Performance of the Global Forecast System's Medium-Range
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Lesson 6 Weather: Collecting Data GRADE 3-5 BACKGROUND Meteorologists Collect Weather Data Daily to Make Forecasts
Lesson 6 Weather: Collecting Data GRADE 3-5 BACKGROUND Meteorologists collect weather data daily to make forecasts. With the aid of high altitude weather balloons, weather equipment and gauges, satellites, and computers, accurate daily forecasts can be made. Collecting weather data in just one location and making a forecast requires a great deal of skill. Since air travels from one location to another, it is helpful to know what the approaching weather will be. In this investigation, the students will collect data for two weeks. At this time they will start seeing patterns in each of the areas. They can predict what the weather will be like the next day and for the next few days. They will also write if their predictions were correct from the previous day. Collecting the data for this lesson can be done instead of collecting the data separately in lesson 1-4. BASIC LESSON Objective(s) Students will be able to… Collect data for two weeks and use the information to detect patterns and predict weather around their location. State Science Content Standard(s) Standard 4. Students through the inquiry process, demonstrate knowledge of the composition, structures, processes and interactions of Earth's systems and other objects in space. A. 4.4 Observe and describe the water cycle and the local weather and demonstrate how weather conditions are measured. A. Record temperature B. Display data on a graph C. Interpret trends and patterns of data D. Identify and explain the use of a barometer, weather vane, and anemometer E. Collect, record and chart data from each weather instrument F. -
List of Dams and Reservoirs 1 List of Dams and Reservoirs
List of dams and reservoirs 1 List of dams and reservoirs The following is a list of reservoirs and dams, arranged by continent and country. Africa Cameroon • Edea Dam • Lagdo Dam • Song Loulou Dam Democratic Republic of Congo • Inga Dam Ethiopia Gaborone Dam in Botswana. • Gilgel Gibe I Dam • Gilgel Gibe III Dam • Kessem Dam • Tendaho Irrigation Dam • Tekeze Hydroelectric Dam Egypt • Aswan Dam and Lake Nasser • Aswan Low Dam Inga Dam in DR Congo. Ghana • Akosombo Dam - Lake Volta • Kpong Dam Kenya • Gitaru Reservoir • Kiambere Reservoir • Kindaruma Reservoir Aswan Dam in Egypt. • Masinga Reservoir • Nairobi Dam Lesotho • Katse Dam • Mohale Dam List of dams and reservoirs 2 Mauritius • Eau Bleue Reservoir • La Ferme Reservoir • La Nicolière Reservoir • Mare aux Vacoas • Mare Longue Reservoir • Midlands Dam • Piton du Milieu Reservoir Akosombo Dam in Ghana. • Tamarind Falls Reservoir • Valetta Reservoir Morocco • Aït Ouarda Dam • Allal al Fassi Dam • Al Massira Dam • Al Wahda Dam • Bin el Ouidane Dam • Daourat Dam • Hassan I Dam Katse Dam in Lesotho. • Hassan II Dam • Idriss I Dam • Imfout Dam • Mohamed V Dam • Tanafnit El Borj Dam • Youssef Ibn Tachfin Dam Mozambique • Cahora Bassa Dam • Massingir Dam Bin el Ouidane Dam in Morocco. Nigeria • Asejire Dam, Oyo State • Bakolori Dam, Sokoto State • Challawa Gorge Dam, Kano State • Cham Dam, Gombe State • Dadin Kowa Dam, Gombe State • Goronyo Dam, Sokoto State • Gusau Dam, Zamfara State • Ikere Gorge Dam, Oyo State Gariep Dam in South Africa. • Jibiya Dam, Katsina State • Jebba Dam, Kwara State • Kafin Zaki Dam, Bauchi State • Kainji Dam, Niger State • Kiri Dam, Adamawa State List of dams and reservoirs 3 • Obudu Dam, Cross River State • Oyan Dam, Ogun State • Shiroro Dam, Niger State • Swashi Dam, Niger State • Tiga Dam, Kano State • Zobe Dam, Katsina State Tanzania • Kidatu Kihansi Dam in Tanzania. -
Emulation of a Full Suite of Atmospheric Physics
Emulation of a Full Suite of Atmospheric Physics Parameterizations in NCEP GFS using a Neural Network Alexei Belochitski1;2 and Vladimir Krasnopolsky2 1IMSG, 2NOAA/NWS/NCEP/EMC email: [email protected] 1 Introduction is captured by periodic functions of day and month, and variability of solar energy output is reflected in the solar constant. In addition to the full atmospheric state, NN receives full land-surface model (LSM) state to Machine learning (ML) can be used in parameterization development at least in two different ways: 1) as an capture impact of surface boundary conditions. All NN outputs are increments of dynamical core's prognostic emulation technique for accelerating calculation of parameterizations developed previously, and 2) for devel- variables that the original atmospheric physics package modifies. opment of new \empirical" parameterizations based on reanalysis/observed data or data simulated by high resolution models. An example of the former is the paper by Krasnopolsky et al. (2012) who have developed highly efficient neural network (NN) emulations of both long{ and short-wave radiation parameterizations for 4 Hybrid Coupling of Full Atmospheric Physics NN to GFS a high resolution state-of-the-art short{ to medium-range weather forecasting model. More recently, Gentine Full atmospheric physics NN only et al. (2018) have used a neural network to emulate 2D cloud resolving models (CRMs) embedded into columns updates the state of the atmo- of a \super-parameterized" general circulation model (GCM) in an aqua-planet configuration with prescribed sphere and does not update the invariant zonally symmetric SST, full diurnal cycle, and no annual cycle. -
Radar Derived Rainfall and Rain Gauge Measurements at SRS
Radar Derived Rainfall and Rain Gauge Measurements at SRS A. M. Rivera-Giboyeaux February 2020 SRNL-STI-2019-00644, Revision 0 SRNL-STI-2019-00644 Revision 0 DISCLAIMER This work was prepared under an agreement with and funded by the U.S. Government. Neither the U.S. Government or its employees, nor any of its contractors, subcontractors or their employees, makes any express or implied: 1. warranty or assumes any legal liability for the accuracy, completeness, or for the use or results of such use of any information, product, or process disclosed; or 2. representation that such use or results of such use would not infringe privately owned rights; or 3. endorsement or recommendation of any specifically identified commercial product, process, or service. Any views and opinions of authors expressed in this work do not necessarily state or reflect those of the United States Government, or its contractors, or subcontractors. Printed in the United States of America Prepared for U.S. Department of Energy ii SRNL-STI-2019-00644 Revision 0 Keywords: Rainfall, Radar, Rain Gauge, Measurements Retention: Permanent Radar Derived Rainfall and Rain Gauge Measurements at SRS A. M. Rivera-Giboyeaux February 2020 Prepared for the U.S. Department of Energy under contract number DE-AC09-08SR22470. iii SRNL-STI-2019-00644 Revision 0 REVIEWS AND APPROVALS AUTHORS: ______________________________________________________________________________ A. M. Rivera-Giboyeaux, Atmospheric Technologies Group, SRNL Date TECHNICAL REVIEW: ______________________________________________________________________________ S. Weinbeck, Atmospheric Technologies Group, SRNL. Reviewed per E7 2.60 Date APPROVAL: ______________________________________________________________________________ C.H. Hunter, Manager Date Atmospheric Technologies Group iv SRNL-STI-2019-00644 Revision 0 EXECUTIVE SUMMARY Over the years rainfall data for the Savannah River Site has been obtained from ground level measurements made by rain gauges. -
COOP Observer Manual (1).Pdf
National Weather Service WFO Mount Holly, NJ Cooperative Observation Program Observer Manual Updated: October 3, 2020 Table of Contents 1. Taking Observations a. Rainfall/Liquid Equivalent Precipitation i. Rainfall 1. Standard 8” Rain Gauge 2. Plastic 4” Rain Gauge ii. Snowfall/Frozen Precipitation Liquid Equivalent 1. Standard 8” Rain Gauge 2. Plastic 4” Rain Gauge b. Snowfall c. Snow Depth d. Maximum and Minimum Temperatures (if equipped) i. Digital Maximum/Minimum Sensor with Nimbus Display ii. Cotton Region Shelter with Liquid-in-Glass Thermometers 2. Reporting Observations a. WxCoder b. Things to Remember 1 1. Taking Observations Measuring precipitation is one of the most basic and useful forms of weather observations. It is important to note that observations will vary based on the type of precipitation that is expected to occur. If any frozen precipitation is forecast, it is important to remove the funnel top and inner tube from your gauge before precipitation begins. This will prevent damage to the equipment and ensure the most accurate measurements possible. Note that the inner tube of the rain gauge only holds a certain amount of precipitation until it begins to overflow into the outer can. If rain falls, but is not measurable inside of the gauge, this should be reported as a Trace (T) of rainfall. This includes sprinkles/drizzle and occurrences where there is some liquid in the inner tube, but it is not measurable on the measuring stick. During the cold season (generally November through early April), we recommend that observers leave their snowboards outside at all times, if possible. -
INTEGRATED FORECAST and MANAGEMENT in NORTHERN CALIFORNIA – INFORM a Demonstration Project
CPASW March 23, 2006 INTEGRATED FORECAST AND MANAGEMENT IN NORTHERN CALIFORNIA – INFORM A Demonstration Project Present: Eylon Shamir HYDROLOGIC RESEARCH CENTER GEORGIA WATER RESOURCES INSTITUTE Eylon Shamir: [email protected] www.hrc-web.org INFORM: Integrated Forecast and Management in Northern California Hydrologic Research Center & Georgia Water Resources Institute Sponsors: CALFED Bay Delta Authority California Energy Commission National Oceanic and Atmospheric Administration Collaborators: California Department of Water Resources California-Nevada River Forecast Center Sacramento Area Flood Control Agency U.S. Army Corps of Engineers U.S. Bureau of Reclamation Eylon Shamir: [email protected] www.hrc-web.org Vision Statement Increase efficiency of water use in Northern California using climate, hydrologic and decision science Eylon Shamir: [email protected] www.hrc-web.org Goal and Objectives Demonstrate the utility of climate and hydrologic forecasts for water resources management in Northern California Implement integrated forecast-management systems for the Northern California reservoirs using real-time data Perform tests with actual data and with management input Eylon Shamir: [email protected] www.hrc-web.org Major Resevoirs in Nothern California Application Area 41.5 Sacramen to River Capacity of Major Reservoirs 41 (million acre-feet): Pit River Trinit y Trinity - 2.4 Trinity Shasta 40.5 Trinity River Shasta Shasta - 4.5 Oroville - 3.5 Feather River 40 Folsom - 1 39.5 Degrees North Latitude Oroville Oroville N. -
METAR/SPECI Reporting Changes for Snow Pellets (GS) and Hail (GR)
U.S. DEPARTMENT OF TRANSPORTATION N JO 7900.11 NOTICE FEDERAL AVIATION ADMINISTRATION Effective Date: Air Traffic Organization Policy September 1, 2018 Cancellation Date: September 1, 2019 SUBJ: METAR/SPECI Reporting Changes for Snow Pellets (GS) and Hail (GR) 1. Purpose of this Notice. This Notice coincides with a revision to the Federal Meteorological Handbook (FMH-1) that was effective on November 30, 2017. The Office of the Federal Coordinator for Meteorological Services and Supporting Research (OFCM) approved the changes to the reporting requirements of small hail and snow pellets in weather observations (METAR/SPECI) to assist commercial operators in deicing operations. 2. Audience. This order applies to all FAA and FAA-contract weather observers, Limited Aviation Weather Reporting Stations (LAWRS) personnel, and Non-Federal Observation (NF- OBS) Program personnel. 3. Where can I Find This Notice? This order is available on the FAA Web site at http://faa.gov/air_traffic/publications and http://employees.faa.gov/tools_resources/orders_notices/. 4. Cancellation. This notice will be cancelled with the publication of the next available change to FAA Order 7900.5D. 5. Procedures/Responsibilities/Action. This Notice amends the following paragraphs and tables in FAA Order 7900.5. Table 3-2: Remarks Section of Observation Remarks Section of Observation Element Paragraph Brief Description METAR SPECI Volcanic eruptions must be reported whenever first noted. Pre-eruption activity must not be reported. (Use Volcanic Eruptions 14.20 X X PIREPs to report pre-eruption activity.) Encode volcanic eruptions as described in Chapter 14. Distribution: Electronic 1 Initiated By: AJT-2 09/01/2018 N JO 7900.11 Remarks Section of Observation Element Paragraph Brief Description METAR SPECI Whenever tornadoes, funnel clouds, or waterspouts begin, are in progress, end, or disappear from sight, the event should be described directly after the "RMK" element. -
5Th International Conference on Reanalysis (ICR5)
5th International Conference on Reanalysis (ICR5) 13–17 November 2017, Rome IMPLEMENTED BY Contents ECMWF | 5th International Conference on Reanalysis (ICR5) 2017 2 Introduction It is our pleasure to welcome the Climate research has benefited over the • Status and plans for future reanalyses • Evaluation of reanalyses reanalysis community at the 5th years from the continuing development Global and regional production, inclusive Comparisons with observations, International Conference on Reanalysis of reanalysis. As reanalysis datasets of all WCRP thematic areas: atmosphere, other types of analysis and models, (ICR5). We are delighted that we are become more diverse (atmosphere, land, ocean and cryosphere – Session inter-comparisons, diagnostics – all able to come together in Rome. ocean and land components), more organisers: Mike Bosilovich (NASA Session organisers: Franco Desiato This five-day international conference complete (moving towards Earth-system GMAO), Shinya Kobayashi (JMA), (ISPRA), Masatomo Fujiwara (Hokkaido is the worldwide leading event for the coupled reanalysis), more detailed, and Simona Masina (CMCC) University), Sonia Seneviratne (ETH), continuing development of reanalysis of longer timespan, community efforts Adrian Simmons (ECMWF) • Observations for reanalyses for climate research, which provides a to evaluate and intercompare them Preparation, organisation in large • Applications of reanalyses comprehensive numerical description become more important. archives, data rescue, reanalysis Generating time-series of Essential -
Evaluation of Cloud Properties in the NOAA/NCEP Global Forecast System Using Multiple Satellite Products
Clim Dyn DOI 10.1007/s00382-012-1430-0 Evaluation of cloud properties in the NOAA/NCEP global forecast system using multiple satellite products Hyelim Yoo • Zhanqing Li Received: 15 July 2011 / Accepted: 19 June 2012 Ó Springer-Verlag 2012 Abstract Knowledge of cloud properties and their vertical are similar to those from the model, latitudinal variations structure is important for meteorological studies due to their show discrepancies in terms of structure and pattern. The impact on both the Earth’s radiation budget and adiabatic modeled cloud optical depth over storm track region and heating within the atmosphere. The objective of this study is to subtropical region is less than that from the passive sensor and evaluate bulk cloud properties and vertical distribution sim- is overestimated for deep convective clouds. The distributions ulated by the US National Oceanic and Atmospheric of ice water path (IWP) agree better with satellite observations Administration National Centers for Environmental than do liquid water path (LWP) distributions. Discrepancies Prediction Global Forecast System (GFS) using three global in LWP/IWP distributions between observations and the satellite products. Cloud variables evaluated include the model are attributed to differences in cloud water mixing ratio occurrence and fraction of clouds in up to three layers, cloud and mean relative humidity fields, which are major control optical depth, liquid water path, and ice water path. Cloud variables determining the formation of clouds. vertical structure data are retrieved from both active (Cloud- Sat/CALIPSO) and passive sensors and are subsequently Keywords Cloud fraction Á NCEP global forecast system Á compared with GFS model results. -
Response to Comments the Authors Thank the Reviewers for Their
Response to comments The authors thank the reviewers for their constructive comments, which provide the basis to improve the quality of the manuscript and dataset. We address all points in detail and reply to all comments here below. We also updated SCDNA from V1 to V1.1 on Zenodo based on the reviewer’s comments. The modifications include adding station source flag, adding original files for location merged stations, and adding a quality control procedure based on the final SCDNA. SCDNA estimates are generally consistent between the two versions, with the total number of stations reduced from 27280 to 27276. Reviewer 1 General comment The manuscript presents and advertises a very interesting dataset of temperature and precipitation observation collected over several years in North America. The work is certainly well suited for the readership of ESSD and it is overall very important for the meteorological and climatological community. Furthermore, creation of quality controlled databases is an important contribution to the scientific community in the age of data science. I have a few points to consider before publication, which I recommend, listed below. 1. Measurement instruments: from my background, I am much closer to the instruments themselves (and their peculiarities and issues), as hardware tools. What I missed here was a description of the stations and their instruments. Questions like: which are the instruments deployed in the stations? How is precipitation measured (tipping buckets? buckets? Weighing gauges? Note for example that some instruments may have biases when measuring snowfall while others may not)? How is it temperature measured? How is this different from station to station in your database? Response: We have added the descriptions of measurement instruments in both the manuscript and dataset documentation. -
The Spacio-Temporal Changes of Kiri Dam and Its Implications” in Adamawa State, Nigeria
International Journal of Scientific and Research Publications, Volume 8, Issue 8, August 2018 469 ISSN 2250-3153 “The Spacio-Temporal Changes of Kiri Dam and Its Implications” In Adamawa State, Nigeria. B. L. Gadiga and I. D. Garandi Department of Geography, Adamawa State University, Mubi, Adamawa State, Nigeria [email protected]/[email protected] +2348064306660 [email protected] +2348030790726 DOI: 10.29322/IJSRP.8.8.2018.p8058 http://dx.doi.org/10.29322/IJSRP.8.8.2018.p8058 ABSTRACT This study focuses on the assessment of the spatial and temporal changes of Kiri lake between 1984 and 2016. The study used both geo-information techniques and field survey to carry out analysis on the spatial as well as the changes in the depth of the lake. Landsat TM and OLI of 1984 and 2016 respectively were digitized in order to determine the extent of surface area changes that has occurred. Field method was used in determining changes in the depth of the lake. The results revealed that the lake has reduced in both surface area and depth. The surface area of the lake in 1984 was 100.3 m2 which reduced to 57.0 m2 in 2016. This means that the surface area of the lake has reduced by 43% within the period of 32 years whereas the depth has reduced by more than half of its original depth. The original depth of which was 20 m has reduced to an average depth of 8.48 m. This revealed that an average siltation of 11.52 m has occurred within the period under study. -
HIRLAM-B Review September 2016
External review of the HIRLAM-B programme 2011 – 2015 Peter Lynch Dominique Marbouty Tiziana Paccagnella September 2015 External review of the HIRLAM-B programme, September 2015 Page 2 Table of contents List of recommendations page 4 Summary page 5 Part one Introduction page 7 Background to the review Composition of the Review Team and its organisation Part two The HIRLAM programme page 10 Structure and governance of the programme Staffing resources Achievements of the HIRLAM-B programme Recommendations of the previous review, follow-up Part three Model performance, forecasters’ feedback page 17 Part four Towards an expanded programme page 22 Scope of the single Consortium, core and optional activities Organisation and governance Staffing resources and code-development Data policy and code ownership Branding of the new collaboration and system Part five Conclusion page33 Annexes page 35 Annex 1 – Scope and Term of Reference for HIRLAM-B External Review Annex 2 – Joint HIRLAM-ALADIN Declaration Annex 3 – List of acronyms External review of the HIRLAM-B programme, September 2015 Page 3 Summary The Review Team appointed by the HIRLAM Council examined the governance, resources and achievement of the HIRLAM-B programme. It reviewed the implementation of the recommendations made by the previous review team in 2010 at the end of HIRLAM-A. The HIRLAM cooperation has a long history and is now well organised. As a result the Review Team made few comments concerning HIRLAM in isolation from the wider collaboration with ALADIN. The review team also met forecasters in most of HIRLAM centers. Benefits of using regional high resolution model for short range forecasts, as compared to ECMWF global forecasts, is no longer questioned.