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Sea of clouds in Mount Pulag, Philippines. A sea of clouds is an overcast layer of stratocumulus clouds, as viewed from above, with a relatively uniform top which shows undulations of very different lengths resembling waves on the sea. [1] A sea of fog is formed from stratus clouds or fog and does not show undulations. [2]
Graph showing ocean temperature versus depth on the vertical axis. The graph shows several thermoclines (or thermal layers) based on seasons and latitude. The temperature at zero depth is the sea surface temperature. The ocean temperature plays a crucial role in the global climate system, ocean currents and for marine habitats.
Weather Monitoring: Real-time cloud tracking, temperature mapping, and storm detection. Climate Studies: Long-term trends, climate variability, and environmental changes. Natural Disasters: Early warning systems for cyclones, wildfires, and floods. Agriculture: Assessing crop health, soil moisture, and vegetation dynamics.
A surface weather analysis for the United States on October 21, 2006. By that time, Tropical Storm Paul was active (Paul later became a hurricane). Surface weather analysis is a special type of weather map that provides a view of weather elements over a geographical area at a specified time based on information from ground-based weather stations.
The current, third-generation features six channels at wavelength ranges important for cloud observation, cloud/snow differentiation, surface temperature observation and atmospheric correction. [3] The modern satellite array is able to give a global coverage with a resolution of 10 km every ~6 h.
Since returning the four-masted barque to life, Sea Cloud Cruises has built two more windjammers—the three-masted Sea Cloud II launched in 2001 and Sea Cloud Spirit launched in 2023—which join ...
Weather satellites have been available to infer sea surface temperature (SST) information since 1967, with the first global composites occurring during 1970. [10] Since 1982, [ 11 ] satellites have been increasingly utilized to measure SST and have allowed its spatial and temporal variation to be viewed more fully.
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