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Operating Instructions Present Weather Sensor Parsivel
Operating instructions Present Weather Sensor Parsivel English We reserve the right to make technical changes! Table of contents 1 Scope of delivery 5 2 Part numbers 5 3 Parsivel Factory Settings 6 4 Safety instructions 7 5 Introduction 8 5.1 Functional principle 8 5.2 Connection Options for the Parsivel 9 6 Installing the Parsivel 10 6.1 Cable Selection 10 6.2 Wiring the Parsivel 11 6.3 Grounding the Parsivel 13 6.4 Installing the Parsivel 14 7 Connecting the Parsivel to a data logger 15 7.1 Connecting the Parsivel to the LogoSens Station Manager via RS-485 interface 15 7.2 Connecting the Parsivel to a Data logger via the SDI-12 Interface 17 7.3 Connecting the Parsivel to a Data Logger with Impulse/Status Input 21 8 Connecting the Parsivel to a PC 23 8.1 Connecting the Parsivel to Interface Converter RS-485/RS-232 (Accessories) 23 8.2 Connecting the Parsivel to the ADAM-4520 Converter RS-485/RS-232 (Accessories) 25 8.3 Connecting the Parsivel to Interface Converter RS-485/USB (Accessories) 26 8.4 Connecting the Parsivel to any RS-485 Interface Converter 27 8.5 Connecting the Parsivel for configuration via the Service-Tool to a PC 27 9 Connecting the Parsivel to a Power Supply (Accessory) 29 10 Heating the Parsivel sensor heads 30 11 Operating Parsivel with a Terminal software 31 11.1 Set up communications between the Parsivel and the terminal program 31 11.2 Measured value numbers 32 11.3 Defining the formatting string 33 11.4 OTT telegram 33 11.5 Updating Parsivel Firmware 34 12 Maintenance 36 12.1 Cleaning the laser’s protective glass -
UMAP Lidars (UMBC Measurements of Atmospheric Pollution)
UMAP Lidars (UMBC Measurements of Atmospheric Pollution) Raymond Hoff Ruben Delgado, Tim Berkoff, Jamie Compton, Kevin McCann, Patricia Sawamura, Daniel Orozco, UMBC October 5 , 2010 DISCOVR-AQ Engel-Cox, J. et.al. 2004. Atmospheric Environment. Baltimore, MD Summer 2004 100 1.6 90 Old Town TEOMPM2.5 MODIS 1.4 80 MODIS AOD July 21 ) 1.2 3 70 Mixed down July 9 smoke 1 g/m 60 High altitude µ ( smoke 50 0.8 (g ) AOD 2.5 40 0.6 PM 30 0.4 20 0.2 MODISAerosol Optical Depth 10 0 0 07/01/04 07/08/04 07/15/04 07/22/04 07/29/04 08/05/04 08/12/04 08/19/04 08/26/04 Courtesy EPA/UWisconsin Conceptually simple idea Η α Extinction Profile and PBL H 100 1.6 Smoke mixing in Hourly PM2.5 90 Daily Average PM2.5 1.4 Maryland 80 MODIS AOD Lidar OD Total Column 20-22 July 2004 Lidar OD Below Boundary Layer 1.2 ) 70 3 60 1 (ug/m 50 0.8 2.5 40 0.6 PM 30 Depth Optical 0.4 20 10 0.2 0 0 07/19/04 07/20/04 07/21/04 07/22/04 07/23/04 Before upgrading: 2008 Existing ALEX - UV N2, H2O Raman lidar - 355, 389, 407 nm ELF - 532(⊥,), 1064 elastic lidar GALION needs QA/QC site for lidars in US Have all the wavelengths that people might use routinely Ability to cross-calibrate instruments Need to add MPL and LEOSPHERE Micropulse Lidar Leosphere UMBC Monitoring of Atmospheric Pollution (UMAP) (NASA Radiation Sciences Supported Project) Weblinks to instruments http://alg.umbc.edu/UMAP Data available 355 nm Leosphere retrieval (new) New instruments BAM and TEOM (PM2.5 continuously) TSI 3683 (3λ nephelometer) CIMEL (8λ AOD, size distribution) LICEL (new detector package for ALEX) MPL Shareware Concept Lidar and radiosonde measurements were also used to evaluate nearby ACARS PBLH estimates at RFK and BWI airports. -
Disdrometer Performance Optimization for Use in Urban Settings Based on the Parameters That Affect the Measurements
S S symmetry Article Disdrometer Performance Optimization for Use in Urban Settings Based on the Parameters that Affect the Measurements Ferran Mocholí Belenguer 1,* , Antonio Martínez-Millana 2 , Antonio Mocholí Salcedo 3 , Víctor Milián Sánchez 4 and María Josefa Palomo Anaya 4 1 Traffic Control Systems Group, ITACA Institute, Universitat Politècnica de València, 46022 Valencia, Spain 2 SABIEN Group, ITACA Institute, Universitat Politècnica de València, 46022 Valencia, Spain; [email protected] 3 Department of Electronic Engineering, ITACA Institute, Universitat Politècnica de València, 46022 Valencia, Spain; [email protected] 4 Chemical and Nuclear Engineering Department, Institute of Industrial, Radiological and Environmental Safety, Universitat Politècnica de València, 46022 Valencia, Spain; [email protected] (V.M.S.); [email protected] (M.J.P.A.) * Correspondence: [email protected]; Tel.: +34-610833056 Received: 15 November 2019; Accepted: 13 February 2020; Published: 20 February 2020 Abstract: There are currently different types of commercial optical disdrometers to measure the rainfall intensity, of which many are commonly used for monitoring road conditions. Having information about the amount of rain, the composition of the precipitation particles and visibility are essential to avoid accidents, which requires intelligent systems that warn drivers and redirect traffic. However, few studies related to Intelligent Transport Systems (ITS) have been performed regarding why these devices are not optimized for this type of applications. Therefore, this paper analyzes and evaluates the operating mode of these equipment through their theoretical model, which will allow the design of prototypes of disdrometers with different characteristics. In addition, this model will be implemented in a simulation program, through which an exhaustive study analyzing how the type of precipitation and its intensity affect the measures provided by the model will be conducted. -
Physical Process Cruise 2018 020720
Physical Process Cruise 2018 Cruise Report The Nansen Legacy Report Series 2/2020 Physical Process Cruise 2018 Cruise 2018709 R.V. Kronprins Haakon Longyearbyen-Longyearbyen September 14 -September 24, 2018 Authors: Ilker Fer – cruise leader Frank Nilsen- cruise co-leader Anthony Bosse Eva Falck Trygve Fossum Lars R Hole Zoe Koenig Eivind Kolås Aleksander Dürr Libæk Ben Lincoln Martin Ludvigsen Marika Marnela Malte Müller Petter Norgren Inger Lise Næss Jean Rabault Andrew Siedl Ragnheid Skogseth Inga Breisnes Utkilen To be cited as: Ilker Fer, Frank Nilsen, Anthony Bosse, Eva Falck, Trygve Fossum, Lars R Hole, Zoe Koenig, Eivind Kolås, Aleksander Dürr Libæk, Ben Lincoln, Martin Ludvigsen, Marika Marnela, Malte Müller, Petter Norgren, Inger Lise Næss, Jean Rabault, Andrew Siedl, Ragnheid Skogseth and Inga Breisnes Utkilen (2020). Physical Process Cruise 2018: Cruise Report. The Nansen Legacy Report Series, 2/2020. DOI: https://doi.org/10.7557/nlrs.5503 © The authors. This report is licensed under the Creative Commons Attribution 4.0 International license ISSN 2703-7525 Publisher: Septentrio Academic Publishing, Tromsø, Norway 1 Contents 1. Background ......................................................................................................................................... 4 2. Survey area ......................................................................................................................................... 5 3. Activity reports ................................................................................................................................. -
Thies Laser Precipitation Monitor
Instruction for Use 021341/07/11 Laser Precipitation Monitor 5.4110.xx.x00 V2.5x STD WEATHER DATA - THE WORLD OF INVISIBLE LASER RADIATION DO NOT VIEW DIRECTLY WITH OPTICAL INSTRUMENTS CLASS 1M LASER PRODUCT ADOLF THIES GmbH & Co. KG Hauptstraße 76 37083 Göttingen Germany Box 3536 + 3541 37025 Göttingen Phone +49 551 79001-0 Fax +49 551 79001-65 www.thiesclima.com [email protected] THE WORLD OF WEATHER DATA - Safety Instructions • Before operating with or at the device/product, read through the operating instructions. This manual contains instructions which should be followed on mounting, start-up, and operation. A non-observance might cause: - failure of important functions - Endangering of persons by electrical or mechanic effect - Damages at objects • Mounting, electrical connection and wiring of the device/product must be carried out only by a qualified technician who is familiar with and observes the engineering regulations, provisions and standards applicable in each case. • Repairs and maintenance may only be carried out by trained staff or Adolf Thies GmbH & Co. KG. Only components and spare parts supplied and/or recommended by Adolf Thies GmbH & Co. KG should be used for repairs. • Electrical devices/products must be mounted and wired only in voltage-free state. • Adolf Thies GmbH & Co KG guarantees proper functioning of the device/products provided that no modifications have been made to the mechanics, electronics or software, and that the following points are observed: • All information, warnings and instructions for use included in these operating instructions must be taken into account and observed as this is essential to ensure trouble-free operation and a safe condition of the measuring system / device / product. -
Comparison of the Compact Dopplar Radar Rain Gauge and Optical
Short Paper J. Agric. Meteorol. 67 (3): 199–204, 2011 Comparison of the compact dopplar radar rain gauge and optical disdrometer Ko NAKAYA†, and Yasushi TOYODA (Central Research Institute of Electric Power Industry, 1646 Abiko, Abiko, Chiba, 270–1194, Japan) Abstract The operations of a compact Doppler radar rain gauge (R2S; Rufft, FRG) and optical disdrometer (LPM; THIES, FRG) are based on raindrop size distribution (DSD) measurements. We checked the instrumental error of these sensors and compared each sensor with a reference tipping-bucket rain gauge. This is because both rain gauges can detect fine particles and so they can function as rain sensors. The R2S has a measuring bias of rainfall intensity when the drop size distribution differs from the assumed statistical DSD model. The instrumental error on the LPM is small; in fact, the LPM shows good agreement with the reference rain gauge. Where the atmospheric density differs remarkably from the standard elevation, as is the case in highland areas, the R2S requires calibration using a reference rain gauge. The resultant calibration coefficient of the R2S to convert the reading into a reference tip- ping-bucket rain-gauge equivalent was 0.51 in a forest at an elevation of 1380 m. Further gathering of calibration coefficients obtained at different elevations will improve the R2S’s applicability. Key words: Doppler radar rain gauge, Drop size distribution, Optical disdrometer, Tipping-bucket rain gauge. Although the accuracy and suggested errors of rainfall 1. Introduction observations using typical Doppler radar have been Rainfall properties, such as the intensity, amount, reviewed in many studies (Maki et al., 1998, for duration, and type, constitute important meteorological example), reviews for the R2S compared to a reference information that is useful for agriculture and forestation rain gauge are few. -
Meteorological Monitoring Guidance for Regulatory Modeling Applications
United States Office of Air Quality EPA-454/R-99-005 Environmental Protection Planning and Standards Agency Research Triangle Park, NC 27711 February 2000 Air EPA Meteorological Monitoring Guidance for Regulatory Modeling Applications Air Q of ua ice li ff ty O Clean Air Pla s nn ard in nd g and Sta EPA-454/R-99-005 Meteorological Monitoring Guidance for Regulatory Modeling Applications U.S. ENVIRONMENTAL PROTECTION AGENCY Office of Air and Radiation Office of Air Quality Planning and Standards Research Triangle Park, NC 27711 February 2000 DISCLAIMER This report has been reviewed by the U.S. Environmental Protection Agency (EPA) and has been approved for publication as an EPA document. Any mention of trade names or commercial products does not constitute endorsement or recommendation for use. ii PREFACE This document updates the June 1987 EPA document, "On-Site Meteorological Program Guidance for Regulatory Modeling Applications", EPA-450/4-87-013. The most significant change is the replacement of Section 9 with more comprehensive guidance on remote sensing and conventional radiosonde technologies for use in upper-air meteorological monitoring; previously this section provided guidance on the use of sodar technology. The other significant change is the addition to Section 8 (Quality Assurance) of material covering data validation for upper-air meteorological measurements. These changes incorporate guidance developed during the workshop on upper-air meteorological monitoring in July 1998. Editorial changes include the deletion of the “on-site” qualifier from the title and its selective replacement in the text with “site specific”; this provides consistency with recent changes in Appendix W to 40 CFR Part 51. -
Standard Methods for the Examination of Water and Wastewater
Standard Methods for the Examination of Water and Wastewater Part 1000 INTRODUCTION 1010 INTRODUCTION 1010 A. Scope and Application of Methods The procedures described in these standards are intended for the examination of waters of a wide range of quality, including water suitable for domestic or industrial supplies, surface water, ground water, cooling or circulating water, boiler water, boiler feed water, treated and untreated municipal or industrial wastewater, and saline water. The unity of the fields of water supply, receiving water quality, and wastewater treatment and disposal is recognized by presenting methods of analysis for each constituent in a single section for all types of waters. An effort has been made to present methods that apply generally. Where alternative methods are necessary for samples of different composition, the basis for selecting the most appropriate method is presented as clearly as possible. However, samples with extreme concentrations or otherwise unusual compositions or characteristics may present difficulties that preclude the direct use of these methods. Hence, some modification of a procedure may be necessary in specific instances. Whenever a procedure is modified, the analyst should state plainly the nature of modification in the report of results. Certain procedures are intended for use with sludges and sediments. Here again, the effort has been to present methods of the widest possible application, but when chemical sludges or slurries or other samples of highly unusual composition are encountered, the methods of this manual may require modification or may be inappropriate. Most of the methods included here have been endorsed by regulatory agencies. Procedural modification without formal approval may be unacceptable to a regulatory body. -
Ott Parsivel - Enhanced Precipitation Identifier for Present Weather, Drop Size Distribution and Radar Reflectivity - Ott Messtechnik, Germany
® OTT PARSIVEL - ENHANCED PRECIPITATION IDENTIFIER FOR PRESENT WEATHER, DROP SIZE DISTRIBUTION AND RADAR REFLECTIVITY - OTT MESSTECHNIK, GERMANY Kurt Nemeth1, Martin Löffler-Mang2 1 OTT Messtechnik GmbH & Co. KG, Kempten (Germany) 2 HTW, Saarbrücken (Germany) as a laser-optic enhanced precipitation identifier and present weather sensor. The patented extinction method for simultaneous measurements of particle size and velocity of all liquid and solid precipitation employs a direct physical measurement principle and classification of hydrometeors. The instrument provides a full picture of precipitation events during any kind of weather phenomenon and provides accurate reporting of precipitation types, accumulation and intensities without degradation of per- formance in severe outdoor environments. Parsivel® operates in any climate regime and the built-in heating device minimizes the negative effect of freezing and frozen precipitation accreting critical surfaces on the instrument. Parsivel® can be integrated into an Automated Surface/ Weather Observing System (ASOS/AWOS) as part of the sensor suite. The derived data can be processed and 1. Introduction included into transmitted weather observation reports and messages (WMO, SYNOP, METAR and NWS codes). ® OTT Parsivel : Laser based optical Disdrometer for 1.2. Performance, accuracy and calibration procedure simultaneous measurement of PARticle SIze and VELocity of all liquid and solid precipitation. This state The new generation of Parsivel® disdrometer provides of the art instrument, designed to operate under all the latest state of the art optical laser technology. Each weather conditions, is capable of fulfilling multiple hydrometeor, which falls through the measuring area is meteorological applications: present weather sensing, measured simultaneously for size and velocity with an optical precipitation gauging, enhanced precipitation acquisition cycle of 50 kHz. -
A Lysimetric Snow Pillow Station at Kùhtai/Tyrol R. KIRNBAUER & G. BLÔSCHL Institut Fur Hydraulik, Gewâsserkunde U. Wasse
Hydrology in Mountainous Regions. J - Hydrological Measurements; the Water Cycle (Proceedings of two Lausanne Symposia, August 1990). IAHS Publ. no. 193, 1990. A lysimetric snow pillow station at Kùhtai/Tyrol R. KIRNBAUER & G. BLÔSCHL Institut fur Hydraulik, Gewâsserkunde u. Wasserwirtschaft, Technische Universitât Wien, Karlsplatz 13, 1040 Vienna, Austria ABSTRACT For properly forecasting snowmeIt-runoff the understanding of processes associated with a melting snow cover may be of primary importance. For this purpose a snow monitoring station was installed at Kuhtai/Tyrol at an elevation of 1930 m a.s.l. In order to study individual physical processes typical snow cover situations are examined. These situations include cold and wet snow under varying weather conditions. Based on a few examples the diversity of phenomena occuring at the snow surface and within the snow cover is demonstrated. INTRODUCTION Within a short-term flood-forecasting system a snowmelt model should be capable of representing extreme conditions. As Leavesley (1989) points out, a more physically based understanding of the processes involved will improve forecast capabilities. Subjective watching of phenomena together with measuring adequate data of sufficient accuracy and time resolution may form the foundations of process understanding. Most field studies performed so far concentrated on investigating the energy input to snow, particularly under melting conditions (see e.g. Kuusisto, 1986). Differences in the relative importance of processes during contrasting weather conditions have been reported by numerous authors (e.g. Lang, 1986). Considering these differences some of the authors (e.g. Anderson, 1973) distinguished between advection and radiation melt situations in their models. In this study meteorological data and snowpack observations from an alpine experimental plot are presented. -
Data Requirements for Ceiling and Visibility Products Development 6
DOT/FAA/RD-94/5 Project Report ATC-212 Data Requirements for Ceiling and Visibility Products Development J. L. Keller 13 April 1994 Lincoln Laboratory MASSACHUSETTS INSTITUTE OF TECHNOLOGY LEXINGTON, MASSACHUSETTS Prepared for the Federal Aviation Administration, Washington, D.C. 20591 This document is available to the public through the National Technical Information Service, Springfield, VA 22161 This document is disseminated under the sponsorship of the Department of Transportation in the interest of information exchange. The United States Government assumes no liability for its contents or use thereof. TECHNICAL REPORT STANDARD TITLE PAGE 1. Report No. 2. Government Accession No. 3. Recipient's Catalog No. ATC-212 DOTfFAAJRD-94/5 4. TItle and Subtitle 5. Report Date 13 April 1994 Data Requirements for Ceiling and Visibility Products Development 6. Performing Organization Code 7. Author(s) 8. Performing Organization Report No. John L. Keller ATC-212 9. Performing Organization Name and Address 10. Work Unit No. (TRAIS) Lincoln Lahoratory, MIT P.O. Box 73 11. Contract or Grant No. Lexington, MA 02173-9108 DTFAO1-93-Z-02012 12. Sponsoring Agency Name and Address 13. Type of Report and Period Covered Department of Transportation Project Report Federal Aviation Administration Washington, DC 20591 14. Sponsoring Agency Code 15. Supplementary Notes This report is hased on studies performed at Lincoln Laboratory, a center for research operated hy Massachusetts Institute of Technology. The work was sponsored hy the Air Force under Contract Fl9628-90-C-0002. 16. Abstract The Federal Aviation Administration (FAA) Integrated Terminal Weather System (ITWS) is supporting the development of weather products important for air traffic control in the terminal area. -
Observation of Present and Past Weather; State of the Ground
CHAPTER CONTENTS Page CHAPTER 14. OBSERVATION OF PRESENT AND PAST WEATHER; STATE OF THE GROUND .. 450 14.1 General ................................................................... 450 14.1.1 Definitions ......................................................... 450 14.1.2 Units and scales ..................................................... 450 14.1.3 Meteorological requirements ......................................... 451 14.1.4 Observation methods. 451 14.2 Observation of present and past weather ...................................... 451 14.2.1 Precipitation. 452 14.2.1.1 Objects of observation ....................................... 452 14.2.1.2 Instruments and measuring devices: precipitation type ........... 452 14.2.1.3 Instruments and measuring devices: precipitation intensity and character ............................................... 454 14.2.1.4 Instruments and measuring devices: multi-sensor approach ....... 455 14.2.2 Atmospheric obscurity and suspensoids ................................ 455 14.2.2.1 Objects of observation ....................................... 455 14.2.2.2 Instruments and measuring devices for obscurity and suspensoid characteristics .................................... 455 14.2.3 Other weather events ................................................ 456 14.2.3.1 Objects of observation ....................................... 456 14.2.3.2 Instruments and measuring devices. 457 14.2.4 State of the sky ...................................................... 457 14.2.4.1 Objects of observation ......................................