Africa's Climate: Helping Decision-Makers Make Sense Of
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3. Electrical Structure of Thunderstorm Clouds
3. Electrical Structure of Thunderstorm Clouds 1 Cloud Charge Structure and Mechanisms of Cloud Electrification An isolated thundercloud in the central New Mexico, with rudimentary indication of how electric charge is thought to be distributed and around the thundercloud, as inferred from the remote and in situ observations. Adapted from Krehbiel (1986). 2 2 Cloud Charge Structure and Mechanisms of Cloud Electrification A vertical tripole representing the idealized gross charge structure of a thundercloud. The negative screening layer charges at the cloud top and the positive corona space charge produced at ground are ignored here. 3 3 Cloud Charge Structure and Mechanisms of Cloud Electrification E = 2 E (−)cos( 90o−α) Q H = 2 2 3/2 2πεo()H + r sinα = k Q = const R2 ( ) Method of images for finding the electric field due to a negative point charge above a perfectly conducting ground at a field point located at the ground surface. 4 4 Cloud Charge Structure and Mechanisms of Cloud Electrification The electric field at ground due to the vertical tripole, labeled “Total”, as a function of the distance from the axis of the tripole. Also shown are the contributions to the total electric field from the three individual charges of the tripole. An upward directed electric field is defined as positive (according to the physics sign convention). 5 5 Cloud Charge Structure and Mechanisms of Cloud Electrification Electric Field Change Due to Negative Cloud-to-Ground Discharge Electric Field Change Due to a Cloud Discharge Electric Field Change, kV/m Change, Electric Field Electric Field Change, kV/m Change, Electric Field Distance, km Distance, km Electric field change at ground, due to the Electric field change at ground, due to the total removal of the negative charge of the total removal of the negative and upper vertical tripole via a cloud-to-ground positive charges of the vertical tripole via a discharge, as a function of distance from cloud discharge, as a function of distance from the axis of the tripole. -
Link Between the Double-Intertropical Convergence Zone Problem and Cloud Biases Over the Southern Ocean
Link between the double-Intertropical Convergence Zone problem and cloud biases over the Southern Ocean Yen-Ting Hwang1 and Dargan M. W. Frierson Department of Atmospheric Sciences, University of Washington, Seattle, WA 98195-1640 Edited by Mark H. Thiemens, University of California at San Diego, La Jolla, CA, and approved February 15, 2013 (received for review August 2, 2012) The double-Intertropical Convergence Zone (ITCZ) problem, in which climate models show that the bias can be reduced by changing excessive precipitation is produced in the Southern Hemisphere aspects of the convection scheme (e.g., refs. 7–9) or changing the tropics, which resembles a Southern Hemisphere counterpart to the surface wind stress formulation (e.g., ref. 10). Given the complex strong Northern Hemisphere ITCZ, is perhaps the most significant feedback processes in the tropics, it is challenging to understand and most persistent bias of global climate models. In this study, we the mechanisms by which the sensitivity experiments listed above look to the extratropics for possible causes of the double-ITCZ improve tropical precipitation. problem by performing a global energetic analysis with historical Recent work in general circulation theory has suggested that simulations from a suite of global climate models and comparing one should not only look within the tropics for features that affect with satellite observations of the Earth’s energy budget. Our results tropical precipitation. A set of idealized experiments showed that show that models with more energy flux into the Southern heating a global climate model exclusively in the extratropics can Hemisphere atmosphere (at the top of the atmosphere and at the lead to tropical rainfall shifts from one side of the tropics to the surface) tend to have a stronger double-ITCZ bias, consistent with other (11). -
Climatic Information of Western Sahel F
Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Clim. Past Discuss., 10, 3877–3900, 2014 www.clim-past-discuss.net/10/3877/2014/ doi:10.5194/cpd-10-3877-2014 CPD © Author(s) 2014. CC Attribution 3.0 License. 10, 3877–3900, 2014 This discussion paper is/has been under review for the journal Climate of the Past (CP). Climatic information Please refer to the corresponding final paper in CP if available. of Western Sahel V. Millán and Climatic information of Western Sahel F. S. Rodrigo (1535–1793 AD) in original documentary sources Title Page Abstract Introduction V. Millán and F. S. Rodrigo Conclusions References Department of Applied Physics, University of Almería, Carretera de San Urbano, s/n, 04120, Almería, Spain Tables Figures Received: 11 September 2014 – Accepted: 12 September 2014 – Published: 26 September J I 2014 Correspondence to: F. S. Rodrigo ([email protected]) J I Published by Copernicus Publications on behalf of the European Geosciences Union. Back Close Full Screen / Esc Printer-friendly Version Interactive Discussion 3877 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract CPD The Sahel is the semi-arid transition zone between arid Sahara and humid tropical Africa, extending approximately 10–20◦ N from Mauritania in the West to Sudan in the 10, 3877–3900, 2014 East. The African continent, one of the most vulnerable regions to climate change, 5 is subject to frequent droughts and famine. One climate challenge research is to iso- Climatic information late those aspects of climate variability that are natural from those that are related of Western Sahel to human influences. -
Along-Axis Variations of Rift Width in a Coupled Lithosphere-Mantle
Along-Axis Variations of Rift Width in a Coupled Lithosphere-Mantle System, Application to East Africa Alexander Koptev, Eric Calais, Evgueni Burov, Sylvie Leroy, Taras Gerya To cite this version: Alexander Koptev, Eric Calais, Evgueni Burov, Sylvie Leroy, Taras Gerya. Along-Axis Variations of Rift Width in a Coupled Lithosphere-Mantle System, Application to East Africa. Geophysical Re- search Letters, American Geophysical Union, 2018, 45 (11), pp.5362 - 5370. 10.1029/2018GL077276. hal-01828935 HAL Id: hal-01828935 https://hal.archives-ouvertes.fr/hal-01828935 Submitted on 19 May 2021 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Geophysical Research Letters RESEARCH LETTER Along-Axis Variations of Rift Width in a Coupled 10.1029/2018GL077276 Lithosphere-Mantle System, Application Key Points: to East Africa • Impingement of a mantle plume under a lithosphere subjected to Alexander Koptev1,2 , Eric Calais3 , Evgueni Burov1,4, Sylvie Leroy1 , and Taras Gerya5 tension focuses brittle strain in the crust 1CNRS, Institut des Sciences de la Terre de -
Cartography and the Conception, Conquest and Control of Eastern Africa, 1844-1914
Delineating Dominion: Cartography and the Conception, Conquest and Control of Eastern Africa, 1844-1914 DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University By Robert H. Clemm Graduate Program in History The Ohio State University 2012 Dissertation Committee: John F. Guilmartin, Advisor Alan Beyerchen Ousman Kobo Copyright by Robert H Clemm 2012 Abstract This dissertation documents the ways in which cartography was used during the Scramble for Africa to conceptualize, conquer and administer newly-won European colonies. By comparing the actions of two colonial powers, Germany and Britain, this study exposes how cartography was a constant in the colonial process. Using a three-tiered model of “gazes” (Discoverer, Despot, and Developer) maps are analyzed to show both the different purposes they were used for as well as the common appropriative power of the map. In doing so this study traces how cartography facilitated the colonial process of empire building from the beginnings of exploration to the administration of the colonies of German and British East Africa. During the period of exploration maps served to make the territory of Africa, previously unknown, legible to European audiences. Under the gaze of the Despot the map was used to legitimize the conquest of territory and add a permanence to the European colonies. Lastly, maps aided the capitalist development of the colonies as they were harnessed to make the land, and people, “useful.” Of special highlight is the ways in which maps were used in a similar manner by both private and state entities, suggesting a common understanding of the power of the map. -
General Atmospheric Circulation of the Tropics
General Atmospheric Circulation of the Tropics By Herbert Riehl Department of Atmospheric Science Colorado State University Fort Collins, Colorado CURRENT PROBLEMS IN RESEi\RCII The General Atmospheric Circulation of the Tropics by Herbert Riehl Colorado State University In science. ,ve are always interested in a well-ordered simple package whenever such a package appears to be in the offing. There has been widespread belief that the general circulation of the tropics meets these requirements. The weather observations which have been gathered in increasing volume in the upper air over the tropics during the last 15 years" ho\vever, have thrown doubt on the validity of such a simple view. They appear to call for a more complex ap proach to an ultimate understanding of the tropical atmospheric ma chineryand of the interaction between tropical and temperate latitudes. The question no\v is: must we really accept an increased order of difficulty, or can the evidence of the new observations be reconciled with the older approach? If so, chances at arriving at a definite solu tion of the tropical general circulation problem within the next decade would be greatly enhanced.. In one respect the story has not changed; the tropics are a heat source for the atmosphere of higher latitudes. This fact, in broad terms. has been appreciated for centuries. Further, circumnaviga tion of the oceans by sailing vessels led to recognition of a second fact; the tropics also are the source of momentum for the westerly winds prevalent especially in temperate latitudes. Essentially half. of the globe has winds from east at the surface (fig. -
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. -
Severe Weather Forecasting Tip Sheet: WFO Louisville
Severe Weather Forecasting Tip Sheet: WFO Louisville Vertical Wind Shear & SRH Tornadic Supercells 0-6 km bulk shear > 40 kts – supercells Unstable warm sector air mass, with well-defined warm and cold fronts (i.e., strong extratropical cyclone) 0-6 km bulk shear 20-35 kts – organized multicells Strong mid and upper-level jet observed to dive southward into upper-level shortwave trough, then 0-6 km bulk shear < 10-20 kts – disorganized multicells rapidly exit the trough and cross into the warm sector air mass. 0-8 km bulk shear > 52 kts – long-lived supercells Pronounced upper-level divergence occurs on the nose and exit region of the jet. 0-3 km bulk shear > 30-40 kts – bowing thunderstorms A low-level jet forms in response to upper-level jet, which increases northward flux of moisture. SRH Intense northwest-southwest upper-level flow/strong southerly low-level flow creates a wind profile which 0-3 km SRH > 150 m2 s-2 = updraft rotation becomes more likely 2 -2 is very conducive for supercell development. Storms often exhibit rapid development along cold front, 0-3 km SRH > 300-400 m s = rotating updrafts and supercell development likely dryline, or pre-frontal convergence axis, and then move east into warm sector. BOTH 2 -2 Most intense tornadic supercells often occur in close proximity to where upper-level jet intersects low- 0-6 km shear < 35 kts with 0-3 km SRH > 150 m s – brief rotation but not persistent level jet, although tornadic supercells can occur north and south of upper jet as well. -
Severe Thunderstorm Safety
Severe Thunderstorm Safety Thunderstorms are dangerous because they include lightning, high winds, and heavy rain that can cause flash floods. Remember, it is a severe thunderstorm that produces a tornado. By definition, a thunderstorm is a rain shower that contains lightning. A typical storm is usually 15 miles in diameter lasting an average of 30 to 60 minutes. Every thunderstorm produces lightning, which usually kills more people each year than tornadoes. A severe thunderstorm is a thunderstorm that contains large hail, 1 inch in diameter or larger, and/or damaging straight-line winds of 58 mph or greater (50 nautical mph). Rain cooled air descending from a severe thunderstorms can move at speeds in excess of 100 mph. This is what is called “straight-line” wind gusts. There were 12 injuries from thunderstorm wind gusts in Missouri in 2014, with only 5 injuries from tornadoes. A downburst is a sudden out-rush of this wind. Strong downbursts can produce extensive damage which is often similar to damage produced by a small tornado. A downburst can easily overturn a mobile home, tear roofs off houses and topple trees. Severe thunderstorms can produce hail the size of a quarter (1 inch) or larger. Quarter- size hail can cause significant damage to cars, roofs, and can break windows. Softball- size hail can fall at speeds faster than 100 mph. Thunderstorm Safety Avoid traveling in a severe thunderstorm – either pull over or delay your travel plans. When a severe thunderstorm threatens, follow the same safety rules you do if a tornado threatens. Go to a basement if available. -
1 the East African Rift System: Tectonics, Climate and Biodiversity
The East African Rift System: Tectonics, climate and biodiversity Uwe Ring1*, Christian Albrecht2,3, Friedemann Schrenk4 1Institutionen för geologiska vetenskaper, Stockholms universitet, 10691 Stockholm, Sweden 2Department of Animal Ecology and Systematics, Justus Liebig University, Giessen, 35393 Giessen, Germany 3Department of Biology, Mbarara University of Science and Technology, Mbarara, Uganda 4Senckenberg Research Institute and Institute for Ecology, Evolution and Diversity, Goethe University, 60323 Frankfurt, Germany Author for correspondence (*): [email protected] Abstract The East African Rift System (EARS) is one of the most prominent rift systems on Earth and transects the high-elevation East African Plateau. The EARS is famous for its tectonics and geology and has also been suggested to be the ‘cradle of mankind’ making it a natural laboratory for interdisciplinary research straddling the Earth and life sciences. Rifting commenced as a result of mantle plume activity under East Africa. Two distinct rift branches are observed: an older, volcanically active Eastern Branch and a younger, much less volcanic Western Branch. The Eastern Branch is generally characterized by high elevation, whereas the Western Branch comprises a number of deep rift lakes (e.g. Lake Tanganyika, Lake Malaŵi). The onset of topographic uplift in the EARS is poorly dated but has preceded graben development, which commenced at ~24 Ma in the Ethiopian Rift, at ~12 Ma in Kenya, and at ~10 Ma in the Western Branch. Pronounced uplift of the East African Plateau since ~10 Ma might be connected to climate change in East Africa and floral and faunal— including human—evolution. But linking global climate changes to biodiversity in East Africa is difficult as long-term global climate records are from marine cores off the African coast, while faunal and floral evidence from the late Miocene onwards comes from local rift valley sediments. -
Thunderstorm Predictors and Their Forecast Skill for the Netherlands
Atmospheric Research 67–68 (2003) 273–299 www.elsevier.com/locate/atmos Thunderstorm predictors and their forecast skill for the Netherlands Alwin J. Haklander, Aarnout Van Delden* Institute for Marine and Atmospheric Sciences, Utrecht University, Princetonplein 5, 3584 CC Utrecht, The Netherlands Accepted 28 March 2003 Abstract Thirty-two different thunderstorm predictors, derived from rawinsonde observations, have been evaluated specifically for the Netherlands. For each of the 32 thunderstorm predictors, forecast skill as a function of the chosen threshold was determined, based on at least 10280 six-hourly rawinsonde observations at De Bilt. Thunderstorm activity was monitored by the Arrival Time Difference (ATD) lightning detection and location system from the UK Met Office. Confidence was gained in the ATD data by comparing them with hourly surface observations (thunder heard) for 4015 six-hour time intervals and six different detection radii around De Bilt. As an aside, we found that a detection radius of 20 km (the distance up to which thunder can usually be heard) yielded an optimum in the correlation between the observation and the detection of lightning activity. The dichotomous predictand was chosen to be any detected lightning activity within 100 km from De Bilt during the 6 h following a rawinsonde observation. According to the comparison of ATD data with present weather data, 95.5% of the observed thunderstorms at De Bilt were also detected within 100 km. By using verification parameters such as the True Skill Statistic (TSS) and the Heidke Skill Score (Heidke), optimal thresholds and relative forecast skill for all thunderstorm predictors have been evaluated. -
Extreme Precipitation in the Tropics Is Closely Associated with Long-Lived Convective Systems ✉ Rémy Roca 1 & Thomas Fiolleau 1
ARTICLE https://doi.org/10.1038/s43247-020-00015-4 OPEN Extreme precipitation in the tropics is closely associated with long-lived convective systems ✉ Rémy Roca 1 & Thomas Fiolleau 1 Water and energy cycles are linked to global warming through the water vapor feedback and heavy precipitation events are expected to intensify as the climate warms. For the mid- latitudes, extreme precipitation theory has been successful in explaining the observations, 1234567890():,; however, studies of responses in the tropics have diverged. Here we present an analysis of satellite-derived observations of daily accumulated precipitation and of the characteristics of convective systems throughout the tropics to investigate the relationship between the organization of mesoscale convective systems and extreme precipitation in the tropics. We find that 40% of the days with more than 250 mm precipitation over land are associated with convective systems that last more than 24 hours, although those systems only represent 5% of mesoscale convective systems overall. We conclude that long-lived mesoscale convective systems that are well organized contribute disproportionally to extreme tropical precipitation. 1 Laboratoire d’Études en Géophysique et Océanographie Spatiales (Université de Toulouse III, CNRS, CNES, IRD), Toulouse, France. ✉ email: [email protected] COMMUNICATIONS EARTH & ENVIRONMENT | (2020) 1:18 | https://doi.org/10.1038/s43247-020-00015-4 | www.nature.com/commsenv 1 ARTICLE COMMUNICATIONS EARTH & ENVIRONMENT | https://doi.org/10.1038/s43247-020-00015-4 ater and energy cycles are intimately linked to global The characteristics of extreme precipitating storms in the tro- Wwarming through the water vapor feedback1. Specifi- pics remain mostly qualitative, lacking in key aspects of the life cally, as temperature increases, the concentration of cycle of organized convection.