The mixing time of the world ocean is estimated to be around 1,000 years. This is because the ocean is a complex system with different circulation patterns and factors influencing mixing rates. It can vary in different regions and depths, but the overall estimate is around 1,000 years for complete mixing.
Actual time refers to the precise, exact time, whereas approximate time is an estimation or rough calculation of the time. Actual time is based on specific time measurements, while approximate time provides a general idea of when something is expected to occur.
Deep ocean currents and surface currents do interact and influence each other. While they flow at different depths and have different driving factors (wind for surface currents and density for deep currents), they are connected through the global ocean circulation system. Changes in one can impact the other over time.
The presence or absence of fossils has been used to compare the relative ages of rocks around the world and to arrange sedimentary rocks into a geologic time scale. Eons are the largest intervals of the time scale and range from 540 to 2,050 million years in length
No, the Titanic was never the biggest ship in the world. At the time of its launch in 1912, it was one of the largest, but it has long been surpassed by modern ocean liners and cruise ships in terms of size and capacity.
The spontaneous mixing of particles is called diffusion. It is the movement of molecules from an area of higher concentration to an area of lower concentration, resulting in a more uniform distribution of particles over time.
1600 years
The approximate population of the world today is around 7.9 billion people.
342,000 (approximate) at time of answering in July 2016.
She had an approximate time to arrive at the airport.The approximate time is 10.15, but if you want to know the exact time try the phone service.
The approximate time is 10.15, but if you want to know the exact time try the phone service.
Carbon moves from the atmosphere to the ocean through a process called carbon sequestration. This can happen through physical processes such as diffusion or ocean mixing, as well as biological processes like photosynthesis by phytoplankton. Carbon dioxide in the atmosphere dissolves in the ocean's surface waters, where it can then be stored for long periods of time.
The actual time may vary according to the traffic and weather. The approximate driving time between these two places is 30 hours.
Approximate time of arrival means the estimated time you will arrive at your destination.
Actual time refers to the precise, exact time, whereas approximate time is an estimation or rough calculation of the time. Actual time is based on specific time measurements, while approximate time provides a general idea of when something is expected to occur.
Salinity remains relatively constant over time because there is a balance between the influx of fresh water (from sources like rivers and precipitation) and the evaporation of water from the ocean. Any changes in salinity are usually localized and temporary, as the ocean has a large volume and slow mixing processes.
no effect of mixing was observed for the storage modulus (G′) of gluten for any of the flours.
Globally yes it is, though locally it may take some time.