This layer is derived from theWorldGeo_Physical_Climate_featuresfeature service that includes multiple versions of this ocean currents layer optimized for different map scales. The ocean currents data was compiled from theNOAA National Weather Serviceand theUS Army. ...
Then, it gets into what influences ocean currents. For example, the wind, tides, water density, rotation, and even ocean floor topography influence currents in the oceans. Finally, the lesson contrasts the differences between surface and deep ocean currents. For example, surface currents control t...
The heatmap (Fig. 5) showing only species with low frequency suggested that the presence of these species may explain the observed pattern in the PCoA based on the Jaccard distances. PERMANOVA (Table 1) analysis based on Bray–Curtis and Jaccard indices revealed that the microbiome within ...
We need global statistics on their distribution, their occurrence in various oceanic regions, their dimensions, and their lifetimes. The prospect of even a single global oceanic 'weather map', comparable to those obtained daily for the atmosphere, is hopeless in terms of in situ oceanographic ...
CAPE map Currents WARNINGS: Tide forecast are not official and are for reference purpose only. Grib files are computer-generated forecast files which are sent without review, and are offered on an as-is basis. There is no assurance that the data is accurate or correct. By using these data ...
Here we show how major rivers can efficiently connect to the deep-sea, by analysing the longest runout sediment flows (of any type) yet measured in action on Earth. These seafloor turbidity currents originated from the Congo River-mouth, with one flow tr
The five major lines of latitude, more commonly referred to as the five major circles of latitude, mark specific points on a globe or map of Earth. Four of the lines run parallel to the equator and sit north or south above or below the equator. Visible on a globe or map of the Earth...
Marine phytoplankton and zooplankton form the basis of the ocean’s food-web, yet the impacts of climate change on their biodiversity are poorly understood. Here, we use an ensemble of species distribution models for a total of 336 phytoplankton and 524
Holocene RSL data afford information on whether such rates are anomalous and can identify transgressions or periods of slowing RSL fall, both of which can be attributed to ice expansion when changes in global ocean volumes are considered. Radiocarbon and exposure-age results Our study focused on ...
"It is unequivocal that human influence has warmed the atmosphere, ocean and land," the report states. Many of the changes inflicted on the planet — especially our oceans — will be "irreversible for centuries to millennia," and continued warming will lead to an accelerat...