Scientists propose that mantle flow, rather than plate boundaries, drives uplift and volcanism in mobile belts. The study identifies two mountain ranges raised almost entirely by mantle flow in Spain and France.
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Researchers found barnacle communities flourish in vertical-upwelling zones with strong currents, contradicting previous theories. The study's findings suggest that barnacles latch onto rock walls due to constant bouncing against rocky surfaces, ultimately leading to the formation of thriving crustacean populations.
Scientists analyzed early Pliocene algae records to find evidence of sustained coastal upwelling off California's coast, even in a warmer climate. This insight provides valuable information on how ocean currents drive regional and global climate patterns.
Researchers have observed dynamic upwelling in the underlying mantle beneath a spreading center, leading to new crust formation. This finding resolves a long-standing debate regarding the relative importance of passive and dynamic upwelling in oceanic crust creation.
Tropical Storm Parma is expected to linger off the northwest coast of Luzon for five days, bringing showers and gusty winds to the northern Philippines and Taiwan. The storm's slow movement is due to a lack of wind pushing it west into the South China Sea.
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A team of scientists suggests that shifting winds in the Southern Ocean around Antarctica may have triggered a rapid increase in carbon dioxide levels at the end of the last ice age. This mechanism could amplify manmade warming and has been supported by sediment core analysis, but other climate models disagree.
Future increases in wind strength along the California coast may lead to more intense upwelling of cold water, potentially causing a larger 'dead zone' off the Oregon coast. Stronger winds could also create hazardous fire conditions in Southern California.
New study reveals that despite increased wind speeds, Southern Ocean currents and upwelling patterns remain unchanged, contradicting previous concerns about the ocean's capacity to combat climate change. The research suggests that small-scale ocean eddies balance stronger winds, preventing a significant impact on carbon dioxide storage.
Researchers from Oregon State University find that Pacific Northwest coast low-oxygen events are unprecedented and may be caused by stronger winds due to global warming. Hypoxic conditions have been recurring since 2002, with severe impacts on marine life.
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Deep-sea hydrothermal vents are found above volcanoes where upwelling of the mantle and spreading of the plates are aligned, allowing magma to breach the crust. In contrast, non-aligned zones lack hot smokers due to cooling and volatiles loss as magma moves laterally.
A study by Oregon State University scientists found that iron-rich winter runoff from Pacific Northwest streams and rivers fertilizes the nearshore Pacific Ocean, leading to robust phytoplankton production and fisheries. The researchers discovered that the iron is trapped on the continental shelf in the winter, but released during summ...
The California Current system has undergone dramatic variations in phytoplankton production, expanding hypoxic zones, and collapsing marine food webs off the western US coast. Climate change is consistent with predictive models of global climate change, but its definitive cause remains uncertain.
A new synthesis of decades of atmospheric and oceanographic data reveals that wild fluctuations in winds and currents are changing the way scientists think about the future of ocean resources off the US West Coast. Key findings include repeated low oxygen zones larger than Rhode Island and massive die-offs of seabirds.
A recent study in Nature supports the traditional theory of mantle plumes as the source of volcanic islands. Researchers found a close correlation between modeled and observed ratios of uranium-series isotopes across eight island locations, allowing them to estimate changes in temperature, speed, and size of mantle plumes.
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The study found a pattern of steady cooling in the EEP over 5 million years, with temperatures dropping by roughly one degree Celsius every million years. The research suggests that ocean regions near Antarctica were the main driver of EEP cooling, contradicting previous theories about rapid glacier growth in high northern latitudes.
Researchers discovered that pockets of water wedge themselves into the subtropical gyre, preventing deep-ocean nutrients from reaching the surface where plants can thrive. The study found that this phenomenon reduces primary productivity and supports the food chain.
A recent study challenges traditional theory that El Niño-La Niña cycles affect sardine and anchovy populations differently. Researchers found that sardines can thrive in warm waters during El Niño events, while anchovies adapt to cold conditions by extending their reproduction periods.
A study by Andrew Bakun and Scarla Weeks found that overfishing sardines can prevent phytoplankton population explosions, which release methane and hydrogen sulfide. The authors warn that areas around California and Africa are at risk of a tipping point, where upwelling processes intensify climate change.
A new hypoxic event has been detected off the Oregon coast, causing a massive die-off of fish and invertebrate marine species. Dissolved oxygen levels are significantly lower than those seen in the past 40 years, suggesting a major change in ocean circulation patterns.
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Computer simulations show that wind-driven upwelling along the California coast will intensify over the next 50 years due to increased carbon dioxide concentrations. The upwelling season is expected to extend further into the fall, supporting some of the observational work showing a trend toward increased upwelling intensity.
Researchers at UCSC have linked oceanographic events with rockfish recruitment patterns, finding two distinct groups of species responding differently to warm and cold water conditions. The study provides insights into the year-to-year variation in replenishment of these fish populations.
Researchers found that climate change may weaken average El Niño events due to a decline in ocean-atmosphere coupling. However, individual El Niños could still be intense, even in a warmer world. The study simulated past and future behavior of El Niño using the NCAR Climate System Model.
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Researchers at Oregon State University found extremely low oxygen levels in the lower water column, leading to mass die-offs of rockfish, Dungeness crabs, sculpins, and other marine life. The unusual event is attributed to coastal upwelling and wind patterns, not human activities.
NASA's QuikSCAT satellite data reveals two ITCZs: a northern zone near the equator and a southern zone south of the equator. The southern zone is weaker due to cooler ocean water, affecting wind speeds and precipitation patterns globally.
Scientists discover African Superswell is caused by hot mantle material rising from the core-mantle boundary, elevating southern Africa and driving tectonic plates. This phenomenon, known as dynamic topography, reveals a link between deep mantle dynamics and surface features.
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