Go to NBCNews.com for breaking news, videos, and the latest top stories in world news, business, politics, health and pop culture. Xem trực tiếp cơn bão tại earth.nullschool.net Nguồn tổng hợp. Đánh Giá post. Related Posts. NEW Hyperloop là gì? Chi tiết về Hyperloop mới nhất 2021. Tổng Hợp Tháng Mười 24, 2021 • 0 Comment. X2Go là giải pháp kết nối máy tính từ xa lý tưởng thay thế UltraViewer. Phần mềm sử dụng giao thức NX, kết nối 2 máy tính từ xa và chiếm dụng ít băng thông. Bằng cách tải X2Go, bạn có thể kết nối và điều khiển các máy tính chạy Linux, macOS và thậm chí là cả Windows. 383. Have you still got the runway OK? Ah .. just barely .. we'll pick up the ILS here. 30 Jun 1967. Thai International. 601. I have no radar contact with you. 06 Nov 1967. Trans World Airlines. brick earth nghĩa là gì, định nghĩa, các sử dụng và ví dụ trong Tiếng Anh. Cách phát âm brick earth giọng bản ngữ. Từ đồng nghĩa, trái nghĩa của brick earth. Từ điển Anh Việt - Chuyên ngành. brick earth * kỹ thuật. xây dựng: đất làm gạch. Định nghĩa what on earth is that? Đăng ký; Đăng nhập; Question mariyedu. 3 Thg 12 2016. Tiếng Tây Ban Nha(Spain) rm9Ov. powered by In Youth, education & environment Earth School was co-created by UNEP and Ted-Ed to provide kids, parents and teachers all over the world with engaging nature-focused content to stay connected to nature during the global covid-19 pandemic, which has seen approximately billion children out of school. Earth School takes students on 30 quests, each focused on a different nature-related topic. The content was curated by an incredible team of collaborators and volunteers and was shaped to help students understand and celebrate our natural world. Now more than ever, we need to take care of this planet we call home. Earth School seeks to inspire such stewardship through its quests, each of which focuses on a different topic and allows us to understand, conceptualize and connect with nature in a different way. Check out the Earth School website to learn more about this amazing resource. In Youth, education & environment une visualisation des conditions météorologiques mondialesprédites par des superordinateursmises à jour toutes les trois heures estimations des courants océaniques de surfacemises à jour tous les cinq jours températures océaniques de surface etanomalie par rapport à la moyenne quotidienne 1981-2011mises à jour quotidiennement vagues océaniquesmises à jour toutes les trois heures auroremise à jour toutes les trente minutes licence contactez inquiries pour obtenir une licence ou pour toute autre question Communauté Page Facebook Auteure Cameron Beccario cambecc Version Libre de source Modules Données Météorologiques GFS Global Forecast System EMC / NCEP / NWS / NOAA Données sur les courants océaniques OSCAR Earth & Space Research Température de Surface de la Mer OI SST Optimum Interpolation Sea Surface Temperature NOAA Physical Sciences Laboratory, Boulder, Colorado, USA note OI SST data is preliminary if fresher than two weeks and may change OSTIA Operational Sea Surface Temperature and Sea Ice Analysis UK Met Office + GHRSST + CMEMS Copernicus Marine Service Information RTGSST Real Time Global Sea Surface Temperature MMAB / EMC / NCEP / NWS / NOAA Vagues océaniques WAVEWATCH III MMAB / EMC / NCEP / NWS / NOAA Bleaching Alert Area Coral Reef Watch / NOAA Aérosols et Chimie GEOS-5 Goddard Earth Observing System GMAO / NASA CAMS Copernicus Atmosphere Monitoring System Copernicus / European Commission + ECMWF Aurore OVATION SWPC / NCEP / NWS / NOAA Processing script written by Dr. Stephanie Deppe profile Ultraviolet Index and Erythemal Dose Rate Climate Prediction Center / NCEP / NWS / NOAA Active Fires Fire Information for Resource Management System FIRMS / EOSDIS / NASA see discussion below Décodeur GRIB/NetCDF UCAR/Unidata THREDDS Données géographiques Natural Earth Hébergement CloudFlare Amazon S3 Polices M+ FONTS Google Noto Fonts Icons Font Awesome Free by fontawesome - CC BY Gestion de la traduction OneSky Echelles de couleurs Kindlmann Linear Luminance MYCARTA Dave Green's cubehelix Papillon Waterman Prototype Inspiration wind map la pression atmosphérique correspond approximativement à l’altitudeplusieurs couches de pression atmosphérique sont intéressantes d’un point de vue météorologiqueles données de ces couches sont présentées comme si la terre était complètement lisseremarque 1 hectoPascal hPa = 1 millibar mb 1000 hPa 00,~100 m, Conditions proches du niveau de la mer 850 hPa 0~1,500 m, couche limite planétaire, basse 700 hPa 0~3,500 m, couche limite planétaire, haute 500 hPa 0~5,000 m, vorticité / tourbillon 250 hPa ~10,500 m, courant-jet 70 hPa ~17,500 m, stratosphère 10 hPa ~26,500 m, encore plus de stratosphère la couche Surface » représente les conditions au niveau du sol ou de l'eaucette couche suit les contours des montagnes, des vallées, etc. les couches superposables montrent une autre dimension de données au moyen de couleurscertaines superpositions sont pertinentes à une hauteur spécifiquetandis que d’autres le sont pour toute l’épaisseur de l’atmosphère Vent vitesse du vent à la hauteur spécifiée Temp température à la hauteur spécifiée HR humidité relative à la hauteur spécifiée DPE Densité de Puissance Éolienne Instantanée mesure de la puissance éolienne disponible ½ρv3, où ρ est la densité de l’air et v la vitesse du vent EPT Eau Précipitable Totale quantité totale d’eau dans une colonne d’air s’étendant depuis le sol jusqu’à l’espace CELT Contenu en Eau Liquide Total quantité totale d’eau contenue dans les nuages présents dans une colonne d’air s’étendant depuis le sol jusqu’à l’espace AP3H Accumulation des Précipitations Pendant 3 Heures quantité de précipitations au cours des trois prochaines heures EPCD Énergie Potentielle de Convection Disponible indique la poussée de l'air, une mesure de l'instabilité atmosphérique et prédicteur de temps violent PMNM Pression Atmosphérique Moyenne au Niveau de la Mer la pression d'air réduite au niveau de la mer II Indice d'Inconfort température atmosphérique perçue comme une combinaison de l'indice de chaleur et du refroidissement éolien UVI Ultraviolet Index risk of harm from unprotected sun exposure due to the strength of sunburn-producing ultraviolet UV radiation 0 - 2 low 3 - 5 moderate 6 - 7 high 8 - 10 very high 11+ extreme TSM Température de Surface de la Mer temperature de surface océanique ATSM Anomalie de Température de Surface de la Mer RTG-SST différence de température de l'océan de la moyenne quotidienne au cours des années 1981-2011 OSTIA calculated from 1981–present Pathfinder climatology OI SST calculated from 1971-2000 OI SST V2 climatology HTSGW Hauteur Significative valeur quasi similaire à la hauteur moyenne des vagues estimée par un observateur qualifié » BAA Bleaching Alert Area 7-day maximum the level of coral bleaching heat stress No Stress No heat stress or coral bleaching is present. Bleaching Watch Low-level heat stress is present. Bleaching Warning Heat stress is accumulating. Coral bleaching is possible. Alert Level 1 Significant coral bleaching is likely. Alert Level 2 Severe coral bleaching and significant coral death is likely. COsc Concentration de Monoxyde de Carbone en Surface la fraction de monoxyde de carbone présente dans l'air à la surface de la Terre CO2sc Concentration de Dioxyde de Carbone en Surface la fraction de dioxyde de carbone présente dans l'air à la surface de la Terre SO2sm Masse de Dioxyde de Soufre en Surface quantité de dioxyde de soufre présente dans l'air près de la surface de la Terre NO2 Nitrogen Dioxide amount of nitrogen dioxide in the air near the earth's surface DUex Extinction des Poussières epaisseur optique des aérosols EOA d’une source de lumière de 550 nm en présence de poussières SO4ex Extinction des Sulfates epaisseur optique des aérosols EOA d’une source de lumière de 550 nm en présence de sulfates PM1 Particule de Matière < 1 µm masse de particules atmosphériques d'un diamètre inférieur à 1 micron Particule de Matière < µm masse de particules atmosphériques d'un diamètre inférieur à 2,5 microns PM10 Particule de Matière < 10 µm masse de particules atmosphériques d'un diamètre inférieur à 10 microns OMaot Organic Matter aerosol optical thickness The aerosol optical thickness AOT of light at 550 nm due to organic matter suspended in air. This layer can be interpreted as the thickness of smoke from wildfires and other sources of combustion. à propos des vagues océnaniques Hauteur Significative est la hauteur moyenne du tiers des plus hautes vagues à un point donné de l’océan. Il y a un grand compte-rendu ici décrivant ce que cela signifie. Période de pic de vagues est la fréquence inverse des vagues les plus énergiques passant par un point particulier, générée par le vent ou la houle. Certes, il y a beaucoup plus de groupes de vagues se déplaçant à travers une zone, chacun dans des directions différentes, mais en essayant de les montrer tous devient rapidement complexe. Au lieu de cela, nous montrons un groupe de vagues contribuant à plus d'énergie. Cela a pour effet, cependant, de créer des frontières» entre les régions de l'océan où le groupe d'ondes 1 passe soudainement à la deuxième place. Souvent, ces limites représentent les fronts de houle, mais d'autres fois, ils ne sont que des artefacts du mécanisme de classement. à propos des concentrations de CO2pour les dates antérieures à 2017-01-24 0430 UTC Lors de la mise en œuvre de la visualisation de la concentration de surface du CO2, j’ai constaté que le modèle GEOS-5 de la NASA présentait une concentration moyenne globale significativement différente de celles généralement rapportées. Par exemple, selon les données du 23/11/2015 à minuit heure UTC, la moyenne globale calculée est seulement de 368 ppmv tandis que les observatoires de CO2 rapportent des concentrations de près de 400 ppmv. GEOS-5 a été construit dans les années 2000. Aussi, est-il possible que ce modèle ne tienne pas compte de l’accumulation du CO2 atmosphérique au cours du temps. Il s’agit toutefois d’une simple spéculation. Je n’en suis pas certain. Afin d’aligner les résultats de GEOS-5 avec ceux des modèles contemporains, j’ai ajouté une compensation uniforme de +32 ppmv, augmentant ainsi la moyenne globale jusqu'à 400 ppmv. Cette démarche n’est pas scientifiquement valide, mais elle permet d’illustrer la discussion actuelle autour du CO2 atmosphérique. Bien entendu, j’accueillerai volontiers une approche plus rigoureuse ou une explication concernant les valeurs calculées par le modèle GEOS-5. À partir du 2017-01-24 0430 UTC, cet ajustement n'est plus nécessaire car GEOS-5 semble avoir été mis à niveau. avertissement Les données GEOS-5 constituant les couches de superposition Chimie » et Particules » sont fournies avec la clause de non-responsabilité suivante Les prévisions utilisant le système GEOS sont expérimentales et produites à des fins de recherche uniquement. Leur utilisation à toute autre fin n’est pas recommandée. à propos des aérosols et du coefficient d’extinction Un aerosol est un aérosol contenant des particules. Les particules communes sont la poussière, la fumée, la suie et les gouttelettes d’eau nuages. Ces particules affectent la lumière solaire principalement par absorption et diffusion, qui se combinent pour réduire la quantité de lumière atteignant le sol. Cette perte de lumière lorsqu’elle traverse l’atmosphère s’appelle extinction. Une mesure courante de ce coefficient est l’épaisseur optique des aérosols EOA, qui est le logarithme du rapport entre l'intensité de lumière incidente et celle transmise. Elle nous aide à comprendre comment la présence de particules épaissie » l’air. about active fire data Fire data is a combination of VIIRS 375m NRT NOAA-20 and VIIRS 375m NRT Suomi NPP active fire products. Each fire detection data point contains the time of detection when the satellite made the measurement and the Fire Radiative Power FRP in units of megawatts MW. For more information on how to interpret the readings, see the FIRMS FAQ and the detailed discussion of VIIRS I-Band 375 m Active Fire Data. We acknowledge the use of data and/or imagery from NASA's Fire Information for Resource Management System FIRMS, part of NASA's Earth Observing System Data and Information System EOSDIS. raccourcis clavier e afficher le menu escape fermer la boîte de dialogue/le menu n aller au temps présent données les plus récentes shift-c show the date selection calendar j reculer dans le temps shift-j reculer dans le temps rapidement k avancer dans le temps shift-k avancer dans le temps rapidement g activer/désactiver la grille p activer/désactiver l'animation shift-h activer/désactiver le mode haute définition shift-t show settings i monter d'un niveau de pression shift-i monter à la stratosphère m descendre d'un niveau de pression shift-m aller à la surface d zoom in shift-d zoom in faster x zoom out shift-x zoom out faster w rotate up shift-w rotate up faster z rotate down shift-z rotate down faster a rotate left shift-a rotate left faster s rotate right shift-s rotate right faster traducteurs Александр Попов Вячеслав Епиков 1599763839 1992pb 2451158917 피시 afropolakwot agagey Aleksander Alexander Kirilov Alexey Dmitriev Alexey Korsakov AlexOrlovets Anderson Porto Andre Lz Andrea de Franco Andrew Pedrini Andrey Bagmanov Antonpek arquerogonza Artur Wisniewski ashawesoman astrostrong asveruz atom bgij bidulem3 Birg3r Bohuslav Šín Bram Versteeve Bryan carlofrc Cassiel Bclamson Ching-ping Yu Christian Leroux contact cuxcoll Daniel Bartsch Daniel Isak Marinosson Daniel Pawlowski Daniel Rakoczy danielruiz1636 Darlite davalenciano98 Davide Carlier Denat250 Dimitris T. Papadimitriou Dominic Douglas dsantosgtm dustyhofman e Eason Huang egarpunov Eric Kim essaii32 estefilippini fantasy_lcl farrasoctara Felipe Faria florian-lerch franci00 FranklinZhang Frederik T. de Ridder fthmiln gherlainfo Gian Centeno giospud graceang grol2901 Hebel holgersson Hyung Wook Jung Ichiro Wang Ignacio Sanz iii1212 InfoSecOne Jae Soo Park Jiří Batelka Joanna Rinne Joao Correia jocelot Jomari Joseph Barrera Jonathan Yang Jose A. Frias Morales juanpaexpedite Karol Sapiński Kiyun Jeon kty5663 ku5an2901 laurapaccini leandro1212 lretamal Luboš Motl Mark markeletona Markus Schley Martine Bolzinger Matt Tang Mattia Raffa mavilesilva melfi Melissa Ortiz Massó Meow Wang mgb Michael Purer Michael Michel Rivero Miquel Bayo Moreno mir597 MirageF1AZ Miroslaw Lisiak Mohannad Alahmadi m_strugale nando nunolava1998 Olivier OLS-RU Oğuzhan Arı Paul Bachem Paweł Kowalczyk pdobrev Personim Intaned Philippe Jabet Plamen Dobrev ProffLex P_A_N_D_A_M_A_N Rafael Nonato Bassora rajeshgodvani RaskiPL reyfran8 Riccardo Monfardini robertrosalex Roger Helman Roller978 rosariainpo Russel Schwartz sapan021 sarogrom Seongmin Park september43 Seregalsv Serega silverhaze030 Simone Dragoni siudzin98 skyneon77 sombrasbaul Somil Thesia Stephen Flynn Steven SUGIMOTO Tatsuo Sunny Miu Tayseer M Alhibshi Telmo John tenderstart thanhhuyenlth Thomas Middelveld Thorsten Schleicher tigormal tigra200sx Tomasz Waligóra torstenleibrich tsuka tama ultordima Vasily Tarasenko vhc1967 Vu Thuong Víctor Velarde wasted webfreelance Wonmin Jeong wtlovergirl xesmedic xorpid xrdeem xsqz 潘柏綸 yaawwad Yauhen Bahashou youngjune4498 Youngmin Jeon Yukun Chen zackcaussy Zulus Οverlord Les données GEOS-5 utilisées sur ce site ont été fournies par le Global Modeling and Assimilation Office GMAO du centre de vols spatiaux Goddard de la NASA par le biais du portail de données en ligne du centre de la NASA pour la simulation du climat. Generated using Copernicus Atmosphere Monitoring Service Information 2017-2020. Neither the European Commission nor ECMWF is responsible for any use that may be made of this information. les données météorologiques et océaniques sont générées par des modèles numériques ne donne aucune garantie quant à l’exactitude des données Copyright c 2023 Cameron Beccario 전세계 날씨상황슈퍼컴퓨터 예보3시간마다 업데이트 해류 예보5일마다 업데이트 해수면 온도 및일평균으로부터의 이상 1981-2011매일 업데이트 바다의 파도는3시간 마다 업데이트 됩니다 오로라는매 30분마다 업데이트됩니다 라이선스 라이선스나 다른 질문은 inquiries 물어보세요 커뮤니티 페이스북 페이지 제작자 Cameron Beccario cambecc 무료 버전의 소스 코드 사용한 라이브러리 기후 데이터 GFS Global Forecast System EMC / NCEP / NWS / NOAA 해류 데이터 OSCAR Earth & Space Research 해수면 온도 OI SST Optimum Interpolation Sea Surface Temperature NOAA Physical Sciences Laboratory, Boulder, Colorado, USA note OI SST data is preliminary if fresher than two weeks and may change OSTIA Operational Sea Surface Temperature and Sea Ice Analysis UK Met Office + GHRSST + CMEMS Copernicus Marine Service Information RTGSST Real Time Global Sea Surface Temperature MMAB / EMC / NCEP / NWS / NOAA 파랑 WAVEWATCH III MMAB / EMC / NCEP / NWS / NOAA Bleaching Alert Area Coral Reef Watch / NOAA 에어로졸과 화학물질 GEOS-5 Goddard Earth Observing System GMAO / NASA CAMS Copernicus Atmosphere Monitoring System Copernicus / European Commission + ECMWF 오로라 OVATION SWPC / NCEP / NWS / NOAA Processing script written by Dr. Stephanie Deppe profile Ultraviolet Index and Erythemal Dose Rate Climate Prediction Center / NCEP / NWS / NOAA Active Fires Fire Information for Resource Management System FIRMS / EOSDIS / NASA see discussion below GRIB/NetCDF 디코더 UCAR/Unidata THREDDS 지도 데이터 Natural Earth 호스팅 CloudFlare Amazon S3 글꼴 M+ FONTS Google Noto Fonts Icons Font Awesome Free by fontawesome - CC BY 번역 관리 OneSky 색상 스케일 Kindlmann Linear Luminance MYCARTA Dave Green's cubehelix 워터맨도법 프로토타입 영감 wind map 대기압은 일반적으로 고도에 반비례합니다몇몇 대기압의 경우 기상학적으로 특별한 의미를 지닙니다지구가 매끄러운 구라 가정하고 계산합니다참고 1 헥토파스칼 hPa = 1 밀리바 mb 1000 hPa 00,~100 m, 해수면 근처 850 hPa 0~1,500 m, planetary boundary, low 700 hPa 0~3,500 m, planetary boundary, high 500 hPa 0~5,000 m, vorticity 250 hPa ~10,500 m, 제트 기류 70 hPa ~17,500 m, 성층권 10 hPa ~26,500 m, 머나먼 성층권 "표면"은 지면이나 수면을 말하며이는 산이나 골짜기의 윤곽을 따라 정해집니다. 오버레이에서는 색상을 이용해 지도에 대략적인 값을 표시하며특정 고도에서만 유효한 오버레이도 있고그 외에는 어느 고도에서나 유효합니다 바람 특정 고도에서의 풍속 온도 특정 고도에서의 기온 상대습도 특정 고도에서의 상대습도 WPD 풍력 에너지 밀도 바람이 가진 힘의 단위입니다 ½ρv3, 여기서 p는 공기 밀도이고 v는 풍속입니다 TPW Total Precipitable Water 지상에서 우주까지 뻗은 기둥에서 대기에 포함된 물의 양 TCW 총 구름 수분함량 지상에서 우주까지 뻗은 기둥에서 구름에 포함된 물의 양 3HPA 3시간 강수량 다음 3시간 동안의 강수량 CAPE Convective Available Potential Energy from Surface 공기가 떠오를 때 쓸 수 있는 힘으로, 대기 불안정 및 악천후를 예측하는 데 이용할 수 있음 MSLP Mean Sea Level Pressure air pressure reduced to sea level MI 불쾌지수 perceived air temperature as combination of heat index and wind chill UVI Ultraviolet Index risk of harm from unprotected sun exposure due to the strength of sunburn-producing ultraviolet UV radiation 0 - 2 low 3 - 5 moderate 6 - 7 high 8 - 10 very high 11+ extreme 해수면 온도 Sea Surface Temperature temperature of the ocean surface 해수면 이상수온 Sea Surface Temperature Anomaly RTG-SST 1981부터 2011년 사이의 해수 온도 일일 평균 차 OSTIA calculated from 1981–present Pathfinder climatology OI SST calculated from 1971-2000 OI SST V2 climatology HTSGW Significant Wave Height roughly equal to mean wave height as estimated by a "trained observer" BAA Bleaching Alert Area 7-day maximum the level of coral bleaching heat stress No Stress No heat stress or coral bleaching is present. Bleaching Watch Low-level heat stress is present. Bleaching Warning Heat stress is accumulating. Coral bleaching is possible. Alert Level 1 Significant coral bleaching is likely. Alert Level 2 Severe coral bleaching and significant coral death is likely. COsc 일산화탄소 지표 농도 the fraction of carbon monoxide present in air at the earth's surface CO2sc 이산화탄소 지표 농도 the fraction of carbon dioxide present in air at the earth's surface SO2sm 지표 아황산가스량 amount of sulfur dioxide in the air near the earth's surface NO2 Nitrogen Dioxide amount of nitrogen dioxide in the air near the earth's surface DUex 분진 소광 the aerosol optical thickness AOT of light at 550 nm due to dust SO4ex 황산염 소광 the aerosol optical thickness AOT of light at 550 nm due to sulfate PM1 초미세먼지 < 1 µm mass of atmospheric particles with a diameter less than 1 micron 초미세먼지 < µm mass of atmospheric particles with a diameter less than microns PM10 미세먼지 < 10 µm mass of atmospheric particles with a diameter less than 10 microns OMaot Organic Matter aerosol optical thickness The aerosol optical thickness AOT of light at 550 nm due to organic matter suspended in air. This layer can be interpreted as the thickness of smoke from wildfires and other sources of combustion. about ocean waves Significant Wave Height is the average height of the highest 1/3 of waves at a particular point in the ocean. There's a great writeup here describing what this means. Peak Wave Period is the inverse frequency of the most energetic waves passing through a particular point, whether wind generated or swells. Certainly, there are many more groups of waves moving through an area, each in different directions, but trying to show them all rapidly becomes complex. Instead, we show the one wave group contributing the most energy. This has the effect, though, of creating "boundaries" between regions of ocean where the 1 wave group suddenly switches to second place. Often these boundaries represent swell fronts, but other times they are just artifacts of the ranking mechanism. CO2 농도2017-01-24 0430 UTC 이전 자료 열람 시 참고 사항 While implementing the visualization of CO2 surface concentration, I noticed the NASA GEOS-5 model reports a global mean concentration that differs significantly from widely reported numbers. For example, from the run at 2015-11-23 0000 UTC, the global mean is only 368 ppmv whereas CO2 observatories report concentrations closer to 400 ppmv. GEOS-5 was constructed in the 2000s, so perhaps the model does not account for accumulation of atmospheric CO2 over time? This is simply speculation. I am just not certain. To bring the GEOS-5 results closer to contemporary numbers, I have added a uniform offset of +32 ppmv, increasing the global mean to 400 ppmv. This is not scientifically valid, but it does allow the visualization to become illustrative of the discussion occurring today around atmospheric CO2. Without question, I would welcome a more rigorous approach or an explanation why the GEOS-5 model produces the data that it does. 2017-01-24 UTC부터는 GEOS-5가 업그레이드 되었으므로 더 이상 값을 조정할 필요가 없습니다. 면책 조항 화학물질 및 미세먼지 레이어 구현에 사용된 GEOS-5 데이터를 이용할 때 다음 면책 조항을 읽어보십시오 GEOS 시스템을 활용한 예측 데이터는 실험적이며 연구 목적으로만 생성되었습니다. 이러한 예측을 단순 조사 이외의 사안에서 이용하는 것은 권장하지 않습니다. 에어로졸과 소광 효과 An aerosol is air containing particles. Common particles are dust, smoke, soot, and water droplets clouds. These particles affect sunlight primarily through absorption and scattering, which combine to reduce the amount of light reaching the ground. This loss of light as it passes through the atmosphere is called extinction. One common measure of extinction is aerosol optical thickness AOT, which is the log of the ratio between the power of incoming light and the power of transmitted light. This helps us understand how "thick" the air is with particulates. about active fire data Fire data is a combination of VIIRS 375m NRT NOAA-20 and VIIRS 375m NRT Suomi NPP active fire products. Each fire detection data point contains the time of detection when the satellite made the measurement and the Fire Radiative Power FRP in units of megawatts MW. For more information on how to interpret the readings, see the FIRMS FAQ and the detailed discussion of VIIRS I-Band 375 m Active Fire Data. We acknowledge the use of data and/or imagery from NASA's Fire Information for Resource Management System FIRMS, part of NASA's Earth Observing System Data and Information System EOSDIS. 키보드 단축키 e 메뉴를 띄우기 escape 메뉴/대화창 닫기 n 현재로 가기가장 최근의 데이터로 shift-c 날짜 선택 달력 표시하기 j 한 단계 과거로 shift-j 여러 단계 과거로 k 한 단계 미래로 shift-k 여러 단계 미래로 g 격자 켜고 끄기 p 애니메이션 켜고 끄기 shift-h 고화질 모드 켜고 끄기 shift-t show settings i 고도 한 단계 높이기 shift-i 성층권으로 올라가기 m 고도 한 단계 내리기 shift-m 표면으로 내려가기 d zoom in shift-d zoom in faster x zoom out shift-x zoom out faster w rotate up shift-w rotate up faster z rotate down shift-z rotate down faster a rotate left shift-a rotate left faster s rotate right shift-s rotate right faster 번역해주신 분들 Александр Попов Вячеслав Епиков 1599763839 1992pb 2451158917 피시 afropolakwot agagey Aleksander Alexander Kirilov Alexey Dmitriev Alexey Korsakov AlexOrlovets Anderson Porto Andre Lz Andrea de Franco Andrew Pedrini Andrey Bagmanov Antonpek arquerogonza Artur Wisniewski ashawesoman astrostrong asveruz atom bgij bidulem3 Birg3r Bohuslav Šín Bram Versteeve Bryan carlofrc Cassiel Bclamson Ching-ping Yu Christian Leroux contact cuxcoll Daniel Bartsch Daniel Isak Marinosson Daniel Pawlowski Daniel Rakoczy danielruiz1636 Darlite davalenciano98 Davide Carlier Denat250 Dimitris T. Papadimitriou Dominic Douglas dsantosgtm dustyhofman e Eason Huang egarpunov Eric Kim essaii32 estefilippini fantasy_lcl farrasoctara Felipe Faria florian-lerch franci00 FranklinZhang Frederik T. de Ridder fthmiln gherlainfo Gian Centeno giospud graceang grol2901 Hebel holgersson Hyung Wook Jung Ichiro Wang Ignacio Sanz iii1212 InfoSecOne Jae Soo Park Jiří Batelka Joanna Rinne Joao Correia jocelot Jomari Joseph Barrera Jonathan Yang Jose A. Frias Morales juanpaexpedite Karol Sapiński Kiyun Jeon kty5663 ku5an2901 laurapaccini leandro1212 lretamal Luboš Motl Mark markeletona Markus Schley Martine Bolzinger Matt Tang Mattia Raffa mavilesilva melfi Melissa Ortiz Massó Meow Wang mgb Michael Purer Michael Michel Rivero Miquel Bayo Moreno mir597 MirageF1AZ Miroslaw Lisiak Mohannad Alahmadi m_strugale nando nunolava1998 Olivier OLS-RU Oğuzhan Arı Paul Bachem Paweł Kowalczyk pdobrev Personim Intaned Philippe Jabet Plamen Dobrev ProffLex P_A_N_D_A_M_A_N Rafael Nonato Bassora rajeshgodvani RaskiPL reyfran8 Riccardo Monfardini robertrosalex Roger Helman Roller978 rosariainpo Russel Schwartz sapan021 sarogrom Seongmin Park september43 Seregalsv Serega silverhaze030 Simone Dragoni siudzin98 skyneon77 sombrasbaul Somil Thesia Stephen Flynn Steven SUGIMOTO Tatsuo Sunny Miu Tayseer M Alhibshi Telmo John tenderstart thanhhuyenlth Thomas Middelveld Thorsten Schleicher tigormal tigra200sx Tomasz Waligóra torstenleibrich tsuka tama ultordima Vasily Tarasenko vhc1967 Vu Thuong Víctor Velarde wasted webfreelance Wonmin Jeong wtlovergirl xesmedic xorpid xrdeem xsqz 潘柏綸 yaawwad Yauhen Bahashou youngjune4498 Youngmin Jeon Yukun Chen zackcaussy Zulus Οverlord 이 사이트에서 사용된 GEOS-5 데이터는 NASA 고다드 우주 비행 센터의 글로벌 모델링 및 동화 사무소GMAO에서 NASA 기후 시뮬레이션 센터의 온라인 데이터 포털을 통해 제공되었습니다 Generated using Copernicus Atmosphere Monitoring Service Information 2017-2020. Neither the European Commission nor ECMWF is responsible for any use that may be made of this information. 날씨 및 해양 데이터는 수치 모델로부터 생성됩니다 자료의 정확도를 보장하지 않습니다. Copyright c 2023 Cameron Beccario 161 2020-01-29 205532 未经作者授权，禁止转载246615512649你是否注意过中国天气官方b站直播间左侧的流场图。在这期视频中，我们将教你读懂流场图最基本的东西 提供了一个可视化的全球风力、温度、空气质量实况和预报，也可以拿来查历史要素。气象 地理 科学 科普 知识 科学科普 联合创作 地球 趣味科普人文 天气 天气预报 创作团队 2人风羽酱-sdkUP主中国天气研发老婆！对不起！这款传奇太顶了！ 【系列】风羽气象小讲堂 3/4 【天气知识入门】天气预报又双叒叕不准了？真相竟然是…… 0846 【天气知识入门】10分钟带你了解卫星云图——懒得抬头看天，那就看看手机上的云图吧～ 1153 【天气知识入门】《8分钟教你看懂Earth全球风力图》 0819 【天气知识入门】看懂这些资料-你也能预报台风-来袭也能从容应对-以利奇马为例 【现代常用天气分析资料介绍和民众适用的易用APP推荐】 1316 【纪录片】天气档案 08 航空天气哔哩哔哩纪录片 29 【纪录片】天气档案 01 龙卷风哔哩哔哩纪录片 415 风暴之下 - 中国首部风暴纪录电影风羽酱-sdk 1346 如何查看天气？Windy软件使用方法ReginaSong 3 带你看天气图之地面天气图，继续和小编一起看看这些线条都是些什么？回眺佳合气象服务 1354 0 【天气知识入门】10分钟带你了解卫星云图——懒得抬头看天，那就看看手机上的云图吧～风羽酱-sdk 325 气压带、风带的形成（地理教学小视频）三三啊zZ 77 高空槽如何影响近地面的天气呢？张舰长2021 2875 17 【天象爱好者】观云识天气——做自己的天气预报员天象爱好者 16 气象小白の宝藏网站成都的雨夹雪 3556 0 【追光的传媒人｜风羽追风】天气和风羽，究竟哪一个先到来？中国传媒大学 9209 13 天气学原理和方法一颗梧桐布丁 91 台风动画介绍鸣戈动画摊 2 【纪录片】国家地理《失控的天气》，全球极端天气、末日景象、恐怖的龙卷风，感受大自然的咆哮麋鹿橙英语之家 30 三个超实用的气象卫星网~啊rua呜QwQ 4197 0 5分钟带你了解专业气象软件Windy｜飞行员,户外爱好者必备｜如何获取云层高度？安愉NZ 2 分享几个气象网站是吴小白呀 9189 3 【气象小科普】如何分析天气变化『one』东风58号 7217 7 地理生必须知道的十个网站我要装深沉 5 【科普/中文字幕/搬运】10分钟认识各种类型的云Ann_231242 67 展开 顶部

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