The Impact of Unique Meteorological Phenomena Detected by the Oklahoma Mesonet and ARS Micronet on Automated Quality Control Christopher A
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2020 Infra Surface Weather Observations
Surface Weather Observations Comparison of Various Observing Systems Scott Landolt & Matthias Steiner National Center for Atmospheric Research [email protected] USHST Infrastructure Summit 12 – 13 March 2020 in Washington, DC © 2020 University Corporation for Atmospheric Research 1 Surface Stations & Reporting Frequency Station Type Frequency of Reports Automated Surface 5 minutes Observing System (ASOS) (limited access to 1 minute data) Automated Weather 20 minutes Observing System (AWOS) 15 minutes (standard), can be Road Weather Information more frequent but varies state to System (RWIS) state and even site to site 5 – 15 minutes, can vary from Mesonet station to station Iowa station network © 2020 University Corporation for Atmospheric Research 2 Reporting Variables Weather Variable ASOS AWOS RWIS Mesonet Temperature X X X X Relative X X X X Humidity/Dewpoint Wind Speed/Direction X X X X Barometric Pressure X X X X Ceiling Height X X X X Visibility X X X X Present Weather X X X X Precipitation X X X X Accumulation Road Condition X X X X X – All Stations Report X – Some Stations Report X – No Stations Report © 2020 University Corporation for Atmospheric Research 3 Station Siting Requirements Station Type Siting Areal Representativeness Automated Surface Miles (varies depending on Airport grounds, unobstructed Observing System (ASOS) local conditions & weather) Automated Weather Miles (varies depending on Airport grounds, unobstructed Observing System (AWOS) local conditions & weather) Next to roadways, can be in canyons, valleys, mountain -
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. -
Relative Forecast Impact from Aircraft, Profiler, Rawinsonde, VAD, GPS-PW, METAR and Mesonet Observations for Hourly Assimilation in the RUC
16.2 Relative forecast impact from aircraft, profiler, rawinsonde, VAD, GPS-PW, METAR and mesonet observations for hourly assimilation in the RUC Stan Benjamin, Brian D. Jamison, William R. Moninger, Barry Schwartz, and Thomas W. Schlatter NOAA Earth System Research Laboratory, Boulder, CO 1. Introduction A series of experiments was conducted using the Rapid Update Cycle (RUC) model/assimilation system in which various data sources were denied to assess the relative importance of the different data types for short-range (3h-12h duration) wind, temperature, and relative humidity forecasts at different vertical levels. This assessment of the value of 7 different observation data types (aircraft (AMDAR and TAMDAR), profiler, rawinsonde, VAD (velocity azimuth display) winds, GPS precipitable water, METAR, and mesonet) on short-range numerical forecasts was carried out for a 10-day period from November- December 2006. 2. Background Observation system experiments (OSEs) have been found very useful to determine the impact of particular observation types on operational NWP systems (e.g., Graham et al. 2000, Bouttier 2001, Zapotocny et al. 2002). This new study is unique in considering the effects of most of the currently assimilated high-frequency observing systems in a 1-h assimilation cycle. The previous observation impact experiments reported in Benjamin et al. (2004a) were primarily for wind profiler and only for effects on wind forecasts. This new impact study is much broader than that the previous study, now for more observation types, and for three forecast fields: wind, temperature, and moisture. Here, a set of observational sensitivity experiments (Table 1) were carried out for a recent winter period using 2007 versions of the Rapid Update Cycle assimilation system and forecast model. -
Weatherscope Weatherscope Application Information: Weatherscope Is a Stand-Alone Application That Makes Viewing Weather Data Easier
User Guide - Macintosh http://earthstorm.ocs.ou.edu WeatherScope WeatherScope Application Information: WeatherScope is a stand-alone application that makes viewing weather data easier. To run WeatherScope, Mac OS X version 10.3.7, a minimum of 512MB of RAM, and an accelerated graphics card with 32MB of VRAM are required. WeatherScope is distributed freely for noncommercial and educational use and can be used on both Apple Macintosh and Windows operating systems. How do I Download WeatherScope? To download the application, go to http://earthstorm.ocs.ou.edu, select Data, Software, Download, or go to http://www. ocs.ou.edu/software. There will be three options: WeatherBuddy, WeatherScope, and WxScope Plugin. You will want to choose WeatherScope. There are two options under the application: Macintosh or Windows. Choose Macintosh to download the application. The installation wizard will automatically save to your desktop. Go to your desktop and double click on the icon that says WeatherScope- x.x.x.pkg. Several dialog messages will appear. The fi rst message will inform you that you are about to install the application. The next message tells you about computer system requirements in order to download the application. The following message is the Software License Agreement. It is strongly suggested that you read this agreement. If you agree, click Agree. If you do not agree, click Disagree and the software will not be installed onto your computer. The next message asks you to select a destination drive (usually your hard drive). The setup will run and install the software on your computer. You may then press Close. -
Reading Mesonet Rain Maps
Oklahoma’s Weather Network Lesson 2 - Rain Maps Reading Mesonet Rain Maps Estimated Lesson Time: 30 minutes Introduction Every morning when you get ready for school, you decide what you are going to wear for the day. Often you might ask your parents what the weather is like or check the weather yourself before getting dressed. Then you can decide if you will wear a t-shirt or sweater, flip-flops or rain boots. The Oklahoma Mesonet, www.mesonet.org, is a weather and climate network covering the state. The Mesonet collects measurements such as air tempera- ture, rainfall, wind speed, and wind direction, every five minutes . These mea- surements are provided free to the public online. The Mesonet has 120 remote weather stations across the state collecting data. There is at least one in every county which means there is one located near you. Our data is used by people across the state. Farmers use our data to grow their crops, and firefighters use it to help put out a fire. Emergency managers in your town use it to warn you of tornadoes, and sound the town’s sirens. Mesonet rainfall data gives a statewide view, updated every five minutes. When reading the Mesonet rainfall accumulation maps, notice each Mesonet site displays accumulated rainfall. The map also displays the National Weather Service (NWS) River Forecast Center’s rainfall estimates (in color) across Oklahoma based on radar (an instrument that can locate precipitation and its motion). For example, areas in blue have lower rainfall than areas in red or purple. -
P1.4 West Texas Mesonet Observations of Wake Lows and Heat Bursts Across Northwest Texas
P1.4 WEST TEXAS MESONET OBSERVATIONS OF WAKE LOWS AND HEAT BURSTS ACROSS NORTHWEST TEXAS Mark R. Conder*, Steven R. Cobb, and Gary D. Skwira National Weather Service Forecast Office, Lubbock, Texas 1. INTRODUCTION Wake lows (WLs) and heat bursts (HBs) are mesoscale phenomena associated with thunderstorms that can result in strong and sometimes severe (>25.5 m s-1), near-surface winds. The operational detection of severe winds is problematic because the associated convection can appear quite innocuous via WSR-88D data. The thermodynamic environment that supports WL and HB development is similar, and is often compared to the classic “onion” sounding structure as described by Zipser (1977). Observational studies such as Johnson et al. (1989) show that nearly dry-adiabatic lapse rates are prevalent in the lower to mid-troposphere, with a shallow stable layer near ground level. This type of environment is most commonly observed in the high plains during the warm season. While documented heat bursts were infrequent in the past, the recent expansion of surface mesonetworks are increasing the likelihood that these events will be sampled. One such network is the West Texas Mesonet (WTXM), a collection of over 40 meteorological stations spread across the Panhandle and South Plains of northwest Texas. During the period 1 June 2004 to 30 August 2006, the authors have FIG. 1. The Study area including the WTXM station recorded 10 WL/HB events that have been sampled by locations. Not all stations were available for every stations of the WTXM. Some of the more extreme event. measurements include a 15 degrees Celsius increase in temperature at the Pampa and McClean WTXM sites in -1 Meteorological data from each WTXM station is one event and 35 m s wind gusts at sites in Brownfield recorded in 5-minute intervals, representing average and Jayton on separate occasions. -
Alternative Earth Science Datasets for Identifying Patterns and Events
https://ntrs.nasa.gov/search.jsp?R=20190002267 2020-02-17T17:17:45+00:00Z Alternative Earth Science Datasets For Identifying Patterns and Events Kaylin Bugbee1, Robert Griffin1, Brian Freitag1, Jeffrey Miller1, Rahul Ramachandran2, and Jia Zhang3 (1) University of Alabama in Huntsville (2) NASA MSFC (3) Carnegie Mellon Universityv Earth Observation Big Data • Earth observation data volumes are growing exponentially • NOAA collects about 7 terabytes of data per day1 • Adds to existing 25 PB archive • Upcoming missions will generate another 5 TB per day • NASA’s Earth observation data is expected to grow to 131 TB of data per day by 20222 • NISAR and other large data volume missions3 Over the next five years, the daily ingest of data into the • Other agencies like ESA expect data EOSDIS archive is expected to grow significantly, to more 4 than 131 terabytes (TB) of forward processing. NASA volumes to continue to grow EOSDIS image. • How do we effectively explore and search through these large amounts of data? Alternative Data • Data which are extracted or generated from non-traditional sources • Social media data • Point of sale transactions • Product reviews • Logistics • Idea originates in investment world • Include alternative data sources in investment decision making process • Earth observation data is a growing Image Credit: NASA alternative data source for investing • DMSP and VIIRS nightlight data Alternative Data for Earth Science • Are there alternative data sources in the Earth sciences that can be used in a similar manner? • -
TC Modelling and Data Assimilation
Tropical Cyclone Modeling and Data Assimilation Jason Sippel NOAA AOML/HRD 2021 WMO Workshop at NHC Outline • History of TC forecast improvements in relation to model development • Ongoing developments • Future direction: A new model History: Error trends Official TC Track Forecast Errors: • Hurricane track forecasts 1990-2020 have improved markedly 300 • The average Day-3 forecast location error is 200 now about what Day-1 error was in 1990 100 • These improvements are 1990 2020 largely tied to improvements in large- scale forecasts History: Error trends • Hurricane track forecasts have improved markedly • The average Day-3 forecast location error is now about what Day-1 error was in 1990 • These improvements are largely tied to improvements in large- scale forecasts History: Error trends Official TC Intensity Forecast Errors: 1990-2020 • Hurricane intensity 30 forecasts have only recently improved 20 • Improvement in intensity 10 forecast largely corresponds with commencement of 0 1990 2020 Hurricane Forecast Improvement Project HFIP era History: Error trends HWRF Intensity Skill 40 • Significant focus of HFIP has been the 20 development of the HWRF better 0 Climo better HWRF model -20 -40 • As a result, HWRF intensity has improved Day 1 Day 3 Day 5 significantly over the past decade HWRF skill has improved up to 60%! Michael Talk focus: How better use of data, particularly from recon, has helped improve forecasts Michael Talk focus: How better use of data, particularly from recon, has helped improve forecasts History: Using TC Observations -
The Southern Plains Cyclone
The Southern Plains Cyclone A Weather Newsletter from your Norman Forecast Office for the Residents of western and central Oklahoma and western north Texas We Make the Difference When it Matters Most! Volume 2 Summer 2004 Issue 3 Behind the Scenes at the Norman Forecast Office Meet Your Weatherman Cheryl Sharpe By Rick Smith, Warning Coordination Meteorologist The National Weather Service’s ther caused by the weather or made main mission is to provide information worse by the weather – tornadoes and to help save lives. This is the reason we severe thunderstorms, flooding, ice come to work everyday. We are part of a storms, blizzards, wildfires, and heat network of 122 local weather forecast waves, among others. But, did you offices that cover the entire United know that the Norman Forecast Office States, with each office responsible for a also plays a key role in assisting with specific group of counties. The people at non-weather related disasters? each of these offices work hard to pro- From the Murrah Building bombing vide the best local weather information in 1995 to wildfires and other non- possible. weather related emergencies, the NWS At the Norman Forecast Office, we provides support and information in a take this responsibility seriously and variety of situations. ¡Hola! I am Cheryl Sharpe, one of strive to be the best when it comes to pro- We are staffed 24 hours a day every- the general forecasters at the Norman viding information you can use to help day of the year with at least two people Forecast Office. In addition to my regu- make decisions, plan activities, or just on shift at all times to allow us to re- lar duties as a meteorologist, I also assist live your day-to-day life in Oklahoma spond. -
Evaluating NEXRAD Multisensor Precipitation Estimates for Operational Hydrologic Forecasting
JUNE 2000 YOUNG ET AL. 241 Evaluating NEXRAD Multisensor Precipitation Estimates for Operational Hydrologic Forecasting C. BRYAN YOUNG,A.ALLEN BRADLEY,WITOLD F. K RAJEWSKI, AND ANTON KRUGER Iowa Institute of Hydraulic Research and Department of Civil and Environmental Engineering, The University of Iowa, Iowa City, Iowa MARK L. MORRISSEY Environmental Veri®cation and Analysis Center, University of Oklahoma, Norman, Oklahoma (Manuscript received 9 August 1999, in ®nal form 10 January 2000) ABSTRACT Next-Generation Weather Radar (NEXRAD) multisensor precipitation estimates will be used for a host of applications that include operational stream¯ow forecasting at the National Weather Service River Forecast Centers (RFCs) and nonoperational purposes such as studies of weather, climate, and hydrology. Given these expanding applications, it is important to understand the quality and error characteristics of NEXRAD multisensor products. In this paper, the issues involved in evaluating these products are examined through an assessment of a 5.5-yr record of multisensor estimates from the Arkansas±Red Basin RFC. The objectives were to examine how known radar biases manifest themselves in the multisensor product and to quantify precipitation estimation errors. Analyses included comparisons of multisensor estimates based on different processing algorithms, com- parisons with gauge observations from the Oklahoma Mesonet and the Agricultural Research Service Micronet, and the application of a validation framework to quantify error characteristics. This study reveals several com- plications to such an analysis, including a paucity of independent gauge data. These obstacles are discussed and recommendations are made to help to facilitate routine veri®cation of NEXRAD products. 1. Introduction WSR-88D radars and a network of gauges that report observations to the RFC in near±real time (Fulton et al. -
Mesorefmatl.PM6.5 For
What is the Oklahoma Mesonet? Overview The Oklahoma Mesonet is a world-class network of environ- mental monitoring stations. The network was designed and implemented by scientists at the University of Oklahoma (OU) and at Oklahoma State University (OSU). The Oklahoma Mesonet consists of 114 automated stations covering Oklahoma. There is at least one Mesonet station in each of Oklahoma’s 77 counties. Definition of “Mesonet” “Mesonet” is a combination of the words “mesoscale” and “network.” • In meteorology, “mesoscale” refers to weather events that range in size from a few kilometers to a few hundred kilo- meters. Mesoscale events last from several minutes to several hours. Thunderstorms and squall lines are two examples of mesoscale events. • A “network” is an interconnected system. Thus, the Oklahoma Mesonet is a system designed to mea- sure the environment at the size and duration of mesoscale weather events. At each site, the environment is measured by a set of instru- ments located on or near a 10-meter-tall tower. The measure- ments are packaged into “observations” every 5 minutes, then the observations are transmitted to a central facility every 15 minutes – 24 hours per day year-round. The Oklahoma Climatological Survey (OCS) at OU receives the observations, verifies the quality of the data and provides the data to Mesonet customers. It only takes 10 to 20 minutes from the time the measurements are acquired until they be- come available to customers, including schools. OCS Weather Series Chapter 1.1, Page 1 Copyright 1997 Oklahoma Climatological Survey. All rights reserved. As of 1997, no other state or nation is known to have a net- Fun Fact work that boasts the capabilities of the Oklahoma Mesonet. -
Observations of Extreme Variations in Radiosonde Ascent Rates
Observations of Significant Variations in Radiosonde Ascent Rates Above 20 km. A Preliminary Report W.H. Blackmore Upper air Observations Program Field Systems Operations Center NOAA National Weather Service Headquarters Ryan Kardell Weather Forecast Office, Springfield, Missouri NOAA National Weather Service Latest Edition, Rev D, June 14, 2012 1. Introduction: Commonly known measurements obtained from radiosonde observations are pressure, temperature, relative humidity (PTU), dewpoint, heights and winds. Yet, another measurement of significant value, obtained from high resolution data, is the radiosonde ascent rate. As the balloon carrying the radiosonde ascends, its' rise rate can vary significantly owing to vertical motions in the atmosphere. Studies on deriving vertical air motions and other information from radiosonde ascent rate data date from the 1950s (Corby, 1957) to more recent work done by Wang, et al. (2009). The causes for the vertical motions are often from atmospheric gravity waves that are induced by such phenomena as deep convection in thunderstorms (Lane, et al. 2003), jet streams, and wind flow over mountain ranges. Since April, 1995, the National Weather Service (NWS) has archived radiosonde data from the MIcroART upper air system at six second intervals for nearly all stations in the NWS 92 station upper air network. With the network deployment of the Radiosonde Replacement System (RRS) beginning in August, 2005, the resolution of the data archived increased to 1 second intervals and also includes the GPS radiosonde height data. From these data, balloon ascent rate can be derived by noting the rate of change in height for a period of time The purpose of this study is to present observations of significant variations of radiosonde balloon ascent rates above 20 km in the stratosphere taken close to (less than 150 km away) and near the time of severe and non- severe thunderstorms.