Ship-Based Contributions to Global Ocean, Weather, and Climate Observing Systems
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Comparing Historical and Modern Methods of Sea Surface Temperature
EGU Journal Logos (RGB) Open Access Open Access Open Access Advances in Annales Nonlinear Processes Geosciences Geophysicae in Geophysics Open Access Open Access Natural Hazards Natural Hazards and Earth System and Earth System Sciences Sciences Discussions Open Access Open Access Atmospheric Atmospheric Chemistry Chemistry and Physics and Physics Discussions Open Access Open Access Atmospheric Atmospheric Measurement Measurement Techniques Techniques Discussions Open Access Open Access Biogeosciences Biogeosciences Discussions Open Access Open Access Climate Climate of the Past of the Past Discussions Open Access Open Access Earth System Earth System Dynamics Dynamics Discussions Open Access Geoscientific Geoscientific Open Access Instrumentation Instrumentation Methods and Methods and Data Systems Data Systems Discussions Open Access Open Access Geoscientific Geoscientific Model Development Model Development Discussions Open Access Open Access Hydrology and Hydrology and Earth System Earth System Sciences Sciences Discussions Open Access Ocean Sci., 9, 683–694, 2013 Open Access www.ocean-sci.net/9/683/2013/ Ocean Science doi:10.5194/os-9-683-2013 Ocean Science Discussions © Author(s) 2013. CC Attribution 3.0 License. Open Access Open Access Solid Earth Solid Earth Discussions Comparing historical and modern methods of sea surface Open Access Open Access The Cryosphere The Cryosphere temperature measurement – Part 1: Review of methods, Discussions field comparisons and dataset adjustments J. B. R. Matthews School of Earth and Ocean Sciences, University of Victoria, Victoria, BC, Canada Correspondence to: J. B. R. Matthews ([email protected]) Received: 3 August 2012 – Published in Ocean Sci. Discuss.: 20 September 2012 Revised: 31 May 2013 – Accepted: 12 June 2013 – Published: 30 July 2013 Abstract. Sea surface temperature (SST) has been obtained 1 Introduction from a variety of different platforms, instruments and depths over the past 150 yr. -
International Agencies O World Meteorological Organization (Https
International Agencies o World Meteorological Organization (https://www.wmo.int/pages/index_en.html) o WMO Regional Climate Centers (http://www.wmo.int/pages/prog/wcp/wcasp/rcc/rcc.php) o World Air Quality Index (http://waqi.info) o International Research Institute for Climate and Society (https://iri.columbia.edu/) o Climate Research Institute (http://www.cru.uea.ac.uk) o Australia Bureau of Meteorology (http://www.bom.gov.au) o Cooperative Institute for Meteorological Studies (http://cimss.ssec.wisc.edu) U.S. Agencies National Centers for Environmental prediction (https://www.ncep.noaa.gov) o Aviation Weather Center (https://aviationweather.gov o Climate Prediction Center (http://www.cpc.noaa.gov) o Environmental Modeling Center (http://www.emc.ncep.noaa.gov) o National Hurricane Center (www.nhc.noaa.gov) o Ocean Prediction Center (http://www.opc.ncep.noaa.gov) o Space Weather Prediction Center (https://www.swpc.noaa.gov) o Storm Prediction Center (www.spc.noaa.gov) o Weather Prediction Center (www.wpc.ncep.noaa.gov) National Oceanic and Atmospheric Administration (https://noaa.gov) National Centers for Environmental Prediction (https://www.ngdc.noaa.gov) Formerly National Geophysical Data Center and National Climate Data Center National Severe Storms Laboratory (http://www.nssl.noaa.gov/) National Snow and Ice Data Center (http://nsidc.org/) National Operational Hydrologic Remote Sensing Center (www.nohrsc.noaa.gov) National Drought Mitigation Center (https://drought.unl.edu/) National Environmental Satellite, Data, & Information Service -
Worldwide Marine Radiofacsimile Broadcast Schedules
WORLDWIDE MARINE RADIOFACSIMILE BROADCAST SCHEDULES U.S. DEPARTMENT OF COMMERCE NATIONAL OCEANIC and ATMOSPHERIC ADMINISTRATION NATIONAL WEATHER SERVICE January 14, 2021 INTRODUCTION Ships....The U.S. Voluntary Observing Ship (VOS) program needs your help! If your ship is not participating in this worthwhile international program, we urge you to join. Remember, the meteorological agencies that do the weather forecasting cannot help you without input from you. ONLY YOU KNOW THE WEATHER AT YOUR POSITION!! Please report the weather at 0000, 0600, 1200, and 1800 UTC as explained in the National Weather Service Observing Handbook No. 1 for Marine Surface Weather Observations. Within 300 nm of a named hurricane, typhoon or tropical storm, or within 200 nm of U.S. or Canadian waters, also report the weather at 0300, 0900, 1500, and 2100 UTC. Your participation is greatly appreciated by all mariners. For assistance, contact a Port Meteorological Officer (PMO), who will come aboard your vessel and provide all the information you need to observe, code and transmit weather observations. This publication is made available via the Internet at: https://weather.gov/marine/media/rfax.pdf The following webpage contains information on the dissemination of U.S. National Weather Service marine products including radiofax, such as frequency and scheduling information as well as links to products. A listing of other recommended webpages may be found in the Appendix. https://weather.gov/marine This PDF file contains links to http pages and FTPMAIL commands. The links may not be compatible with all PDF readers and e-mail systems. The Internet is not part of the National Weather Service's operational data stream and should never be relied upon as a means to obtain the latest forecast and warning data. -
The Unnamed Atlantic Tropical Storms of 1970
944 MONTHLY WEATHER REVIEW Vol. 99, No. 12 UDC 551.515.23:661.507.35!2:551.607.362.2(261) “1970.08-.lo” THE UNNAMED ATLANTIC TROPICAL STORMS OF 1970 DAVID B. SPIEGLER Allied Research Associates, Inc., Concord, Mass. ABSTRACT A detailed analysis of conventional and aircraft reconnaissance data and satellite pictures for two unnamed Atlantic Ocean cyclones during 1970 indicates that the stqrms were of tropical nature and were probably of at least minimal hurricane intensity for part of their life history. Prior to becoming a hurricane, one of the storms exhibited characteristics not typical of any of the recognized classical cyclone types [i.e., tropical, extratropical, and subtropical (Kona)]. The implications of this are discussed and the concept of semitropical cyclones as a separate cyclone category is advanced. 6. INTRODUCTION ing recognition of hybrid-type storms provides additional support for the recommendation. During the 1970 tropical cyclone season, tn7o storms occurred that were not given names at the time. The 2. UNNAMED STORM NO. I-AUG. Q3-$8, 6970 National Hurricane Center (NHC) monitored their prog- ress and issued bulletins throughout their life history but A mell-organized tropical disturbance noted on satellite they mere not officially recognized as tropical cyclones of pictures during August 8, south of the Cape Verde Islands tropical storm or hurricane intensity. In their annual post- in the far eastern tropical Atlantic, intensified to ti strong season summary of the hurricane season, NHC discusses depression as it moved westmarcl. On Thursday, August 13, these storms in some detail (Simpson and Pelissier 1971) some further intensification of the system appeared to be but thej- are not presently included in the official list of taking place while the depression was about 250 mi 1970 tropical storms. -
NWS Unified Surface Analysis Manual
Unified Surface Analysis Manual Weather Prediction Center Ocean Prediction Center National Hurricane Center Honolulu Forecast Office November 21, 2013 Table of Contents Chapter 1: Surface Analysis – Its History at the Analysis Centers…………….3 Chapter 2: Datasets available for creation of the Unified Analysis………...…..5 Chapter 3: The Unified Surface Analysis and related features.……….……….19 Chapter 4: Creation/Merging of the Unified Surface Analysis………….……..24 Chapter 5: Bibliography………………………………………………….…….30 Appendix A: Unified Graphics Legend showing Ocean Center symbols.….…33 2 Chapter 1: Surface Analysis – Its History at the Analysis Centers 1. INTRODUCTION Since 1942, surface analyses produced by several different offices within the U.S. Weather Bureau (USWB) and the National Oceanic and Atmospheric Administration’s (NOAA’s) National Weather Service (NWS) were generally based on the Norwegian Cyclone Model (Bjerknes 1919) over land, and in recent decades, the Shapiro-Keyser Model over the mid-latitudes of the ocean. The graphic below shows a typical evolution according to both models of cyclone development. Conceptual models of cyclone evolution showing lower-tropospheric (e.g., 850-hPa) geopotential height and fronts (top), and lower-tropospheric potential temperature (bottom). (a) Norwegian cyclone model: (I) incipient frontal cyclone, (II) and (III) narrowing warm sector, (IV) occlusion; (b) Shapiro–Keyser cyclone model: (I) incipient frontal cyclone, (II) frontal fracture, (III) frontal T-bone and bent-back front, (IV) frontal T-bone and warm seclusion. Panel (b) is adapted from Shapiro and Keyser (1990) , their FIG. 10.27 ) to enhance the zonal elongation of the cyclone and fronts and to reflect the continued existence of the frontal T-bone in stage IV. -
Automated Underway Oceanic and Atmospheric Measurements from Ships
AUTOMATED UNDERWAY OCEANIC AND ATMOSPHERIC MEASUREMENTS FROM SHIPS Shawn R. Smith (1), Mark A. Bourassa (1), E. Frank Bradley (2), Catherine Cosca (3), Christopher W. Fairall (4), Gustavo J. Goni (5), John T. Gunn (6), Maria Hood (7), Darren L. Jackson (8), Elizabeth C. Kent (9), Gary Lagerloef (6), Philip McGillivary (10), Loic Petit de la Villéon (11), Rachel T. Pinker (12), Eric Schulz (13), Janet Sprintall (14), Detlef Stammer (15), Alain Weill (16), Gary A. Wick (17), Margaret J. Yelland (9) (1) Center for Ocean-Atmospheric Prediction Studies, Florida State University, Tallahassee, FL 32306-2840, USA, Emails: [email protected], [email protected] (2) CSIRO Land and Water, PO Box 1666, Canberra, ACT 2601, AUSTRALIA, Email: [email protected] (3) NOAA/PMEL, 7600 Sand Point Way NE, Seattle, WA 98115, USA, Email: [email protected] (4) NOAA/ESRL/PSD, R/PSD3, 325 Broadway, Boulder, CO 80305-3328, USA, Email: [email protected] (5) USDC/NOAA/AOML/PHOD, 4301 Rickenbacker Causeway, Miami, FL 33149, USA, Email: [email protected] (6) Earth and Space Research, 2101 Fourth Ave., Suite 1310, Seattle, WA, 98121, USA, Emails: [email protected], [email protected] (7) Intergovernmental Oceanographic Commission UNESCO, 1, rue Miollis, 75732 Paris Cedex 15, FRANCE, Email: [email protected] (8) Cooperative Institute for Research in Environmental Sciences, NOAA/ESRL/PSD, 325 Broadway, R/PSD2, Boulder, CO 80305, USA, Email: [email protected] (9) National Oceanography Centre, European Way, Southampton, SO14 3ZH, UK, Emails: [email protected], -
'Service Assessment': Hurricane Isabel September 18-19, 2003
Service Assessment Hurricane Isabel September 18-19, 2003 U.S. DEPARTMENT OF COMMERCE National Oceanic and Atmospheric Administration National Weather Service Silver Spring, Maryland Cover: Moderate Resolution Imaging Spectroradiometer (MODIS) Rapid Response Team imagery, NASA Goddard Space Flight Center, 1555 UTC September 18, 2003. Service Assessment Hurricane Isabel September 18-19, 2003 May 2004 U.S. DEPARTMENT OF COMMERCE Donald L. Evans, Secretary National Oceanic and Atmospheric Administration Vice Admiral Conrad C. Lautenbacher, Jr., U.S. Navy (retired), Administrator National Weather Service Brigadier General David L. Johnson, U.S. Air Force (Retired), Assistant Administrator Preface The hurricane is one of the most potentially devastating natural forces. The potential for disaster increases as more people move to coastlines and barrier islands. To meet the mission of the National Oceanic and Atmospheric Administration’s (NOAA) National Weather Service (NWS) - provide weather, hydrologic, and climatic forecasts and warnings for the protection of life and property, enhancement of the national economy, and provide a national weather information database - the NWS has implemented an aggressive hurricane preparedness program. Hurricane Isabel made landfall in eastern North Carolina around midday Thursday, September 18, 2003, as a Category 2 hurricane on the Saffir-Simpson Hurricane Scale (Appendix A). Although damage estimates are still being tabulated as of this writing, Isabel is considered one of the most significant tropical cyclones to affect northeast North Carolina, east central Virginia, and the Chesapeake and Potomac regions since Hurricane Hazel in 1954 and the Chesapeake-Potomac Hurricane of 1933. Hurricane Isabel will be remembered not for its intensity, but for its size and the impact it had on the residents of one of the most populated regions of the United States. -
Section 5 Development of and Studies with Regional and Smaller-Scale
Section 5 Development of and studies with regional and smaller-scale atmospheric models, regional ensemble forecasting Verification of mesoscale forecasts by a high resolution non-hydrostatic model at JMA Kohei Aranami and Tomonori Segawa Numerical Prediction Division, 1-3-4 Otemachi, Chiyoda-ku, Tokyo 100-8122, Japan E-mail: [email protected], [email protected] 1 Introduction etary boundary layer is reduced to be half of 10km- Japan Meteorological Agency (JMA) started op- NHM. The horizontal mixing length is reduced to erating a mesoscale numerical weather prediction the same value of that of vertical. system for disaster prevention in March 2001 us- The Kessler-type conversion threshold from con- ing a hydrostatic model (MSM) with a horizon- vective condensate to precipitation is increased tal resolution 10 km. A non-hydrostatic model and life times of deep and shallow convection are (JMANHM, Saito et al., 2006, hereafter 10km- changed in the Kain Fritsch cumulus parameteri- NHM) has been operating since September 2004 zation scheme (Kain and Fritsch, 1993) that affects with the same horizontal resolution. The horizon- greatly the accuracy of precipitation forecasts. tal resolution is planned to be enhanced to 5 km 3 Verification results (5km-NHM) in March 2006 on the new computer In this section, the performance of 5km-NHM is system of JMA. shown in terms of statistical verification scores in 2 Specifications of 5km-NHM comparison with 10km-NHM for the period of June In this section, the specifications which are to July in 2004 and January to February in 2005. -
The Aerograph Will Be Mailed the First of September
Before I get started with whatever it is I am going to say, I have an important bit of information for you. "AFTER TALKING WITH JIM STONE AND GETTING CONCURRENCE FROM THE PRESIDENT, THERE IS GOING TO BE A CHANGE IN THE DATES FOR THE AUGUST AEROGRAPH. SINCE INPUT WAS DUE BY JULY 15TH AND THE REUNION WON'T BE OVER TILL JULY 24TH, THE DATES FOR THE AUGUST AEROGRAPH WILL BE MOVED FORWARD ONE MONTH. I WILL NEED YOUR INPUT BY AUGUST 15TH AND THE AEROGRAPH WILL BE MAILED THE FIRST OF SEPTEMBER. THIS WILL ACCOMMODATE BEING ABLE TO PRINT THE MINUTES FROM THE EXECUTIVE AND GENERAL MEETINGS OF THE 19TH REUNION." ----------------------------------------------------------------------------------------------------------------------------- ------------------------------------- In the last issue I said I would be in my new office and would have looked up and different subjects that we have asked for articles on, and print them in this issue. Well, I was partly right. I did get the office built in the garage but, for what-ever reason, I haven't gotten to the past issues to check on subject material. IT WILL BE IN THE MAY ISSUE. ----------------------------------------------------------------------------------------------------------------------------- ------------------------------------- It seems as though everyone is asking for money these days, and NWSA is right in their pitching. Jim Stone has an article asking for a small donation to pay for the new computer the association just purchased for the Secretary/Treasurer. Jim mentioned in this issue that these donations are tax deductible. President Roby mentioned in his article that, due to low interest rates, we might be limited in our giving of scholarships this year. -
Regional Science Centers and Related Labs and Field Stations
NOAA’s National Weather Service (NWS) In Your Neighborhood Facilities National Support and Specialized Centers Alaska Aviation Weather Unit (AAWU) – Anchorage, AK AAWU provides en-route aviation weather forecasts and warnings for all of Alaska. The Unit also includes the Volcanic Ash Advisory Center for the North Pacific, which provides worldwide warnings and advisories to aviation interests regarding volcanic ash hazards. Central Pacific Hurricane Center (CPHC) – Honolulu, HI CPHC issues tropical cyclone warnings, watches, advisories, discussions, and statements for all tropical cyclones in the Central Pacific. Hydrologic Information Center (HIC) – Silver Spring, MD HIC provides real-time updates of current hydrologic conditions, flood watches & warnings, river forecasts, droughts, and related information. NOAA’s Office of Legislative Affairs Tel: 202-482-4981 http://www.legislative.noaa.gov March 2008 1 Hydrologic Research Laboratory (HRL) – Silver Spring, MD HRL conducts studies, investigations and analyses leading to the application of new scientific and computer technologies for hydrologic forecasting and related water resources problems. National Centers for Environmental Prediction (NCEP) – Camp Springs, MD NCEP gives overarching management to nine centers, which include the: • Aviation Weather Center (AWC) – Kansas City, MO: The AWC provides aviation warnings and forecasts of hazardous flight conditions at all levels within domestic and international air space. • Climate Prediction Center (CPC) – Camp Springs, MD: The CPC monitors and forecasts short-term climate fluctuations and provides information on the effects climate patterns can have on the nation. • Environmental Modeling Center (EMC) - Camp Springs, MD: The EMC develops and improves numerical weather, climate, hydrological and ocean prediction through a broad program in partnership with the research community. -
6A.4 the National Weather Service Unified Surface Analysis
6A.4 THE NATIONAL WEATHER SERVICE UNIFIED SURFACE ANALYSIS Robbie Berg* NWS/NCEP/National Hurricane Center, Miami, FL James Clark NWS/NCEP/Ocean Prediction Center, Camp Springs, MD David Roth NWS/NCEP/Hydrometeorological Prediction Center, Camp Springs, MD Thomas Birchard NWS/Honolulu Forecast Office, Honolulu, HI 1. INTRODUCTION 2. HISTORY The Unified Surface Analysis is a near- For several decades, various offices within hemispheric surface analysis created every six the NWS and its predecessor the U. S. Weather hours at the four synoptic times and produced by Bureau produced separate surface analyses which four different offices within the U. S. National covered geographic areas important to their Weather Service—the Hydrometeorological forecast and warning operations. These analyses Prediction Center (HPC), the Ocean Prediction usually overlapped and led to a duplication of Center (OPC), the National Hurricane Center effort by the offices—and often brought confusion (NHC), and the Honolulu Weather Forecast Office to users who would see features analyzed (HFO). While each office produces separate differently from office to office. To remedy this analyses to suit their own operational needs and redundancy, the various analysis centers agreed objectives, a process is in place whereby a to limit their analyses to their respective areas of collaboration between the four offices results in responsibility and to combine them to create one one seamless analysis covering an area of seamless Unified Surface Analysis covering much 177,106,111 km 2 , or about 70% of the Northern of the Northern Hemisphere (Figure 1). This effort Hemisphere. was intended to make the entire process more Users of any of the various surface efficient and to allow each center to bring its own analyses produced within the NWS may not be particular regional and meteorological expertise to aware that all contain contributions from the other the analysis process. -
Oceanic Cyclone Analysis and Forecasting at the NCEP/Ocean Prediction Center: the Role of Observations & Progress in Medium Range Forecasting
Oceanic Cyclone Analysis and Forecasting at the NCEP/Ocean Prediction Center: The Role of Observations & Progress in Medium Range Forecasting James D Clark – National Center for Environmental Prediction, Camp Springs, MD 1. Introduction The Ocean Prediction Center’s (OPC) primary responsibility is the issuance of marine warnings, forecasts, and guidance in both text and graphical formats for maritime users over the Northern hemisphere Atlantic and Pacific marine areas extending from 20°N to 67°N for purposes of protection of life and property, safety at sea, and the enhancement of economic opportunity. In addition, these forecast products fulfill the US obligations under the World Meteorological Organization and Safety of Life at Sea Convention. A brief summary of US National Weather Service marine and coastal weather services and OPC forecast operations will be given in section two. This paper emphasizes OPC’s handling of atmospheric and oceanographic observations over the data sparse oceans from a fore - caster’s perspective, specifically, the visualization techniques utilized to rapidly determine model initialization errors, model trends, and global model differences. Examples focusing on the use of observations in the forecast and verification of extreme events will be presented in the third portion. The fourth section of this paper centers on the recent progress made in medium range forecasting at OPC, including warning criteria probabilities through the use of the NCEP Global Ensemble Forecast System and ECMWF Ensemble Prediction System members. In the final part of this paper a summary with upcoming OPC science priorities will be offered. Fig. 1 OPC Atlantic 500 hPa analysis. Fig .