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Imagine2014 8B3 02 Gehrke
Loss Adjustment via Unmanned Aerial Systems (UAS) – Experiences and Challenges for Crop Insurance Thomas Gehrke, Regional Director Berlin, Resp. for International Affairs Loss Adjustment via UAS - Experiences and 20.10.2014 1 Challenges for Crop Insurance Structure 1. Introduction – Demo 2. Vereinigte Hagel – Market leader in Europe 3. Precision Agriculture – UAS 4. Crop insurance – Loss adjustment via UAS 5. Challenges and Conclusion Loss Adjustment via UAS - Experiences and Challenges for Crop Insurance 20.10.2014 2 Introduction – Demo Short film (not in pdf-file) Loss Adjustment via UAS - Experiences and Challenges for Crop Insurance 20.10.2014 3 Structure 1. Introduction – Demo 2. Vereinigte Hagel – Market leader in Europe 3. Precision Agriculture – UAS 4. Crop insurance – Loss adjustment via UAS 5. Challenges and Conclusion Loss Adjustment via UAS - Experiences and Challenges for Crop Insurance 20.10.2014 4 190 years of experience Secufarm® 1 Hail * Loss Adjustment via UAS - Experiences and Challenges for Crop Insurance 20.10.2014 5 2013-05-09, Hail – winter barley Loss Adjustment via UAS - Experiences and Challenges for Crop Insurance 20.10.2014 6 … and 4 weeks later Loss Adjustment via UAS - Experiences and Challenges for Crop Insurance 20.10.2014 7 Our Line of MPCI* Products PROFESSIONAL RISK MANAGEMENT is crucial part of modern agriculture. With Secufarm® products, farmers can decide individually which agricultural Secufarm® 6 crops they would like to insure against ® Fire & Drought which risks. Secufarm 4 Frost Secufarm® 3 Storm & Intense Rain Secufarm® 1 certain crop types are eligible Hail only for Secufarm 1 * MPCI: Multi Peril Crop Insurance Loss Adjustment via UAS - Experiences and Challenges for Crop Insurance 20.10.2014 8 Insurable Damages and their Causes Hail Storm Frost WEATHER RISKS are increasing further. -
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. -
Dock and Crop Images
orders: [email protected] (un)subscribe: [email protected] Current Availability for September 25, 2021 Dock and Crop images Click any thumbnail below for the slideshow of what we shipped this past week: CYCS ARE RED HOT GIANT GLOSSY LEAVES BLUE MOONSCAPE SUCCULENT BLUE LEAVES SUCCULENT ORANGE LEAVES SPECKLED LEAVES CYCS ARE RED HOT RED SUNSETSCAPE Jeff's updates - 9/16 dedicated this week's favorites Chimi's favorite climbing structure 4FL = 4" pot, 15 per flat 10H = 10" hanging basket n = new to the list ys = young stock 6FL = 6" pot, 6 per flat 10DP = 10" Deco Pot, round b&b = bud and bloom few = grab 'em! QT= quart pot, 12 or 16 per flat nb = no bloom * = nice ** = very nice Quarts - 12 per flat, Four Inch - 15 per flat, no split flats, all prices NET code size name comments comments 19406 4FL Acalypha wilkesiana 'Bronze Pink' ** Copper Plant-colorful lvs 12210 QT Acorus gramineus 'Ogon' ** lvs striped creamy yellow 19069 4FL Actiniopteris australis ** Eyelash Fern, Ray Fern 17748 4FL Adiantum hispidulum ** Rosy Maidenhair 17002 4FL Adiantum raddianum 'Microphyllum' ** extremely tiny leaflets 21496 4FL Adromischus filicaulis (cristatus?) ** Crinkle Leaf 16514 4FL Aeonium 'Kiwi' ** tricolor leaves 13632 QT Ajuga 'Catlin's Giant' ** huge lvs, purple fls 13279 QT Ajuga pyramidalis 'Metallica Crispa' ** crinkled leaf 17560 4FL Aloe vera * Healing Aloe, a must-have 13232 QT Anthericum sanderii 'Variegated' *b&b grassy perennial 13227 QT Asparagus densiflorus 'Meyer's' ** Foxtail Fern 19161 4FL Asplenium 'Austral Gem' -
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. -
How Do Heat Waves, Cold Waves, Droughts, Hail and Tornadoes Affect US Agriculture? Southern Great Plains (Better Known As the Dust Bowl)
Research Papers Issue RP0271 How do heat waves, cold waves, December 2015 droughts, hail and tornadoes affect ECIP – Economic analysis of Climate US agriculture? Impacts and Policy Division By Emanuele Massetti SUMMARY We estimate the impact of extreme events on corn and Georgia Institute of Technology, soybeans yields, and on agricultural land values in the Eastern United CESIfo and States. We find the most harmful event is a severe drought but that cold Fondazione CMCC – Centro waves, heat waves, and storms all reduce both corn and soybean yields. Euro -Mediterraneo sui Over 80% of the damage from extreme events is caused by droughts and Cambiamenti Climatici cold waves with heat waves causing only 6% of the damage. Including FEEM – Fondazione Eni Enrico Mattei extreme events in a panel model of weather alters how temperature emanuele.massetti@ affects yields, making cold temperature more harmful and hot pubpolicy.gatech.edu temperatures less harmful. Extreme events have no effect on farmland values probably because American farmers are buffered from extreme events by subsidized public crop insurance. Robert Mendelsohn Yale University [email protected] Keywords Climate change, agriculture, extreme events, heat waves, droughts. JEL codes: Q1, Q54 This report represents the Deliverable P152 developed within the framework of Work Package 7.1.3 of the GEMINA project, funded by the Italian Ministry of Education, University and Research and the Italian Ministry of Environment, Land and Sea. CMCC Research Papers 1. INTRODUCTION 02 There is a large literature that studies how climate and weather affect agricultural productivity using a wide range of methods: large agro-economic models that combine atmospheric science, plant science and agricultural economics (Adams et al. -
Hail TYPICAL DAMAGE Information on Weather-Readyhail Landscapes Information on Weather-Ready Landscapes
Hail TYPICAL DAMAGE Information on weather-readyHail landscapes Information on weather-ready landscapes WHAT IS IT? Type of Damage The frequency of hail in the U.S. is greatest stated here in the Great Plains due to a higher elevation The(closer frequency to freezing of level). hail inHail the forms U.S. when is greatest rain/ice in the Greatparticles Plains are carried due toin the a higher updrafts elevation and downdrafts (closerin thunderstorms to freezing colliding level). and freezing onto one Hailanother, forms while when growing rain/ice into larger particles pieces are of ice. carried in the updrafts and downdrafts in thunderstorms colliding and freezing onto one another, while growing into Type of Damage stated here larger pieces of ice. An average of 70% of hail reports in Nebraska occur from May-July (1955-2015). AnFrom average 2003-2012, there of were70% 7-11 of severe hail hail reportsdays (>1.0” hail in within Nebraska 25 miles of occur from May-Julyany point) per year(1955-2015). in Nebraska. From 2003-2012, there were 7-11 severe hail days (>1.0” hail within 25 miles of any point) Typical Damage: Impact from hailstones can per year in Nebraska. damage leaves, stems and fruit. The size of the hailstone, the amount of hail, time of year, and Number of days per year, within 25 miles of any point from 1986-2015: Number of days per year, within 25 miles of the wind speed plays a big role in the amount of any point from 1986-2015: Typical damageDamage: Impact to from plant hailstones material. -
A Decade Lost I ABOUT the AUTHORS
A DECADE LOST i ABOUT THE AUTHORS The Center for Human Rights and Global Justice (CHRGJ) brings together and expands the rich array of teaching, research, clinical, internship, and publishing activities undertaken within New York University (NYU) School of Law on international human rights issues. Philip Alston and Ryan Goodman are the Center’s Faculty co-Chairs; Smita Narula and Margaret Satterthwaite are Faculty Directors; Jayne Huckerby is Research Director; and Veerle Opgenhaffen is Senior Program Director. The Global Justice Clinic (GJC) at NYU School of Law provides high quality, professional human rights lawyering services to individual clients and non-governmental and inter-governmental human rights organizations, partnering with groups based in the United States and abroad. Working as legal advisers, counsel, co-counsel, or advocacy partners, Clinic students work side-by-side with human rights activists from around the world. The Clinic is directed by Professor Margaret Satterthwaite and in Fall 2010 to Spring 2011 was co-taught with Adjunct Assistant Professor Jayne Huckerby; Diana Limongi is Clinic Administrator. All publications and statements of the CHRGJ can be found at its website: www.chrgj.org. This Report should be cited as: Center for Human Rights and Global Justice, A Decade Lost: Locating Gender in U.S. Counter-Terrorism (New York: NYU School of Law, 2011). © NYU School of Law Center for Human Rights and Global Justice A DECADE LOST 1 ACKNOWLEDGEMENTS The Global Justice Clinic (GJC)/Center for Human Rights and Global Justice (CHRGJ) at New York University (NYU) School of Law acknowledges the following individuals for their contributions in the preparation of this report. -
Hail Size and Melting Considerations in Thunderstorms
Hail Size and Melting Considerations in Thunderstorms NWS Louisville, KY Hail Size and Melting Considerations Two primary factors associated with surface hail size: • Hail generation and initial size in storm • How much melting occurs as hail falls to ground Factors Contributing to Hail Generation and Size in Storm • Storm type: supercells produce larger hail than quasi-linear convective systems (QLCSs) and pulse storms; incipient cells (intense updraft) produce larger hail than after cells congeal into a mesoscale convective system (MCS) • Storm tilt: updraft/downdraft separation promotes hail growth • Updraft strength: increases hail generation and residence time in storm • Dry air aloft (~800-500): leads to evaporative cooling which promotes hail growth and size • Steep mid-level lapse rates: suggests presence of mid-level cool/dry air; promotes strong updraft • Echo tops: taller storms can tap colder air aloft (high refl above -20° C levels) and increase hail residence time in cloud • Cell/boundary mergers: promotes stronger updraft and better chance for hail formation • Values of WBZ height: hail is most favorable with height of 7-12 kft; less favorable if < 6 kft (air mass too cool, although small hail/graupel likely from low-top storms) and if >> 12 kft (melting) The size of hail at surface can’t be determined from looking at reflectivity values in a storm alone Factors Contributing to Hail Size at Surface • Large stones: better chance to reach ground than small stones which melt faster on their descent • Stones melt faster in wet environment than in dry (RH has strong effect); dry air in ~800-500 mb layer is very important to produce evaporative cooling and limit hail melting during descent (why stones are smaller or non-existent during MCSs due to saturated environment – and weaker updraft) • Hail falling within rain melts at a much greater rate than hail falling separate from rain (especially for small hail) • Vertical wind shear is critical in surface hail size to separate the updraft and downdraft and limit duration hail falls in heavy rain. -
Scavenger Hunt: Learn All About the Weather!
Scavenger Hunt: Learn All About the Weather! Hello, young scientists! Your task is to go on a scavenger hunt to learn all about weather–from snowflakes to firestorms, to hurricanes and many things in between! In this activity, you will adventure between articles on the NOAA SciJinks website, learning all about Earth’s many weather phenomena and gathering the missing words or phrases needed to assemble your secret word. All About Precipitation! When you see rain or snow fall from above, you are watching precipitation in action! Follow this link to learn all about precipitation and to find the missing word: Go to: What Is Precipitation? Answer 1: When gas cools and turns to liquid water or ice, it is called _______. All About Snowflakes! Snow is not simply a frozen droplet of water falling from a cloud. What makes a snowflake different is that it forms slowly, and that it grows in the cloud. But, how exactly does a snowflake form? Learn all about it in the following article and fill in the missing word below! Go to: How Do Snowflakes Form? Answer 2: Snowflakes form when water vapor travels through the air and condenses on a _____. All About Tornadoes! A strong tornado’s winds can pick up massive objects like trucks and drop them many miles away. It is difficult to measure the winds in a tornado directly, though. Because of this, tornadoes are evaluated by the amount of damage they cause. What tool do meteorologists use to measure the intensity of a tornado? Follow the link to find out and fill in the missing word below! Go to: Tornadoes Answer 3: The ______ ______ scale is a tool meteorologists use to measure the intensity of a tornado based on damage. -
Flood ACC Article
Breadth of the Flood Exclusion: A Flood is a Flood, Including Storm Surge TRED R. EYERLY A case involving an Alaska Native Corporation and property damage caused by a hurricane is bound to be of interest. Arctic Slope Regional Corp. v. Affiliated FM Ins. Co. did not disappoint.1 The Arctic Slope Regional Corporation, based in Barrow, Alaska, and one of the thirteen Corporations formed under the Alaska Native Claims Settlement Act of 1971, owned an office and construction yard in Iberia Parish, Louisiana. The property was inundated with three feet of water after Hurricane Rita’s storm surge hit in September 2005. Arctic Slope filed a claim for property damage with Affiliated. The claim was denied and suit was filed. Before the district court, the parties disputed which policy provisions applied to the storm surge related claims. The distinction was critical because the policy covered damage caused by “Wind and/or hail,” but excluded damage caused by flood. The policy defined “Wind and/or hail” as “direct and/or indirect action of wind and all loss or damage resulting there from whether caused by wind, by hail or by any other peril . when water . is carried, blown, driven, or otherwise transported by wind onto or into said location.” “Flood,” on the other hand, was defined as “surface water; tidal or seismic sea wave; rising (including overflowing or breaking of boundaries) of any body of water . all whether driven by wind or not. .”2 1 Arctic Slope argued that, because storm surge is caused by strong onshore winds, coverage was provided under the “Wind and/or hail” definition. -
Mediterranean Firestorm, Are Extreme Wildfires a Specular Aspect of Floods?
Plinius Conference Abstracts Vol. 12, Plinius12-57 12th Plinius Conference on Mediterranean Storms Corfu Island Greece, September 2010 © Author(s) 2010 Mediterranean Firestorm, are extreme wildfires a specular aspect of floods? P. Fiorucci, L. Molini, and A. Parodi CIMA Research Foundation, Italy (paolo.fi[email protected]) Severe weather and rainfall extremes predictors are a long standing issue for risk mitigation and civil protection purposes, analogously this work is focused on finding precursors for extreme wildfires throughout Mediterranean regions. Mediterranean storm are usually related with extreme precipitation and consequent floods. In this paper we propose to consider extreme wildfires in the Mediterranean as a specular aspect of “traditional” Mediterranean storms. Floods are related with soil moisture conditions, vegetation cover and topography but the main driver is represented by extreme precipitation. Rainfall is well evident in its happening. Nevertheless, the necessity of measuring it has become fundamental since the implementation of instruments needed to prevent floods. Wildfires are usually considered as the complex results of several heterogeneous aspects. Many peculiarities make Mediterranean wildfires different from other natural risk, fire ignition, human caused in more than 90% of fire occurrences, being the most evident. Fire spread and fire damages are related with vegetation cover, topography, moisture content and wind conditions but also with the ability to cope with the fire front. In the international literature all these aspects are considered to define tools able to predict and manage wildfire risk. Strong winds and high temperature are often considered as the main drivers in extreme wildfire risk conditions. Strong winds are usually associated also to floods event during Mediterranean storm but in this case it is evident it doesn’t the main driver. -
Cnow: Eldritch Witchery
Advanced Dungeons & Dragons 2nd Edition The Complete Netbook of Witches & Warlocks: Eldritch Witchery Supplement I 1 The Complete Netbook of Witches and Warlocks: Eldritch Witchery Forward Welcome to the first supplement to the Complete Netbook of Witches and Warlocks. This supplement will contain new ideas, revised old ones, and some extra things I thought you might enjoy. It took me close to 10 years to start and then finish my first netbook. Hopefully this one will not take as long. To begin with, none of the information in this volume is necessary or required to continue to play your witch characters. There is some additional information and errata, but most will be new information. Also there will be some information that is not necessarily witch related, but designed to add extra background to the worlds the witch is likely to play in. This supplement pays homage to the Original Dungeons and Dragons game supplement Eldritch Wizardry. That supplement introduced demons, psionics, artifacts and druids to the D&D game for the first time. It also was the first D&D product that came close to being banned. The controversial cover art, a nude blond woman bound up for a sacrifice, made this a rare item to find. Eldritch Witchery, which conversely has no cover art, will not be as rare or as collectable, but hopefully it will provide you with as much fun as the first provided me. Copies of this supplement, the original Complete Netbook of Witches and Warlocks, as well as any future supplements can be found at my website at http://www.rpghost.com/WebWarlock or http://go.to/WebWarlock.