did 50 years ago, but we still have a protect ourselves against it. long way to go before we can truly ‘control’ Our atmosphere is the relatively thin barrier weather,” says Darrel. Atmospheric science has a huge amount to that separates the Earth’s surface from space. teach us about the present and the future of “Although the atmosphere makes up a small WHAT ARE THE REAL-WORLD our planet, and a career in it could have far- fraction of the Earth’s volume, it is critical to APPLICATIONS OF ATMOSPHERIC reaching positive impacts for society. life, not only for the oxygen we need but also SCIENCE? for the hydrological cycle.” The science that Weather forecasting, although it might seem attempts to explain it is complex and detailed, a rather bland aspect of everyday life, has the but has come on in leaps and bounds in recent potential to save countless lives. Forecasting decades. tropical storms, tornados or hurricanes, for instance, can help people prepare and HOW HAS THE FIELD CHANGED OVER safeguard themselves and their livelihoods. THE YEARS? “We are now able to make faster and more Atmospheric science also underpins much Seeding material is dispensed by burning flares like accurate measurements with much smaller of what we know about climate change. “We those seen attached to the trailing edge of the wing of this seeding aircraft. How to become an atmospheric scientist • According to NASA, a career in
Recommended publications
  • Geography and Atmospheric Science 1
    Geography and Atmospheric Science 1 Undergraduate Research Center is another great resource. The center Geography and aids undergraduates interested in doing research, offers funding opportunities, and provides step-by-step workshops which provide Atmospheric Science students the skills necessary to explore, investigate, and excel. Atmospheric Science labs include a Meteorology and Climate Hub Geography as an academic discipline studies the spatial dimensions of, (MACH) with state-of-the-art AWIPS II software used by the National and links between, culture, society, and environmental processes. The Weather Service and computer lab and collaborative space dedicated study of Atmospheric Science involves weather and climate and how to students doing research. Students also get hands-on experience, those affect human activity and life on earth. At the University of Kansas, from forecasting and providing reports to university radio (KJHK 90.7 our department's programs work to understand human activity and the FM) and television (KUJH-TV) to research project opportunities through physical world. our department and the University of Kansas Undergraduate Research Center. Why study geography? . Because people, places, and environments interact and evolve in a changing world. From conservation to soil science to the power of Undergraduate Programs geographic information science data and more, the study of geography at the University of Kansas prepares future leaders. The study of geography Geography encompasses landscape and physical features of the planet and human activity, the environment and resources, migration, and more. Our Geography integrates information from a variety of sources to study program (http://geog.ku.edu/degrees/) has a unique cross-disciplinary the nature of culture areas, the emergence of physical and human nature with pathway options (http://geog.ku.edu/geography-pathways/) landscapes, and problems of interaction between people and the and diverse faculty (http://geog.ku.edu/faculty/) who are passionate about environment.
    [Show full text]
  • Air Quality in North America's Most Populous City
    Atmos. Chem. Phys., 7, 2447–2473, 2007 www.atmos-chem-phys.net/7/2447/2007/ Atmospheric © Author(s) 2007. This work is licensed Chemistry under a Creative Commons License. and Physics Air quality in North America’s most populous city – overview of the MCMA-2003 campaign L. T. Molina1,2, C. E. Kolb3, B. de Foy1,2,4, B. K. Lamb5, W. H. Brune6, J. L. Jimenez7,8, R. Ramos-Villegas9, J. Sarmiento9, V. H. Paramo-Figueroa9, B. Cardenas10, V. Gutierrez-Avedoy10, and M. J. Molina1,11 1Department of Earth, Atmospheric and Planetary Science, Massachusetts Institute of Technology, Cambridge, MA, USA 2Molina Center for Energy and Environment, La Jolla, CA, USA 3Aerodyne Research, Inc., Billerica, MA, USA 4Saint Louis University, St. Louis, MO, USA 5Laboratory for Atmospheric Research, Department of Civil and Environmental Engineering, Washington State University, Pullman, WA, USA 6Department of Meteorology, Pennsylvania State University, University Park, PA, USA 7Department of Chemistry and Biochemistry, University of Colorado at Boulder, Boulder, CO, USA 8Cooperative Institute for Research in the Environmental Sciences (CIRES), Univ. of Colorado at Boulder, Boulder, CO, USA 9Secretary of Environment, Government of the Federal District, Mexico, DF, Mexico 10National Center for Environmental Research and Training, National Institute of Ecology, Mexico, DF, Mexico 11Department of Chemistry and Biochemistry, University of California at San Diego, San Diego, CA, USA Received: 22 February 2007 – Published in Atmos. Chem. Phys. Discuss.: 27 February 2007 Revised: 10 May 2007 – Accepted: 10 May 2007 – Published: 14 May 2007 Abstract. Exploratory field measurements in the Mexico 1 Introduction City Metropolitan Area (MCMA) in February 2002 set the stage for a major air quality field measurement campaign in 1.1 Air pollution in megacities the spring of 2003 (MCMA-2003).
    [Show full text]
  • Assessing and Improving Cloud-Height Based Parameterisations of Global Lightning Flash Rate, and Their Impact on Lightning-Produced Nox and Tropospheric Composition
    https://doi.org/10.5194/acp-2020-885 Preprint. Discussion started: 2 October 2020 c Author(s) 2020. CC BY 4.0 License. Assessing and improving cloud-height based parameterisations of global lightning flash rate, and their impact on lightning-produced NOx and tropospheric composition 5 Ashok K. Luhar1, Ian E. Galbally1, Matthew T. Woodhouse1, and Nathan Luke Abraham2,3 1CSIRO Oceans and Atmosphere, Aspendale, 3195, Australia 2National Centre for Atmospheric Science, Department of Chemistry, University of Cambridge, Cambridge, UK 3Department of Chemistry, University of Cambridge, Cambridge, UK 10 Correspondence to: Ashok K. Luhar ([email protected]) Abstract. Although lightning-generated oxides of nitrogen (LNOx) account for only approximately 10% of the global NOx source, it has a disproportionately large impact on tropospheric photochemistry due to the conducive conditions in the tropical upper troposphere where lightning is mostly discharged. In most global composition models, lightning flash rates used to calculate LNOx are expressed in terms of convective cloud-top height via the Price and Rind (1992) (PR92) 15 parameterisations for land and ocean. We conduct a critical assessment of flash-rate parameterisations that are based on cloud-top height and validate them within the ACCESS-UKCA global chemistry-climate model using the LIS/OTD satellite data. While the PR92 parameterisation for land yields satisfactory predictions, the oceanic parameterisation underestimates the observed flash-rate density severely, yielding a global average of 0.33 flashes s-1 compared to the observed 9.16 -1 flashes s over the ocean and leading to LNOx being underestimated proportionally. We formulate new/alternative flash-rate 20 parameterisations following Boccippio’s (2002) scaling relationships between thunderstorm electrical generator power and storm geometry coupled with available data.
    [Show full text]
  • Atmospheric Science Brochure
    Welcome from the Atmospheric Science Program! FForor MMoreore IInformationnformation Our program is led by seven faculty members Professor Clark Evans with expertise in atmospheric dynamics, weather Atmospheric Science Program Coordinator analysis and forecasting, cloud physics, air pollution meteorology, tropical and mesoscale meteorology, P. O. Box 413, Milwaukee, WI 53201 and chaotic systems. (414) 229-5116 [email protected] Your professional development is our top priority! We offer lots of faculty contact, opportunities for hands-on research, excellent computational facilities, and an array of courses to prepare you for your career. Learn more about the Atmospheric Science Study Abroad Visit us Online Atmospheric Science UWM offers the world’s www.math.uwm.edu/atmo fi rst faculty-led Major J study-abroad www.facebook.com/UWMAtmoSci program in www.innovativeweather.com Atmospheric Science. In this course, you can explore the effects of acid rain on Mexico’s cultural heritage sites. Atmospheric Science Major at the University of Wisconsin – Milwaukee The study of weather, climate, and their impacts on both Earth and human activities AAtmospherictmospheric SSciencecience CCareersareers PPreparatoryreparatory CCreditsredits BBeyondeyond tthehe CClassroomlassroom A career in atmospheric science is very rewarding • Math 231: Calculus and Analytic Geometry I Atmospheric Science because of the impact weather and climate have on • Math 232: Calculus and Analytic Geometry I INNNOVANOVATTIVEIVE students can work everyday life. You will fi nd atmospheric scientists • Math 233: Calculus and Analytic Geometry III WEEATHERATHER with real clients in many different roles: nearly 36% work in the • Math 234: Linear Algebra/Differential Equations providing forecasts, private sector; 33% for governmental agencies; 24% • Math 320: Intro to Differential Equations risk assessments and other weather-related services at educational institutions or laboratories; and 7% in • Physics 209/214: Physics I with Lab to the community and business partners across the media.
    [Show full text]
  • ESSENTIALS of METEOROLOGY (7Th Ed.) GLOSSARY
    ESSENTIALS OF METEOROLOGY (7th ed.) GLOSSARY Chapter 1 Aerosols Tiny suspended solid particles (dust, smoke, etc.) or liquid droplets that enter the atmosphere from either natural or human (anthropogenic) sources, such as the burning of fossil fuels. Sulfur-containing fossil fuels, such as coal, produce sulfate aerosols. Air density The ratio of the mass of a substance to the volume occupied by it. Air density is usually expressed as g/cm3 or kg/m3. Also See Density. Air pressure The pressure exerted by the mass of air above a given point, usually expressed in millibars (mb), inches of (atmospheric mercury (Hg) or in hectopascals (hPa). pressure) Atmosphere The envelope of gases that surround a planet and are held to it by the planet's gravitational attraction. The earth's atmosphere is mainly nitrogen and oxygen. Carbon dioxide (CO2) A colorless, odorless gas whose concentration is about 0.039 percent (390 ppm) in a volume of air near sea level. It is a selective absorber of infrared radiation and, consequently, it is important in the earth's atmospheric greenhouse effect. Solid CO2 is called dry ice. Climate The accumulation of daily and seasonal weather events over a long period of time. Front The transition zone between two distinct air masses. Hurricane A tropical cyclone having winds in excess of 64 knots (74 mi/hr). Ionosphere An electrified region of the upper atmosphere where fairly large concentrations of ions and free electrons exist. Lapse rate The rate at which an atmospheric variable (usually temperature) decreases with height. (See Environmental lapse rate.) Mesosphere The atmospheric layer between the stratosphere and the thermosphere.
    [Show full text]
  • Cloud and Precipitation Radars
    Sponsored by the U.S. Department of Energy Office of Science, the Atmospheric Radiation Measurement (ARM) Climate Research Facility maintains heavily ARM Radar Data instrumented fixed and mobile field sites that measure clouds, aerosols, Radar data is inherently complex. ARM radars are developed, operated, and overseen by engineers, scientists, radiation, and precipitation. data analysts, and technicians to ensure common goals of quality, characterization, calibration, data Data from these sites are used by availability, and utility of radars. scientists to improve the computer models that simulate Earth’s climate system. Storage Process Data Post- Data Cloud and Management processing Products Precipitation Radars Mentors Mentors Cloud systems vary with climatic regimes, and observational DQO Translators Data capabilities must account for these differences. Radars are DMF Developers archive Site scientist DMF the only means to obtain both quantitative and qualitative observations of clouds over a large area. At each ARM fixed and mobile site, millimeter and centimeter wavelength radars are used to obtain observations Calibration Configuration of the horizontal and vertical distributions of clouds, as well Scan strategy as the retrieval of geophysical variables to characterize cloud Site operations properties. This unprecedented assortment of 32 radars Radar End provides a unique capability for high-resolution delineation Mentors science users of cloud evolution, morphology, and characteristics. One-of-a-Kind Radar Network Advanced Data Products and Tools All ARM radars, with the exception of three, are equipped with dual- Reectivity (dBz) • Active Remotely Sensed Cloud Locations (ARSCL) – combines data from active remote sensors with polarization technology. Combined -60 -40 -20 0 20 40 50 60 radar observations to produce an objective determination of hydrometeor height distributions and retrieval with multiple frequencies, this 1 μm 10 μm 100 μm 1 mm 1 cm 10 cm 10-3 10-2 10-1 100 101 102 of cloud properties.
    [Show full text]
  • Spatial Trends in United States Tornado Frequency
    www.nature.com/npjclimatsci ARTICLE OPEN Spatial trends in United States tornado frequency Vittorio A. Gensini 1 and Harold E. Brooks2 Severe thunderstorms accompanied by tornadoes, hail, and damaging winds cause an average of 5.4 billion dollars of damage each year across the United States, and 10 billion-dollar events are no longer uncommon. This overall economic and casualty risk—with over 600 severe thunderstorm related deaths in 2011—has prompted public and scientific inquiries about the impact of climate change on tornadoes. We show that national annual frequencies of tornado reports have remained relatively constant, but significant spatially-varying temporal trends in tornado frequency have occurred since 1979. Negative tendencies of tornado occurrence have been noted in portions of the central and southern Great Plains, while robust positive trends have been documented in portions of the Midwest and Southeast United States. In addition, the significant tornado parameter is used as an environmental covariate to increase confidence in the tornado report results. npj Climate and Atmospheric Science (2018) 1:38 ; doi:10.1038/s41612-018-0048-2 INTRODUCTION A derived covariate, such as STP, is complementary to tornado Recent trends in global and United States temperature have reports for climatological studies. For example, it has been shown provoked questions about the impact on frequency, intensity, that variables like storm relative helicity and convective precipita- timing, and location of tornadoes. When removing many non- tion adequately represent United States monthly tornado 16 meteorological factors, it is shown that the annual frequency of frequency. Reports are subject to a human reporting process, United States tornadoes through the most reliable portions of the whereas environmental covariates allow for an objective model- historical record has remained relatively constant.1–4 The most derived climatology.
    [Show full text]
  • Our Atmosphere Greece Sicily Athens
    National Aeronautics and Space Administration Sardinia Italy Turkey Our Atmosphere Greece Sicily Athens he atmosphere is a life-giving blanket of air that surrounds our Crete T Tunisia Earth; it is composed of gases that protect us from the Sun’s intense ultraviolet Gulf of Gables radiation, allowing life to flourish. Greenhouse gases like carbon dioxide, Mediterranean Sea ozone, and methane are steadily increasing from year to year. These gases trap infrared radiation (heat) emitted from Earth’s surface and atmosphere, Gulf of causing the atmosphere to warm. Conversely, clouds as well as many tiny Sidra suspended liquid or solid particles in the air such as dust, smoke, and Egypt Libya pollution—called aerosols—reflect the Sun’s radiative energy, which leads N to cooling. This delicate balance of incoming and reflected solar radiation 200 km and emitted infrared energy is critical in maintaining the Earth’s climate Turkey Greece and sustaining life. Research using computer models and satellite data from NASA’s Earth Sicily Observing System enhances our understanding of the physical processes Athens affecting trends in temperature, humidity, clouds, and aerosols and helps us assess the impact of a changing atmosphere on the global climate. Crete Tunisia Gulf of Gables Mediterranean Sea September 17, 1979 Gulf of Sidra October 6, 1986 September 20, 1993 Egypt Libya September 10, 2000 Aerosol Index low high September 24, 2006 On August 26, 2007, wildfires in southern Greece stretched along the southwest coast of the Peloponnese producing Total Ozone (Dobson Units) plumes of smoke that drifted across the Mediterranean Sea as far as Libya along Africa’s north coast.
    [Show full text]
  • The Cloud Cycle and Acid Rain
    gX^\[`i\Zk\em`ifed\ekXc`dgXZkjf]d`e`e^Xkc`_`i_`^_jZ_ffcYffbc\k(+ ( K_\Zcfl[ZpZc\Xe[XZ`[iX`e m the mine ke fro smo uld rain on Lihir? Co e acid caus /P 5IJTCPPLMFUXJMM FYQMBJOXIZ K_\i\Xjfe]fik_`jYffbc\k K_\i\`jefXZ`[iX`efeC`_`i% `jk_Xkk_\i\_XjY\\ejfd\ K_`jYffbc\k\ogcX`ejk_\jZ`\eZ\ d`jle[\ijkXe[`e^XYflkk_\ Xe[Z_\d`jkipY\_`e[XZ`[iX`e% \o`jk\eZ\f]XZ`[iX`efeC`_`i% I\X[fekfÔe[flkn_pk_\i\`jef XZ`[iX`efeC`_`i55 page Normal rain cycle and acid rain To understand why there is no acid rain on Lihir we will look at: 1 How normal rain is formed 2 2 How humidity effects rain formation 3 3 What causes acid rain? 4 4 How much smoke pollution makes acid rain? 5 5 Comparing pollution on Lihir with Sydney and China 6 6 Where acid rain does occur 8–9 7 Could acid rain fall on Lihir? 10–11 8 The effect of acid rain on the environment 12 9 Time to check what you’ve learnt 13 Glossary back page Read the smaller text in the blue bar at the bottom of each page if you want to understand the detailed scientific explanations. > > gX^\) ( ?fnefidXciX`e`j]fid\[ K_\eXkliXcnXk\iZpZc\ :cfl[jXi\]fid\[n_\e_\Xk]ifdk_\jleZXlj\jk_\nXk\i`e k_\fZ\Xekf\mXgfiXk\Xe[Y\Zfd\Xe`em`j`Yc\^Xj% K_`j^Xji`j\j_`^_`ekfk_\X`in_\i\Zffc\ik\dg\iXkli\jZXlj\ `kkfZfe[\ej\Xe[Y\Zfd\k`epnXk\i[ifgc\kj%N_\edXepf] k_\j\nXk\i[ifgc\kjZfcc`[\kf^\k_\ik_\pdXb\Y`^^\inXk\i [ifgj#n_`Z_Xi\kff_\XmpkfÕfXkXifle[`ek_\X`iXe[jfk_\p ]Xcc[fneXjiX`e%K_`jgifZ\jj`jZXcc\[gi\Z`g`kXk`fe% K_\eXkliXcnXk\iZpZc\ _\Xk]ifd k_\jle nXk\imXgflijZfe[\ej\ kfZi\Xk\Zcfl[j gi\Z`g`kXk`fe \mXgfiXk`fe K_\jZ`\eZ\Y\_`e[iX`e K_\_\Xk]ifdk_\jleZXlj\jnXk\i`ek_\
    [Show full text]
  • 2009, Umaine News Press Releases
    The University of Maine DigitalCommons@UMaine General University of Maine Publications University of Maine Publications 2009 2009, UMaine News Press Releases University of Maine George Manlove University of Maine Joe Carr University of Maine Follow this and additional works at: https://digitalcommons.library.umaine.edu/univ_publications Part of the Higher Education Commons, and the History Commons Repository Citation University of Maine; Manlove, George; and Carr, Joe, "2009, UMaine News Press Releases" (2009). General University of Maine Publications. 1091. https://digitalcommons.library.umaine.edu/univ_publications/1091 This Monograph is brought to you for free and open access by DigitalCommons@UMaine. It has been accepted for inclusion in General University of Maine Publications by an authorized administrator of DigitalCommons@UMaine. For more information, please contact [email protected]. UMaine News Press Releases from Word Press XML export 2009 UMaine Climate Change Institute Community Lecture in Bangor Jan. 14 02 Jan 2009 Contact: Gregory Zaro, 581-1857 or [email protected] ORONO -- Gregory Zaro, assistant professor in the University of Maine's Anthropology Department and Climate Change Institute, will present "Ancient Civilizations, Archaeology and Environmental Change in South America" from 6:30 to 7:45 p.m. Wednesday, Jan.14, at the Bangor Public Library. Zaro's talk is the third installment in the Climate Change Institute's monthly lecture series, which is free and open to the public. According to Zaro, humans are active components of the environment and have been manipulating the physical world for thousands of years. While modern industrial nations are often viewed to have the greatest impact on ecological change, ancient civilizations have also left long-lasting imprints on the landscape that continue to shape our contemporary world.
    [Show full text]
  • Cold Season Cloud Seeding
    Weather Modification UNDERSTANDING Cloud seeding—a form of weather modification— ALBERTA CANADA COLD SEASON is a safe, scientific, time-tested, and proven set of Cloud Seeding technologies used to enhance rain and snow, re- ND duce hail damage, and alleviate fog. The benefits ID of cloud seeding can be measured in additional WY water for cities and agriculture, as well as the re- NV UT duction of damage from severe weather. CA CO KS TX Target area—Cold-season cloud-seeding Target area—Warm-season cloud-seeding A ground-based generator is used to burn a silver iodide solution to release microscopic silver-iodide particles which can create additional ice crystals, then snow, in winter clouds. Research has shown that placing equipment at high elevations increases cloud seeding effectiveness. NAWMC Members Cold Season Seeding California Department of Water Resources When moist air flows over the mountains, water vapor Colorado Water Conservation Board condenses and forms clouds composed of water droplets. These droplets become “super cooled” and have the unique Desert Research Institute quality to remain liquid even at temperatures below freez- North Dakota Atmospheric Resource Board ing. Given enough time and mixing with surrounding air, many of the droplets will evaporate, but under the correct Texas Department of Licensing and Regulation conditions some will eventually become ice crystals, grow Utah Division of Water Resources into snowflakes and precipitate to the ground. Cloud seed- Wyoming Water Development Office ing provides an opportunity to increase the number of ice crystals that can become snowflakes. NAWMC Associate Members Who Conducts Cloud Seeding? Central Arizona Water Conservation District In North America, cloud-seeding programs are conducted in Metropolitan Water District of Southern California California, Colorado, Idaho, Nevada, Utah, Wyoming, Kansas, Santa Barbara County Water Agency North Dakota, and Texas, as well as Alberta, Canada.
    [Show full text]
  • Atmospheric Physics I
    Atmospheric Physics I PHYS 621, Fall 2016 Dates and Location: Tuesday & Thursday, 2:30PM- 3:45AM; Public Policy 367 INSTRUCTOR: Dr. Pengwang Zhai Email: [email protected] Ph.: 410-455-3682 (office) OFFICE HOURS: Anytime Through Email appointment TEXTS: Wallace, J.M. and P. V. Hobbs, Atmospheric Science: An Introductory Survey, 2nd ed., Elsevier, 2006 Salby, M. L., Fundamentals of Atmospheric Physics, Academic Press, 1996. REFERENCE TEXTS (Highly recommend): Holton, J. R. Introduction to Dynamic Meteorology, 4th ed., Academic Press, 2004. DESCRIPTION: Composition and structure of the earth's atmosphere, atmospheric radiation and thermodynamics, fundamentals of atmospheric dynamics, overview of climatology. GRADING: Homework (25%), Midterm (30%), Final (40%), Participation/Discussion(5%) Course Strategy: There will be no exam make-up except for University-policy accepted absence. To promote active learning, students are strongly encouraged to read the corresponding textbook chapters before each lecture. Pre-lecture homework and discussion assignments are given routinely before lectures. Reading the sections of the textbook corresponding to the assigned homework exercises is considered part of the homework assignment; you are responsible for material in the assigned reading whether or not it is discussed in the lecture. Homework will be due weekly in Thursday’s lecture. There will be a 30% penalty on late homework submissions. COURSE OUTLINE: Overview A. Earth's atmosphere System of units The Sun and the orbit and size of Earth Chemical constituents of Earth’s atmosphere Vertical structure of temperature and density Wind and precipitation Ozone layer, hydrological and carbon cycles Global Energy Budget B. Atmospheric Radiation Maxwell’s Equation & EM wave Blackbody radiation: Planck’s Law and Stefan-Boltzmann’s law Spectral characteristics of Solar and Thermal infrared radiation Atmospheric absorption & Greenhouse effect Atmospheric scattering, clouds and aerosols Radiative forcing and climate Spatial and Temporal distribution of solar radiation C.
    [Show full text]