Product/Service Description Document Polygon-Based Dust Storm Warning and Dust Advisory Products
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Technical Report
Establishing a WMO Sand and Dust Storm Warning Advisory and Assessment System Regional Node for West Asia: Current Capabilities and Needs Technical Report For more information, please contact: World Meteorological Organization Research Department Atmospheric Research and Environment Branch 7 bis, avenue de la Paix – P.O. Box 2300 – CH 1211 Geneva 2 – Switzerland Tel.: +41 (0) 22 730 81 11 – Fax: +41 (0) 22 730 81 81 E-mail: [email protected] Website: http://www.wmo.int/pages/prog/arep/wwrp/new/wwrp_new_en.html WMO-No. 1121 Establishing a WMO Sand and Dust Storm Warning Advisory and Assessment System Regional Node for West Asia: Current Capabilities and Needs Technical Report NOVEMBER 2013 Cover photogtraph:Soil Solutions Ltd. © United Nations Environment Programme, 2013 General disclaimers The views expressed in this publication are those of the authors and do not necessarily reflect the views of the United Nations Environment Programme (UNEP). The opinions, figures and estimates set forth in this publication are not the responsibility of the author, and should not necessarily be considered as reflecting the views or carrying the endorsement of the United Nations Environment Programme. The contents of this publication do not necessarily reflect the views or policies of UNEP or the editors, nor are they an official record. The contents of this publication do not necessarily reflect the views or policies of UNEP or contributory organizations. Technical content disclaimers While reasonable efforts have been made to ensure that the contents of this publication are factually correct and properly referenced, UNEP does not accept responsibility for the accuracy or completeness of the contents, and shall not be liable for any loss or damage that may be occasioned directly or indirectly through the use of, or reliance on, the contents of this publication. -
Episodic Dust Events of Utah's Wasatch Front and Adjoining Region
1654 JOURNAL OF APPLIED METEOROLOGY AND CLIMATOLOGY VOLUME 51 Episodic Dust Events of Utah’s Wasatch Front and Adjoining Region W. JAMES STEENBURGH AND JEFFREY D. MASSEY Department of Atmospheric Sciences, University of Utah, Salt Lake City, Utah THOMAS H. PAINTER Jet Propulsion Laboratory, Pasadena, California (Manuscript received 4 January 2012, in final form 4 April 2012) ABSTRACT Episodic dust events cause hazardous air quality along Utah’s Wasatch Front and dust loading of the snowpack in the adjacent Wasatch Mountains. This paper presents a climatology of episodic dust events of the Wasatch Front and adjoining region that is based on surface weather observations from the Salt Lake City International Airport (KSLC), Geostationary Operational Environmental Satellite (GOES) imag- ery, and additional meteorological datasets. Dust events at KSLC—defined as any day [mountain standard time (MST)] with at least one report of a dust storm, blowing dust, and/or dust in suspension with a visi- bility of 10 km or less—average 4.3 per water year (WY: October–September), with considerable in- terannual variability and a general decline in frequency during the 1930–2010 observational record. The distributions of monthly dust-event frequency and total dust flux are bimodal, with primary and secondary maxima in April and September, respectively. Dust reports are most common in the late afternoon and evening. An analysis of the 33 most recent (2001–10 WY) events at KSLC indicates that 11 were associated with airmass convection, 16 were associated with a cold front or baroclinic trough entering Utah from the west or northwest, 4 were associated with a stationaryorslowlymovingfrontorbaroclinictroughwestof Utah, and 2 were associated with other synoptic patterns. -
An American Haboob U.S
S. B. Idso, R. S. Ingram, and J. M. Pritchard an american haboob U.S. Water Conservation Laboratory and National Weather Service, Phoenix, Ariz. 85040 1. Introduction by thunder and/or rain after a time interval varying up One of the world's most awesome displays of blowing to 2 hr. dust and sand is the legendary "haboob" of Khartoum in Satellite photographs have shown that the squall line the Sudan. Raised by strong winds often generated storms that develop south and east of Tucson appear by the outflow of rain-cooled air from a cumulonimbus to originate from large dense masses of clouds over the cloud, the leading edges of these storms take on the Sierra Madre Occidental of northern Sonora, Mexico. appearance of "solid walls" of dust that conform to These cloud masses over Sonora seem to form some the shape of a density current head and rise on the days rather explosively in the deep semi-tropical air average to between 1000 and 2000 meters (Sutton, 1925; mass. During this season of the year, the Bermuda High Lawson, 1971). The average speed of advance of the often extends westward into eastern Arizona, and during Khartoum haboobs is 32 mph, with the greatest speed the afternoon some of the Mexican activity has been seen being about 45 mph (Sutton, 1925). Maximum duration to move northwestward, steered by variations in the approaches 6-1/2 hr with a peak between 30 min and easterly flow (possibly easterly waves) on the bottom side one hour, the average duration being about 3 hr (Free- of the lobe of the Bermuda High. -
National Weather Service Reference Guide
National Weather Service Reference Guide Purpose of this Document he National Weather Service (NWS) provides many products and services which can be T used by other governmental agencies, Tribal Nations, the private sector, the public and the global community. The data and services provided by the NWS are designed to fulfill us- ers’ needs and provide valuable information in the areas of weather, hydrology and climate. In addition, the NWS has numerous partnerships with private and other government entities. These partnerships help facilitate the mission of the NWS, which is to protect life and prop- erty and enhance the national economy. This document is intended to serve as a reference guide and information manual of the products and services provided by the NWS on a na- tional basis. Editor’s note: Throughout this document, the term ―county‖ will be used to represent counties, parishes, and boroughs. Similarly, ―county warning area‖ will be used to represent the area of responsibility of all of- fices. The local forecast office at Buffalo, New York, January, 1899. The local National Weather Service Office in Tallahassee, FL, present day. 2 Table of Contents Click on description to go directly to the page. 1. What is the National Weather Service?…………………….………………………. 5 Mission Statement 6 Organizational Structure 7 County Warning Areas 8 Weather Forecast Office Staff 10 River Forecast Center Staff 13 NWS Directive System 14 2. Non-Routine Products and Services (watch/warning/advisory descriptions)..…….. 15 Convective Weather 16 Tropical Weather 17 Winter Weather 18 Hydrology 19 Coastal Flood 20 Marine Weather 21 Non-Precipitation 23 Fire Weather 24 Other 25 Statements 25 Other Non-Routine Products 26 Extreme Weather Wording 27 Verification and Performance Goals 28 Impact-Based Decision Support Services 30 Requesting a Spot Fire Weather Forecast 33 Hazardous Materials Emergency Support 34 Interactive Warning Team 37 HazCollect 38 Damage Surveys 40 Storm Data 44 Information Requests 46 3. -
DUST DEVIL METEOROLOGY Jack R
NOAA~NWS /1(}q, 3~;).. ~ . NOAA Technicai ·Memoran_dlim Nws·CR-42 U.S. DEPARTMENT OF COMMERCE National Oceanic and Atmospheric Adminlstretian National Weather Service DUST 1DEV-IL... ,. METEOROLOGY.. .. ... .... - 1!. Jack ,R. .Cooley \ i ,. CiHTRAL REGION Kansas City.. Mo. () U. S. DEPARTMENT OF COMMERCE NATIONAL OCEANIC AND ATMOSPHERIC ADMINISTRATION NATIONAL WEATHER SERVICE NOAA Technical Memoran:l.um NWS CR-42 Il.JST DEVIL METEOROLOGY Jack R. Cooley CENTRAL REJJION KANSAS CITY, MISSOORI May 1971 CONTENTS () l. Page No. INTRODUCTION 1 1.1 Some Early Accounts of Dust Devils 1 1.2 Definition 2 1.3 The Atmospheric Circulation Family 2 1.4 Other Similar Small-Scale Circulations 2 1.41 Small Waterspouts 3 l. 42 Whirlies 3 1.43 Fire 1-!hirhdnds 3 1.44 Whirlwinds Associated With Cold Fronts 4 l. 5 Damage Caused by Dust Devils 4 1.51 Dust DeVils Vs. Aircraft Safety 5 2. FORMATION 5 2.1 Optimum Locations (Macro and Micro) 5 2.2 Optimum Time of Occurrence (During Day and Year) 6 2.3 Conditions Favoring Dust Devil Formation 7 2.31 Factors Favoring Steep Lapse Rates Near the Ground 7 A. Large Incident Solar Radiation Angles 7 B. Minimum Cloudiness 7 C. Lmr Humidity 8 D. Dry Barren Soil 8 E. Surface Winds Below a Critical Value 9 2.32 Potential Lapse Rates Near the Ground 9 2.33 Favorable Air Flow 12 2 ,34 Abundant Surface Material 12 2.35 Level Terrain 13 2.4 Triggering Devices 13 2.5 Size and Shape 14. 2.6 Dust Size·and Distribution 14 2.7 Duration 15 2.8 Direction of Rotation 16 2.9 Lateral Speed and Direction of Movement 17 3. -
NWSI 10-1701, “Text Product Formats and Codes,” Dated March 29, 2018
Department of Commerce • National Oceanic & Atmospheric Administration • National Weather Service NATIONAL WEATHER SERVICE INSTRUCTION 10-1701 OCTOBER 29, 2019 Operations and Services Dissemination Services NWSPD 10-17 TEXT PRODUCT FORMATS AND CODES NOTICE: This publication is available at: http://www.nws.noaa.gov/directives/. OPR: DIS (A. Hardy) Certified by: W/DIS (M. Mainelli-McInerny) Type of Issuance: Routine SUMMARY OF REVISIONS: This directive supersedes NWSI 10-1701, “Text Product Formats and Codes,” dated March 29, 2018. Changes were made to reflect the addition of Section 8 – 11 to address actions to take when inadvertent messages are sent by NWS or by a third party. Content changes were made to: 1. Throughout the document, updated titles and sections for formatting, section reference numbers and web links to correct sites. 2. Add Section 8, Recommended Actions to Take Following the Inadvertent NWS Dissemination of Messages by NWS Offices. 3. Add Section 9, Steps to Take After a Correctly-Formatted NWS Message is Incorrectly Disseminated by a Third Party 4. Add Section 10, Steps to Take for Messaging After an Inadvertent Dissemination of Test Alerts by a Third Party 5. Add Section 11, Role of NWS Rapid Response Team 6. Updated Appendix B, Section 2.3 to rewrite message example in mixed case. /signed/ 10/15/19____ Michelle Mainelli-McInerney Date Director, Office of Dissemination NWSI 10-1701 OCTOBER 29, 2019 Text Product Formats and Codes – Table of Contents Page 1. Introduction ............................................................................................................................... 4 1.1 Mission Connection ...........................................................................................................5 1.2 Text Products in Languages Other Than English ............................................................. 5 1.3 Format of Text Examples ..................................................................................................5 2. -
KJAX 2018 Product Criteria.Xlsx
Product Criteria Coastal Products Coastal Flood Statement Used to describe coastal hazards that do not meet advisory, warning or watch criteria such as minor beach erosion & elevated (Action) water levels. Coastal Flood Advisory Highlight minor flooding like tidal overflow that is imminent or possible within 12 Hours& if confidence is high (equal to or greater than 50%), then may extend or set to begin within 24 hrs. Coastal Flood Watch Significant coastal flooding is possible. This includes Moderate and Major flooding in the Advanced Hydrologic Prediction Service (AHPS) product. Coastal Flood Warning Significant coastal flooding is occurring, imminent or highly likely. This includes Moderate and Major flooding in AHPS. High Surf Advisory Breaker heights ≥ 7 Feet Rip Current Statement When a high risk of rip currents is expected Marine Products Small Craft Exercise Caution Winds 15-20 knots and/or seas 6 Feet Small Craft Advisory Winds 20-33 knots and/or seas ≥ 7 Feet Small Craft Advisory (seas only) Winds< 20 knots & seas ≥ 7 Feet (usually with a swell) Gale Watch Wind speed 34-47 knots or frequent gusts 34-47 knots Gale Warning Wind speed 34-47 knots or frequent gusts 34-47 knots Storm Watch Wind speed 48-63 knots or gusts of 48-63 knots Storm Warning Wind speed 48-63 knots or gusts of 48-63 knots Marine Dense Fog Advisory Widespread visibility < 1 nautical mile in fog Marine Dense Smoke Advisory Widespread visibility < 1 nautical mile in smoke Marine Weather Statement Update or cancel at Special Marine Warning (SMW), a statement on non-severe showers & thunderstorms, short-lived wind/sea increase that could be dangerous for small boats, significant conditions prevailing for 2+ Hours that could impact marine operations including: rough seas near inlets/passes, dense fog, low water events, HAZMAT spills, rapidly increasing/decreasing or shifting winds, or details on potential water landings. -
Episodic Dust Events of Utah's Wasatch
1654 JOURNAL OF APPLIED METEOROLOGY AND CLIMATOLOGY VOLUME 51 Episodic Dust Events of Utah’s Wasatch Front and Adjoining Region W. JAMES STEENBURGH AND JEFFREY D. MASSEY Department of Atmospheric Sciences, University of Utah, Salt Lake City, Utah THOMAS H. PAINTER Jet Propulsion Laboratory, Pasadena, California (Manuscript received 4 January 2012, in final form 4 April 2012) ABSTRACT Episodic dust events cause hazardous air quality along Utah’s Wasatch Front and dust loading of the snowpack in the adjacent Wasatch Mountains. This paper presents a climatology of episodic dust events of the Wasatch Front and adjoining region that is based on surface weather observations from the Salt Lake City International Airport (KSLC), Geostationary Operational Environmental Satellite (GOES) imag- ery, and additional meteorological datasets. Dust events at KSLC—defined as any day [mountain standard time (MST)] with at least one report of a dust storm, blowing dust, and/or dust in suspension with a visi- bility of 10 km or less—average 4.3 per water year (WY: October–September), with considerable in- terannual variability and a general decline in frequency during the 1930–2010 observational record. The distributions of monthly dust-event frequency and total dust flux are bimodal, with primary and secondary maxima in April and September, respectively. Dust reports are most common in the late afternoon and evening. An analysis of the 33 most recent (2001–10 WY) events at KSLC indicates that 11 were associated with airmass convection, 16 were associated with a cold front or baroclinic trough entering Utah from the west or northwest, 4 were associated with a stationaryorslowlymovingfrontorbaroclinictroughwestof Utah, and 2 were associated with other synoptic patterns. -
The Footprints of Saharan Air Layer and Lightning on the Formation of Tropical Depressions Over the Eastern Atlantic Ocean
San Jose State University SJSU ScholarWorks Master's Theses Master's Theses and Graduate Research Summer 2014 The Footprints of Saharan Air Layer and Lightning on the Formation of Tropical Depressions over the Eastern Atlantic Ocean Diana Caroly Centeno San Jose State University Follow this and additional works at: https://scholarworks.sjsu.edu/etd_theses Recommended Citation Centeno, Diana Caroly, "The Footprints of Saharan Air Layer and Lightning on the Formation of Tropical Depressions over the Eastern Atlantic Ocean" (2014). Master's Theses. 4456. DOI: https://doi.org/10.31979/etd.cq5z-6zek https://scholarworks.sjsu.edu/etd_theses/4456 This Thesis is brought to you for free and open access by the Master's Theses and Graduate Research at SJSU ScholarWorks. It has been accepted for inclusion in Master's Theses by an authorized administrator of SJSU ScholarWorks. For more information, please contact [email protected]. THE FOOTPRINTS OF SAHARAN AIR LAYER AND LIGHTNING ON THE FORMATION OF TROPICAL DEPRESSIONS OVER THE EASTERN ATLANTIC OCEAN A Thesis Presented to The Faculty of the Department of Meteorology and Climate Science San José State University In Partial Fulfillment of the Requirements for the Degree Master of Science by Diana C. Centeno Delgado August 2014 © 2014 Diana C. Centeno Delgado ALL RIGHTS RESERVED The Designated Thesis Committee Approves the Thesis Titled THE FOOTPRINTS OF SAHARAN AIR LAYER AND LIGHTNING ON THE FORMATION OF TROPICAL DEPRESSIONS OVER THE EASTERN ATLANTIC OCEAN by Diana C. Centeno Delgado APPROVED FOR THE DEPARTMENT OF METEOROLOGY AND CLIMATE SCIENCE SAN JOSÉ STATE UNIVERSITY August 2014 Dr. Sen Chiao Department of Meteorology and Climate Science Dr. -
Dust Storms in Arizona
Radar-Based Characteristics of Dust Storms in Arizona DUST WORKSHOP 2020 JARET ROGERS2 SAMUEL MELTZER1 PAUL INIGUEZ2 1: Arizona State University, Tempe, AZ 2: National Weather Service, Phoenix, AZ Dust Storm (Haboob) Definition “An intense sandstorm or dust storm with sand and/or dust often lofted to heights as high as 1500 m (~5000 ft), resulting in a “wall of dust” along the leading edge of the haboob that can be visually stunning.” – AMS Glossary NWS definition: Dust storm warning is ¼ or less mile visibility. NWS warnings now use polygons (Waters 2018). Impacts Past Incidents Due to Dust Storms 28 June 1970 – 12 fatalities after several vehicles collided on Interstate 10 near Casa Grande. 9 April 1995 – 10 fatalities and 20 injured on Interstate 10 near Bowie after 4 different accidents, totaling 24 vehicles. 12 July 1964 – 8 fatalities and 25 injured after 9 cars, 3 trailer rigs, and 1 pickup were involved in a chain reaction collision on Interstate 10 near Red Rock. 4 Oct 2011 – 1 fatality and 15 injured in 25 vehicle crash on I-10 Statewide Arizona dust events Phoenix dust events Adapted from Lader et al. 2016 Adapted from Lader et al. 2016 Dust storm NWS local storm reports (2005-2018) Dust Storm Climatology (LSRs) * 2018 shattered previous record with 175 reports. Radar Analysis of Dust Storms Goal: Create a small climatology of summer haboobs across southern/central Arizona, using combination of radar and storm reports. Dataset: 35 unique dust storms from 2010 through 2018. >= 3 dust storm reports (1/4 mile) separated by more than 20 miles. -
Sand and Dust Storms in Asia and the Pacific: Opportunities for Regional Cooperation and Action
Asia and the Pacific: Sand and Dust Storms in Opportunities for Regional Cooperation and Action Sand and Dust Storms in Asia and the Pacific: Opportunities for Regional Cooperation and Action This report—Sand and Dust Storms in Asia and the Pacific: Opportunities for Regional Cooperation and Action—analyses potential drivers, points to the risk of problem areas and identifies gaps in information, cooperation and policy action to enhance the science-based understanding of the phenomenon among policymakers. It aims to support the development of adaptation and mitigationpolicies related sandtoanddust storm at the regional and national levels. UNITED NATIONS PUBLICATION PRINTED IN BANGKOK MAY 2018 The shaded areas of the map indicate ESCAP members and associate members.* The Economic and Social Commission for Asia and the Pacific (ESCAP) serves as the United Nations’ regional hub promoting cooperation among countries to achieve inclusive and sustainable development. The largest regional intergovernmental platform with 53 Member States and 9 Associate Members, ESCAP has emerged as a strong regional think-tank offering countries sound analytical products that shed insight into the evolving economic, social and environmental dynamics of the region. The Commission’s strategic focus is to deliver on the 2030 Agenda for Sustainable Development, which it does by reinforcing and deepening regional cooperation and integration to advance connectivity, financial cooperation and market integration. ESCAP’s research and analysis coupled with its policy advisory services, capacity building and technical assistance to governments aims to support countries’ sustainable and inclusive development ambitions. The ESCAP office is located in Bangkok, Thailand. Please visit the ESCAP website at www.unescap. -
Sand and Dust Storms
UNEA-2 FACT SHEET: SAND AND DUST STORMS Why sand and dust storms matter Sand and dust storms are a global environmental problem that affects the health and livelihoods of millions of people across the world. These storms, which have increased in frequency, intensity and geographical range in recent decades, have an immense impact on the global economy, forcing airports and schools to close, inter- rupting supply chains, destroying crops and overwhelming hospitals. Fine particles of dust can travel thousands of miles on the back of these storms, which may also carry pathogens and harmful substances, causing acute and chronic respiratory problems. Dust storms also increase desertifi- cation, drought and soil salinity while reducing water supplies and impeding renewable energy sources. Dust storms can also be triggered and exacerbated by climate change, drought, land degradation and un-sustainable management of land and water resources. The state of play • In the Middle East and North Africa, about $13 billion in Gross Domestic Product (GDP) are lost every year due to dust storms. • Dust storms contribute to poor air quality. The World Health Organization estimates that seven million people die from poor air quality every year. • Dust storms damage crops and remove the fertile top soil, which reduces agricultural productivity. Much of Iraq’s fertile lands have been literally blown away as desertification intensifies. The Iraqi government recorded 122 dust storms and 283 dusty days in a single year. Within the next ten years, Iraq could witness 300 dust events per year. • About two to three billion tonnes of fine soil particles leave Africa every year in dust storms, draining the continent of its fertility and biological productivity.