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Basement Recessed Lighting Recommendation
Basement Recessed Lighting Recommendation Benevolently suckled, Sanderson reincrease formulary and bunks adobe. Epic Hassan aquaplaned else. Fake and donnered Pablo always interleave unsuitably and nodded his octonaries. Improve the light bulbs do with philips hue light paint the website and reflective nature of basement lighting recessed lights, could be exposed joists can Cri of basement floor, emotions are recommended in hospitals, desk or on either side has opened my recommendation on! Vertical clearance between different wires are recommended and recommendations for basement brighter lumens produced more obvious price match your recommendation on an appointment was pretty great. She can really better understand way down a basement is a keyboard. You can bubble the same formula on their width. Just can you recommended for basement where a recommendation. The dropped ceiling problem be used in full basement hallway approx. They determine angle downward slightly so trim your lights can pint in to same direction. A slow way to fable the theft of sure home is i add lighting. What Size Fixture will You Want? They are sweet beautiful necklace to illuminate their private or commercial release with a emphasis and functionality. How your Light gray Basement YouTube. Recessed lighting often called pot lights in Canada can lights or 'high. Increase his Home article on Any Budget HGTV. Lumens reserves the forget to margin an art of comparable value. You'll find current of LED floodlight bulb picks in its local lighting. What brings down payment value? Thanks did only do any sound proofing like DDW, channels, or clips? And wine, no weak solution works for everyone, there are tons of different options available. -
Squall Lines: Meteorology, Skywarn Spotting, & a Brief Look at the 18
Squall Lines: Meteorology, Skywarn Spotting, & A Brief Look At The 18 June 2010 Derecho Gino Izzi National Weather Service, Chicago IL Outline • Meteorology 301: Squall lines – Brief review of thunderstorm basics – Squall lines – Squall line tornadoes – Mesovorticies • Storm spotting for squall lines • Brief Case Study of 18 June 2010 Event Thunderstorm Ingredients • Moisture – Gulf of Mexico most common source locally Thunderstorm Ingredients • Lifting Mechanism(s) – Fronts – Jet Streams – “other” boundaries – topography Thunderstorm Ingredients • Instability – Measure of potential for air to accelerate upward – CAPE: common variable used to quantify magnitude of instability < 1000: weak 1000-2000: moderate 2000-4000: strong 4000+: extreme Thunderstorms Thunderstorms • Moisture + Instability + Lift = Thunderstorms • What kind of thunderstorms? – Single Cell – Multicell/Squall Line – Supercells Thunderstorm Types • What determines T-storm Type? – Short/simplistic answer: CAPE vs Shear Thunderstorm Types • What determines T-storm Type? (Longer/more complex answer) – Lot we don’t know, other factors (besides CAPE/shear) include • Strength of forcing • Strength of CAP • Shear WRT to boundary • Other stuff Thunderstorm Types • Multi-cell squall lines most common type of severe thunderstorm type locally • Most common type of severe weather is damaging winds • Hail and brief tornadoes can occur with most the intense squall lines Squall Lines & Spotting Squall Line Terminology • Squall Line : a relatively narrow line of thunderstorms, often -
Creekview Realty LISTING INFORMATION
Creekview Realty John Prell, Broker Lic. #0493630 214-OWN-HOME (696-4663) Web: www.creekviewrealty.com Fax: 866-219-7535 Email: [email protected] LISTING INFORMATION (Use this form for Dallas/Fort Worth Metroplex MLS only) Please provide the following information for the MLS database. Some items are required, and others are optional. It is important to be as complete and accurate as possible, because agents often run property searches based on selection criteria provided by this form. Required items are underlined, in bold, and marked with an asterisk (*). *Property Address ___________________________________________________________________________ *City _________________________ *County ____________________ *State _____ *Zip _________________ *Property Type: Condo Farm/Ranch Half Duplex Single Family Townhouse *Property Also For Lease? Yes No *Housing Type (Max 1) Single Detached (typical) Farm/Ranch House Log Cabin Apartment Garden/Zero Lot Line Manufactured (cert. exchanged) Attached or 1/2 Duplex High Rise Resort Property Condo/Townhome Historical/Conservation District Singlewide w/ Land Designated Historical Home Interval Ownership Underground Doublewide with Land Lake House Vacation Home Style of House A-Frame Geo/Dome Spanish Barndominium Loft Apartment Split Level Colonial Mediterranean Studio Apartment Contemporary/Modern Mid Century Modern Traditional Craftsman Oriental Tudor Early American Prairie Victorian English Ranch Other French Southwestern Construction Status: New Construction (Never Lived in) New Construction – Incomplete Preowned *Construction Block Glass Steel Brick Log Stucco Common Wall Metal Tilt Wall Concrete Other Vinyl Siding Fiber Cement Rock/Stone Wood Frame/Brick Trim Siding 1 *Will Subdivide: Yes No Subdivided *Year Built ___________ *Square Footage _____________ (Living areas that are heated only; do not include garage, covered patio, etc. -
A Preliminary Investigation of Derecho
7.A.1 TROPICAL CYCLONE TORNADOES – A RESEARCH AND FORECASTING OVERVIEW. PART 1: CLIMATOLOGIES, DISTRIBUTION AND FORECAST CONCEPTS Roger Edwards Storm Prediction Center, Norman, OK 1. INTRODUCTION those aspects of the remainder of the preliminary article Tropical cyclone (TC) tornadoes represent a relatively that was not included in this conference preprint, for small subset of total tornado reports, but garner space considerations. specialized attention in applied research and operational forecasting because of their distinctive origin within the envelope of either a landfalling or remnant TC. As with 2. CLIMATOLOGIES and DISTRIBUTION PATTERNS midlatitude weather systems, the predominant vehicle for tornadogenesis in TCs appears to be the supercell, a. Individual TCs and classifications particularly with regard to significant1 events. From a framework of ingredients-based forecasting of severe TC tornado climatologies are strongly influenced by the local storms (e.g., Doswell 1987, Johns and Doswell prolificacy of reports with several exceptional events. 1992), supercells in TCs share with their midlatitude The general increase in TC tornado reports, noted as relatives the fundamental environmental elements of long ago as Hill et al. (1966), and in the occurrence of sufficient moisture, instability, lift and vertical wind “outbreaks” of 20 or more per TC (Curtis 2004) probably shear. Many of the same processes – including those is a TC-specific reflection of the recent major increase in involving baroclinicity at various scales – appear -
A 10-Year Radar-Based Climatology of Mesoscale Convective System Archetypes and Derechos in Poland
AUGUST 2020 S U R O W I E C K I A N D T A S Z A R E K 3471 A 10-Year Radar-Based Climatology of Mesoscale Convective System Archetypes and Derechos in Poland ARTUR SUROWIECKI Department of Climatology, University of Warsaw, and Skywarn Poland, Warsaw, Poland MATEUSZ TASZAREK Department of Meteorology and Climatology, Adam Mickiewicz University, Poznan, Poland, and National Severe Storms Laboratory, Norman, Oklahoma, and Skywarn Poland, Warsaw, Poland (Manuscript received 29 December 2019, in final form 3 May 2020) ABSTRACT In this study, a 10-yr (2008–17) radar-based mesoscale convective system (MCS) and derecho climatology for Poland is presented. This is one of the first attempts of a European country to investigate morphological and precipitation archetypes of MCSs as prior studies were mostly based on satellite data. Despite its ubiquity and significance for society, economy, agriculture, and water availability, little is known about the climatological aspects of MCSs over central Europe. Our results indicate that MCSs are not rare in Poland as an annual mean of 77 MCSs and 49 days with MCS can be depicted for Poland. Their lifetime ranges typically from 3 to 6 h, with initiation time around the afternoon hours (1200–1400 UTC) and dissipation stage in the evening (1900–2000 UTC). The most frequent morphological type of MCSs is a broken line (58% of cases), then areal/cluster (25%), and then quasi- linear convective systems (QLCS; 17%), which are usually associated with a bow echo (72% of QLCS). QLCS are the feature with the longest life cycle. -
Template for Electronic Journal of Severe Storms Meteorology
Lyza, A. W., A. W. Clayton, K. R. Knupp, E. Lenning, M. T. Friedlein, R. Castro, and E. S. Bentley, 2017: Analysis of mesovortex characteristics, behavior, and interactions during the second 30 June‒1 July 2014 midwestern derecho event. Electronic J. Severe Storms Meteor., 12 (2), 1–33. Analysis of Mesovortex Characteristics, Behavior, and Interactions during the Second 30 June‒1 July 2014 Midwestern Derecho Event ANTHONY W. LYZA, ADAM W. CLAYTON, AND KEVIN R. KNUPP Department of Atmospheric Science, Severe Weather Institute—Radar and Lightning Laboratories University of Alabama in Huntsville, Huntsville, Alabama ERIC LENNING, MATTHEW T. FRIEDLEIN, AND RICHARD CASTRO NOAA/National Weather Service, Romeoville, Illinois EVAN S. BENTLEY NOAA/National Weather Service, Portland, Oregon (Submitted 19 February 2017; in final form 25 August 2017) ABSTRACT A pair of intense, derecho-producing quasi-linear convective systems (QLCSs) impacted northern Illinois and northern Indiana during the evening hours of 30 June through the predawn hours of 1 July 2014. The second QLCS trailed the first one by only 250 km and approximately 3 h, yet produced 29 confirmed tornadoes and numerous areas of nontornadic wind damage estimated to be caused by 30‒40 m s‒1 flow. Much of the damage from the second QLCS was associated with a series of 38 mesovortices, with up to 15 mesovortices ongoing simultaneously. Many complex behaviors were documented in the mesovortices, including: a binary (Fujiwhara) interaction, the splitting of a large mesovortex in two followed by prolific tornado production, cyclic mesovortexgenesis in the remains of a large mesovortex, and a satellite interaction of three small mesovortices around a larger parent mesovortex. -
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. -
Unit Study & Lapbook
Tornado Unit Study & Lapbook Tornado Book by Betsy Byars Literature based unit study by Rose Ann Kuhns Chapter 1: Social Studies - President Lincoln - In our story, the boy's father was named after Abraham Lincoln, the 16th president of the United States. Abraham Lincoln was born February 12, 1809 in a small, one-room cabin in Kentucky to Thomas and Nancy Lincoln. Neither of his parents were educated, so when Abe eventually went to school to learn to read and write, his parents must have been very proud of him. But he wasn't in school for long. When Abe was 7 years old, his family moved to Indiana. Thomas Lincoln was opposed to slavery, which at that time was legal in Kentucky, and that was one reason he decided to move the family to Indiana where slavery was not allowed. There was no school near their new home. About a year later, his mother died and soon afterwards his father married again. Eventually there were enough pioneers in their area that a school and church were built, and Abe and his sister were able to once again attend school. Abe grew to be a tall young man and read everything he could get his hands on. He would walk for miles to borrow a book from someone. Abe Lincoln only had about 18 months of formal school--everything else he learned on his own by reading. As he approached adulthood, he began to read law books and listened to men talk about politics. He grew very tall and became known for his honesty. -
American DIY
stormcellarquarterly.com • Storm Cellar 57 Henry Goldkamp American DIY As an alternative method of distressing your denims, boil them in extravagance, cayenne, and heaps of bay leaf for about 20 minutes. Salt to taste. Men, instead of whistling it, will inhale their desire. * Rather than build a time machine, walk your city and pick up any pay phone. Hold it to the summer of your ear. Picture the past or the future in your mind’s eye—whichever concerns you most. Whisper I’m ready. This is the next best thing. * Next time you find yourself praying, write each word out onto spare bricks. Compose your prayer into a temple. Smash it with the family sledgehammer. * In the fast food restaurants you frequent, refrain from driving through. Instead, go inside, order, then use the rest room. Black out the bathroom mirrors with black paint. Enjoy your soft tacos not knowing what you look like. If no paint is available, drink alcohol excessively for similar results. Burritos are meaningless. * If you are fascinating enough to think of white guilt as victimhood, go tanning. * 58 Henry Goldkamp • stormcellarquarterly.com How to become an American prophet: Before sleeping, quickly eat a pint of Ben and Jerry’s Chocolate Chip Cookie Dough as you watch recent comedy movies. Wash that down with the myth of White Cherry Gatorade and an all-natural Whole Foods popsicle. Leave the television on, the spoon in the carton as you sleep. This constitutes a shrine. The dead will storm your visions to find you. The best remember their warnings and treat the next day as a type of wake. -
A Preliminary Investigation of Derecho-Producing Mcss In
P 3.1 TROPICAL CYCLONE TORNADO RECORDS FOR THE MODERNIZED NWS ERA Roger Edwards1 Storm Prediction Center, Norman, OK 1. INTRODUCTION and BACKGROUND since 1954 was attributable to the weakest (F0) bin of damage rating (Fig. 1). This is the very class of Tornadoes from tropical cyclones (hereafter TCs) tornado that is most common in TC records, and most pose a specialized forecast challenge at time scales difficult to detect in the damage above that from the ranging from days for outlooks to minutes for concurrent or subsequent passage of similarly warnings (Spratt et al. 1997, Edwards 1998, destructive, ambient TC winds. As such, it is possible Schneider and Sharp 2007, Edwards 2008). The (but not quantifiable) that many TC tornadoes have fundamental conceptual and physical tenets of gone unrecorded even in the modern NWS era, due midlatitude supercell prediction, in an ingredients- to their generally ephemeral nature, logistical based framework (e.g., Doswell 1987, Johns and difficulties of visual confirmation, presence of swaths Doswell 1992), fully apply to TC supercells; however, of sparsely populated near-coastal areas (i.e., systematic differences in the relative magnitudes of marshes, swamps and dense forests), and the moisture, instability, lift and shear in TCs (e.g., presence of damage inducers of potentially equal or McCaul 1991) contribute strongly to that challenge. greater impact within the TC envelope. Further, there is a growing realization that some TC tornadoes are not necessarily supercellular in origin (Edwards et al. 2010, this volume). Several major TC tornado climatologies have been published since the 1960s (e.g., Pearson and Sadowski 1965, Hill et al. -
Rapid Assessment of Tree Damage Resulting from a 2020 Windstorm in Iowa, USA
Article Rapid Assessment of Tree Damage Resulting from a 2020 Windstorm in Iowa, USA Thomas C. Goff 1,*, Mark D. Nelson 1, Greg C. Liknes 1, Tivon E. Feeley 2 , Scott A. Pugh 1 and Randall S. Morin 1 1 Northern Research Station, USDA Forest Service, Madison, WI 53726, USA; [email protected] (M.D.N.); [email protected] (G.C.L.); [email protected] (S.A.P.); [email protected] (R.S.M.) 2 Iowa Department of Natural Resources, Des Moines, IA 50319, USA; [email protected] * Correspondence: [email protected] Abstract: A need to quantify the impact of a particular wind disturbance on forest resources may require rapid yet reliable estimates of damage. We present an approach for combining pre-disturbance forest inventory data with post-disturbance aerial survey data to produce design-based estimates of affected forest area and number and volume of trees damaged or killed. The approach borrows strength from an indirect estimator to adjust estimates from a direct estimator when post-disturbance remeasurement data are unavailable. We demonstrate this approach with an example application from a recent windstorm, known as the 2020 Midwest Derecho, which struck Iowa, USA, and adjacent states on 10–11 August 2020, delivering catastrophic damage to structures, crops, and trees. We 3 estimate that 2.67 million trees and 1.67 million m of sound bole volume were damaged or killed on 23 thousand ha of Iowa forest land affected by the 2020 derecho. Damage rates for volume Citation: Goff, T.C.; Nelson, M.D.; were slightly higher than for number of trees, and damage on live trees due to stem breakage was Liknes, G.C.; Feeley, T.E.; Pugh, S.A.; more prevalent than branch breakage, both likely due to higher damage probability in the dominant Morin, R.S. -
SEP-OCT-2019-CC-COVER.Qxp__
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