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Libros sobre el tema "Wind Forecasts"

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Publicado: 11 de marzo de 2023

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1

G, Benjamin Stanley y Forecast Systems Laboratory (U.S.), eds. A study of the accuracy of RUC-1 and RUC-2 wind and aircraft trajectory forecasts using ACARS observations. Boulder, Colo: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Forecast Systems Laboratory, 1998.

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2

Grasping for the wind: The search for meaning in the 20th century. Grand Rapids, Mich: Zondervan, 2001.

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3

John F. Kennedy Space Center. y United States. National Aeronautics and Space Administration. Scientific and Technical Information Program., eds. Statistical short-range guidance for peak wind speed forecasts on Kennedy Space Center/Cape Canaveral Air Force Station: Phase 1 results. [Washington, D.C.]: National Aeronautics and Space Administration, Office of Management, Scientific and Technical Information Program, 2002.

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4

John F. Kennedy Space Center. y United States. National Aeronautics and Space Administration. Scientific and Technical Information Program., eds. Statistical short-range guidance for peak wind speed forecasts on Kennedy Space Center/Cape Canaveral Air Force Station: Phase 1 results. [Washington, D.C.]: National Aeronautics and Space Administration, Office of Management, Scientific and Technical Information Program, 2002.

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5

Inc, Icon Group International, ed. The 2002 world market forecasts for imported wine. San Diego, Calif: Icon Group, 2002.

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6

K, Sahai A. y Indian Institute of Tropical Meteorology., eds. Experimental seasonal forecast of Indian summer monsoon 2007: Statistical and dynamical models. Pune: Indian Institute of Tropical Meteorology, 2007.

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7

Mandke, S. K. Dynamical ensemble seasonal forecast experiments of recent Indian summer monsoons: An assessment using new approach. Pune: Indian Institute of Tropical Meteorology, 2005.

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8

Space Environment Center (U.S.), ed. Wang and Sheeley medium-range planetary A index forecast verification statistics. Boulder, Colo: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Space Environment Center, 1996.

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9

Space Environment Center (U.S.), ed. Wang and Sheeley medium-range planetary A index forecast verification statistics. Boulder, Colo: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Space Environment Center, 1996.

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10

Space Environment Center (U.S.), ed. Wang and Sheeley medium-range planetary A index forecast verification statistics. Boulder, Colo: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Space Environment Center, 1996.

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11

Space Environment Center (U.S.), ed. Wang and Sheeley medium-range planetary A index forecast verification statistics. Boulder, Colo: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Space Environment Center, 1996.

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12

Space Environment Center (U.S.), ed. Wang and Sheeley medium-range planetary A index forecast verification statistics. Boulder, Colo: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Space Environment Center, 1996.

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13

Canada Oil and Gas Lands Administration. Evaluation of wave forecasting models and forecast wind fields in the Canadian context. [Ottawa: Energy Mines and Resources], 1988.

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14

(Canada), Environmental Studies Revolving Funds. Evaluation of wave forecasting models and forecast wind fields in the Canadian context. S.l: s.n, 1988.

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15

United States. National Aeronautics and Space Administration, ed. The forecast?: Look for storms, gale-force winds, and plasma blobs. [Washington, D.C.?: National Aeronautics and Space Administration, 1998.

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16

Small, Ivory J. Forecasters handbook for extreme southwestern California based on short term climatological approximations. Salt Lake City, Utah: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, National Weather Service, Scientific Services Division, Western Region, 2006.

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17

Jones, Marcia L. A prototype expert system to forecast severe winds in the western Mediterranean Sea. Monterey, Calif: Naval Postgraduate School, 1989.

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18

Out of the blue: Wild cards and other big future surprises : how to anticipate and respond to profound change. Arlington, VA: Danielle LaPorte Book, 1997.

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19

Karlheinz, Steinmüller, ed. Wai ka xiao ying: Rang qu shi tu bian de 58 ge wei lai guan jian shi jian = Wild cards: Wenn das Unwahrscheinliche eintritt. Taibei Shi: Lian pu chu ban, 2006.

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20

K, Britton Randall, Bond Thomas H y United States. National Aeronautics and Space Administration., eds. Role of wind tunnels and computer codes in the certification and qualification of rotorcraft for flight in forecast icing. [Washington, DC]: National Aeronautics and Space Administration, 1994.

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21

K, Britton Randall, Bond Thomas H y United States. National Aeronautics and Space Administration., eds. Role of wind tunnels and computer codes in the certification and qualification of rotorcraft for flight in forecast icing. [Washington, DC]: National Aeronautics and Space Administration, 1994.

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22

executive, Health and safety. The Accuracy of Wind and Wave Forecasts. Health and Safety Executive (HSE), 1997.

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23

Performance of a High Resolution Diagnostic Model for Short Range Mesoscale Wind Forecasts in Complex Terrain. Storming Media, 2002.

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24

Statistical short-range guidance for peak wind speed forecasts on Kennedy Space Center/Cape Canaveral Air Force Station: Phase 1 results. [Washington, D.C.]: National Aeronautics and Space Administration, Office of Management, Scientific and Technical Information Program, 2002.

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25

National Aeronautics and Space Administration (NASA) Staff. Statistical Short-Range Guidance for Peak Wind Speed Forecasts on Kennedy Space Center/Cape Canaveral Air Force Station: Phase I Results. Independently Published, 2018.

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26

Group, Research. The 2000 World Market Forecasts for Imported Wine. Icon Group International, 2000.

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27

Group, The Wine Research. The 2000 World Forecasts of Wine Export Supplies (World Trade Report). 2a ed. Icon Group International, 2000.

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28

Essentials, CampingLife. Weekend Forecast Camping with a 100% Chance of Wine: Campground Logbook for Wine Lovers. Independently Published, 2021.

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29

Kindle Weather Station. kindlews.com, 2012.

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30

Notebooks, Wine Lovers Tracking. Tonight's Forecast 101 Percent Chances of Wine: Journal 6 X 9, 100 Page Wine Tracker. Independently Published, 2020.

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31

Paige, Stephanie. Weekend Forecast Camping with a Chance of Wine: Journals for Camping. Independently Published, 2018.

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32

Fatal Forecast: An Incredible True Tale of Disaster and Survival at Sea. Scribner, 2009.

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33

Tougias, Michael J. Fatal Forecast: An Incredible True Tale of Disaster and Survival at Sea. Scribner, 2007.

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34

Tougias, Michael J. Fatal Forecast: An Incredible True Tale of Disaster and Survival at Sea. Scribner, 2007.

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35

Jackquelin T. Ince Wwl Publications. Weather Forecast Logbook: A Climate Journal to Keep Track of the Weather and Record Wind and Temperature. Independently Published, 2021.

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36

Notebooks, Punny. Weekend Forecast Gardening And Wine: Funny Quotes and Pun Themed College Ruled Composition Notebook. Independently published, 2019.

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37

Wang, Bin. Intraseasonal Modulation of the Indian Summer Monsoon. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.616.

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The strongest Indian summer monsoon (ISM) on the planet features prolonged clustered spells of wet and dry conditions often lasting for two to three weeks, known as active and break monsoons. The active and break monsoons are attributed to a quasi-periodic intraseasonal oscillation (ISO), which is an extremely important form of the ISM variability bridging weather and climate variation. The ISO over India is part of the ISO in global tropics. The latter is one of the most important meteorological phenomena discovered during the 20th century (Madden & Julian, 1971, 1972). The extreme dry and wet events are regulated by the boreal summer ISO (BSISO). The BSISO over Indian monsoon region consists of northward propagating 30–60 day and westward propagating 10–20 day modes. The “clustering” of synoptic activity was separately modulated by both the 30–60 day and 10–20 day BSISO modes in approximately equal amounts. The clustering is particularly strong when the enhancement effect from both modes acts in concert. The northward propagation of BSISO is primarily originated from the easterly vertical shear (increasing easterly winds with height) of the monsoon flows, which by interacting with the BSISO convective system can generate boundary layer convergence to the north of the convective system that promotes its northward movement. The BSISO-ocean interaction through wind-evaporation feedback and cloud-radiation feedback can also contribute to the northward propagation of BSISO from the equator. The 10–20 day oscillation is primarily produced by convectively coupled Rossby waves modified by the monsoon mean flows. Using coupled general circulation models (GCMs) for ISO prediction is an important advance in subseasonal forecasts. The major modes of ISO over Indian monsoon region are potentially predictable up to 40–45 days as estimated by multiple GCM ensemble hindcast experiments. The current dynamical models’ prediction skills for the large initial amplitude cases are approximately 20–25 days, but the prediction of developing BSISO disturbance is much more difficult than the prediction of the mature BSISO disturbances. This article provides a synthesis of our current knowledge on the observed spatial and temporal structure of the ISO over India and the important physical processes through which the BSISO regulates the ISM active-break cycles and severe weather events. Our present capability and shortcomings in simulating and predicting the monsoon ISO and outstanding issues are also discussed.
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38

Chan, Johnny C. L. Physical Mechanisms Responsible for Track Changes and Rainfall Distributions Associated with Tropical Cyclone Landfall. Oxford University Press, 2017. http://dx.doi.org/10.1093/oxfordhb/9780190676889.013.16.

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As a tropical cyclone approaches land, its interaction with the characteristics of the land (surface roughness, topography, moisture availability, etc.) will lead to changes in its track as well as the rainfall and wind distributions near its landfall location. Accurate predictions of such changes are important in issuing warnings and disaster preparedness. In this chapter, the basic physical mechanisms that cause changes in the track and rainfall distributions when a tropical cyclone is about to make landfall are presented. These mechanisms are derived based on studies from both observations and idealized simulations. While the latter are relatively simple, they can isolate the fundamental and underlying physical processes that are inherent when an interaction between the land and the tropical cyclone circulation takes place. These processes are important in assessing the performance of the forecast models, and hence could help improve the model predictions and subsequently disaster preparedness.
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39

Chan, Johnny C. L. Physical Mechanisms Responsible for Track Changes and Rainfall Distributions Associated with Tropical Cyclone Landfall. Oxford University Press, 2017. http://dx.doi.org/10.1093/oxfordhb/9780190699420.013.16.

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As a tropical cyclone approaches land, its interaction with the characteristics of the land (surface roughness, topography, moisture availability, etc.) will lead to changes in its track as well as the rainfall and wind distributions near its landfall location. Accurate predictions of such changes are important in issuing warnings and disaster preparedness. In this chapter, the basic physical mechanisms that cause changes in the track and rainfall distributions when a tropical cyclone is about to make landfall are presented. These mechanisms are derived based on studies from both observations and idealized simulations. While the latter are relatively simple, they can isolate the fundamental and underlying physical processes that are inherent when an interaction between the land and the tropical cyclone circulation takes place. These processes are important in assessing the performance of the forecast models, and hence could help improve the model predictions and subsequently disaster preparedness.
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40

Strong Winds Are Forecast: A solo, 1850 mile journey by sea kayak, to every lifeboat station around Scotland. LifeAfloat Books, 2022.

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41

Phelps, Latisha. I Take Weather Cirrus: Climate Nature Earth Atmosphere Heat Wind Season Gift For Weather Forecaster Dot Grid Notebook To Write In. Independently Published, 2019.

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42

Boating, Navi. Sea Time Log for Captain: Simple Sailing Journal, Daily Log Entry for Boating, Track and Record Trip Information, Weather, Wind, Forecast, Gift for Sailors. Independently Published, 2021.

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43

Using the WSR-88D to Forecast Downburst Winds at Cape Canaveral Air Station and the Kennedy Space Center (CCAS/KSC). Storming Media, 1999.

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44

WARD, William. Cribbage Funny Cribbage and Wine Forecast: Lined for Memo Diary Journal, Perfect for School, Office and Home - 6 X 9 , 120 Pages. Independently Published, 2022.

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45

Press, Cute Malik Netball. Weekend Forecast Netball with a Chance of Wine: Netball Gifts-Cute Netball Blank Lined Notebook for Netball Lovers-perfect Gift for Valentine's Day,christmas,anniversary,birthday. Independently Published, 2020.

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46

Happens, Knit. THIS WEEKEND'S FORECAST IS MOSTLY KNITTING with a chance of wine 8.5" x 11" : Knitting Graph Paper 2 : 3 & 4: 5 Ratio for large and small projects. Independently Published, 2019.

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47

Wiek, Till. Tonight's Forecast : 99. 9% Chance of Wine: 110 Game Sheets - 660 Tic-Tac-Toe Blank Games - Soft Cover Book for Kids for Traveling & Summer Vacations - Mini Game - Clever Kids - 110 Lined Pages - 6 X 9 in - 15. 24 X 22. 86 Cm - Single Player - Funny Great Gif. Independently Published, 2019.

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48

Wiek, Till. Tonight's Forecast : 99. 9% Chance of Wine: 110 Game Sheets - 660 Tic-Tac-Toe Blank Games - Soft Cover Book for Kids for Traveling & Summer Vacations - Mini Game - Clever Kids - 110 Lined Pages - 6 X 9 in - 15. 24 X 22. 86 Cm - Single Player - Funny Great Gif. Independently Published, 2019.

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49

Tibaldi, Stefano y Franco Molteni. Atmospheric Blocking in Observation and Models. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.611.

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The atmospheric circulation in the mid-latitudes of both hemispheres is usually dominated by westerly winds and by planetary-scale and shorter-scale synoptic waves, moving mostly from west to east. A remarkable and frequent exception to this “usual” behavior is atmospheric blocking. Blocking occurs when the usual zonal flow is hindered by the establishment of a large-amplitude, quasi-stationary, high-pressure meridional circulation structure which “blocks” the flow of the westerlies and the progression of the atmospheric waves and disturbances embedded in them. Such blocking structures can have lifetimes varying from a few days to several weeks in the most extreme cases. Their presence can strongly affect the weather of large portions of the mid-latitudes, leading to the establishment of anomalous meteorological conditions. These can take the form of strong precipitation episodes or persistent anticyclonic regimes, leading in turn to floods, extreme cold spells, heat waves, or short-lived droughts. Even air quality can be strongly influenced by the establishment of atmospheric blocking, with episodes of high concentrations of low-level ozone in summer and of particulate matter and other air pollutants in winter, particularly in highly populated urban areas.Atmospheric blocking has the tendency to occur more often in winter and in certain longitudinal quadrants, notably the Euro-Atlantic and the Pacific sectors of the Northern Hemisphere. In the Southern Hemisphere, blocking episodes are generally less frequent, and the longitudinal localization is less pronounced than in the Northern Hemisphere.Blocking has aroused the interest of atmospheric scientists since the middle of the last century, with the pioneering observational works of Berggren, Bolin, Rossby, and Rex, and has become the subject of innumerable observational and theoretical studies. The purpose of such studies was originally to find a commonly accepted structural and phenomenological definition of atmospheric blocking. The investigations went on to study blocking climatology in terms of the geographical distribution of its frequency of occurrence and the associated seasonal and inter-annual variability. Well into the second half of the 20th century, a large number of theoretical dynamic works on blocking formation and maintenance started appearing in the literature. Such theoretical studies explored a wide range of possible dynamic mechanisms, including large-amplitude planetary-scale wave dynamics, including Rossby wave breaking, multiple equilibria circulation regimes, large-scale forcing of anticyclones by synoptic-scale eddies, finite-amplitude non-linear instability theory, and influence of sea surface temperature anomalies, to name but a few. However, to date no unique theoretical model of atmospheric blocking has been formulated that can account for all of its observational characteristics.When numerical, global short- and medium-range weather predictions started being produced operationally, and with the establishment, in the late 1970s and early 1980s, of the European Centre for Medium-Range Weather Forecasts, it quickly became of relevance to assess the capability of numerical models to predict blocking with the correct space-time characteristics (e.g., location, time of onset, life span, and decay). Early studies showed that models had difficulties in correctly representing blocking as well as in connection with their large systematic (mean) errors.Despite enormous improvements in the ability of numerical models to represent atmospheric dynamics, blocking remains a challenge for global weather prediction and climate simulation models. Such modeling deficiencies have negative consequences not only for our ability to represent the observed climate but also for the possibility of producing high-quality seasonal-to-decadal predictions. For such predictions, representing the correct space-time statistics of blocking occurrence is, especially for certain geographical areas, extremely important.
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50

Holy Bible: New Living Translation, TuTone Wine/Gold, Leatherlike Premium Slimline Reference Large Print. 2a ed. Tyndale House Publishers, 2005.

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