When fossil fuels are burned, carbon is released into the atmosphere in the form of carbon dioxide (CO2). This process contributes to the greenhouse effect, leading to global climate change and impacts such as rising temperatures and ocean acidification.
Water in the ocean turns into water vapor through a process called evaporation. This occurs when the water absorbs enough heat energy from the sun to break the intermolecular bonds and transition into a gaseous state. The water vapor then rises into the atmosphere and can form clouds or contribute to the water cycle.
One effect of water's cohesion is surface tension, which allows water to form droplets and support objects that are denser than itself, such as insects walking on water.
The majority of carbon dioxide is found in the ocean, which absorbs about 30% of human-generated CO2 emissions. The atmosphere contains the rest of the CO2, with concentrations fluctuating due to human activities and natural processes.
The main source of dissolved oxygen in the ocean is from photosynthesis by marine plants, such as phytoplankton and seaweed. They use sunlight to convert carbon dioxide and water into oxygen through the process of photosynthesis.
The process of the ocean absorbing CO2 leads to ocean acidification, causing a drop in pH. This can have negative impacts on marine life, particularly organisms that rely on calcium carbonate to build their shells and skeletons. Ocean acidification can disrupt the ocean's ecosystem and biodiversity.
The hydrogen ion concentration increases.
The hydrogen ion concentration increases.
The hydrogen ion concentration increases.
The hydrogen ion concentration increases.
When the ocean absorbs too much CO2, it becomes more acidic, which can harm marine life such as coral reefs, shellfish, and plankton. This process is known as ocean acidification and can disrupt the overall balance of marine ecosystems, affecting biodiversity and the food chain.
There are different kinds of process that deeply affects the salinity of ocean water. Continental deflections, Coriolis Effect, convection current and also evaporation.
The ocean absorbs heat through the suns rays
The ocean absorbs solar energy due to its high heat capacity and large surface area. This allows it to store and distribute heat effectively, regulating Earth's temperature. Additionally, the ocean's dark surface absorbs sunlight, contributing to the warming effect.
it means that by starting something small you can go to great extents. without those little drops of water how can an ocean exist? all those tiny drops collected together made the ocean
The ocean soaks up energy from the sun through a process called solar radiation, which warms up the surface of the water. The ocean also absorbs heat from the atmosphere through conduction and convection, which helps regulate the Earth's temperature and climate.
There is no such 'triangle'.