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uma visualização das condições de climaticas globais
boletins gerados por supercomputadores
atualizados a cada três horas


superfície estimatida do oceano
atualizadas a cada cinco dias


temperaturas de superfície do oceano e
anomalia da média diária (1981-2011)
atualizada diariamente


ondas do oceano
atualizadas a cada três horas


updated every thirty minutes

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Comunidade Página do Facebook
Autor Cameron Beccario @cambecc
Versão gratuita do código fonte
Módulos D3.js
Dados meteorológicos GFS (Global Forecast System)
Dados de correntes do oceano OSCAR
Earth & Space Research
Temperatura de Superfície do Mar OI SST (Optimum Interpolation Sea Surface Temperature) V2.1
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 (E.U. Copernicus Marine Service Information)
RTGSST (Real Time Global Sea Surface Temperature)
Ondas do oceano WAVEWATCH III
Bleaching Alert Area Coral Reef Watch / NOAA
Aerossóis e química GEOS-5 (Goddard Earth Observing System)
CAMS (Copernicus Atmosphere Monitoring System)
Copernicus / European Commission + ECMWF
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)
Decodificador de GRIB/NetCDF UCAR/Unidata THREDDS
Dados geográficos Natural Earth
Hospedagem CloudFlare
Amazon S3
Fontes M+ FONTS
Google Noto Fonts
Icons Font Awesome Free by @fontawesome - CC BY 4.0
Translation Management OneSky
Escalas de Cores
Kindlmann Linear Luminance
Dave Green's cubehelix
Borboleta Waterman
Inspiração HINT.FM wind map

atmospheric pressure corresponds roughly to altitude
several pressure layers are meteorologically interesting
they show data assuming the earth is completely smooth
note: 1 hectopascal (hPa) = 1 millibar (mb)

1000 hPa 00,~100 m, condições ao nível do mar
850 hPa 0~1,500 m, camada limite atmosférica, baixa
700 hPa 0~3,500 m, camada limite atmosférica, elevada
500 hPa 0~5,000 m, vorticidade
250 hPa ~10,500 m, corrente de jato
70 hPa ~17,500 m, estratosfera
10 hPa ~26,500 m, ainda mais estratosfera

A camada de "Superfície" representa as condições no terreno ou do nível da água
esta camada segue os contornos das montanhas, vales, etc.


overlays show another dimension of data using color
some overlays are valid at a specific height
while others are valid for the entire thickness of the atmosphere

Vento velocidade do vento na altura especificada
Temp temperatura na altura especificada
UH umidade relativa na altura especificada
WPD Densidade instantânea do vento
measure of power available in the wind: ½ρv3, where ρ is air density and v is wind velocity
TAP Total Precipitable Water
quantidade total de água em uma coluna de ar que se estende do solo ao espaço
TAN Total de água na nuvem
quantidade total de água nas nuvens em uma coluna de ar da terra para o espaço
3AP Acúmulo de precipitação em 3 horas
quantidade de precipitação nas próximas três horas
CAPE Energia Potencial Convectiva Disponível
indica o empuxo do ar, uma medida da instabilidade atmosférica e indicador de tempo severo
MSLP Pressão ao nível do mar
pressão de ar reduzida ao nível do mar
MI Índice de Desconforto Térmico
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
TSM Temperatura de Superfície do Mar
temperatura na superfície do oceano
ATSM Anomalia de Temperatura na Superfície do Mar
RTG-SST: diferença na temperatura do mar de média diária durante anos 1981-2011
OSTIA: calculated from 1981–present Pathfinder climatology
OI SST: calculated from 1971-2000 OI SST V2 climatology
ASO Altura Significativa de Onda
aproximadamente igual a altura de onda, como estimado por um "observador"
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 Concentração de Monóxido de Carbono Superficial
Uma fração de monóxido de carbono presente no ar da superfície da terra
CO2sc Concetração de Dióxido de Carbono na Superfície
uma fração de dióxido de carbono presente no ar da superfície terrestre
SO2sm Massa de Dióxido de Enxofre Superficial
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 Extinção de pó
the aerosol optical thickness (AOT) of light at 550 nm due to dust
SO4ex Extinção de sulfato
the aerosol optical thickness (AOT) of light at 550 nm due to sulfate
PM1 Particulate Matter < 1 µm
mass of atmospheric particles with a diameter less than 1 micron
PM2.5 Particulate Matter < 2.5 µm
mass of atmospheric particles with a diameter less than 2.5 microns
PM10 Particulate Matter < 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.

sobre ondas do oceano

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.

sobre concentrações de CO2
for dates earlier than 2017-01-24 04:30 UTC

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 00:00 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.

From 2017-01-24 04:30 UTC, this adjustment is no longer necessary because GEOS-5 appears to have been upgraded.


GEOS-5 data (covering all Chem and Particulates layers) comes with the following disclaimer: Forecasts using the GEOS system are experimental and are produced for research purposes only. Use of these forecasts for purposes other than research is not recommended.

sobre aerossóis e extinção

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).

atalhos do teclado

e mostrar o menu
escape feche a caixa de diálogo/menu
n ir para (data mais recente)
shift-c show the date selection calendar
j voltar vários passos
shift-j voltar vários passos
k ir para a frente
shift-k avançar vários passos
g alternar a grade ligar/desligar
p alternar a animação ligar/desligar
shift-h habilitar/desabilitar modo de alta definição
shift-t show settings
i subir um nível de pressão
shift-i subir para a estratosfera
m descer um nível de pressão
shift-m descer para a superfície
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


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Selected-by-CLEAN logo

Selected for inclusion in the Climate Literacy and Energy Awareness Network (CLEAN) collection of educational resources.

Os dados usados no GEOS-5 foram fornecidos pelo escritório de assimilação (GMAO) na NASA Goddard Space Flight Center e modelagem Global através do portal de dados on-line no centro da NASA para a simulação de clima

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.

clima e oceano de dados gerados a partir de modelos numéricos não garante a precisão das informações

Copyright (c) 2023 Cameron Beccario