Sentence examples for increased heat flow from inspiring English sources

There is a fairly uniform background field with areas of increased heat flow associated with the radiogenic granites in southwestern England and the buried granites of northern England.

Instead they tend to cluster, which is possibly linked to an increased heat flow during periods of a more shallow-seated magma column.

3) Due to the increased heat flow and possibly due to the blanketing effect of the atmosphere [e.g., [84]], we assume the mean ocean water temperature to be 70°C.

The increase in thermal conductivity due to the increase of the shape factor could be offset by a negative contribution of increased heat flow resistance at the solid-liquid interface [27].

Once a quartz-weakened patch of crust has begun stretching or folding, increased heat flow from underlying rocks helps drive water out of the crustal minerals, a process that weakens the rocks even further, ensuring that large-scale deformations take place there and not elsewhere.

This indicates that the eruption frequencies follow a bi-modal distribution that most likely stems from the two mechanisms leading to phreatic eruptions: (i) increased heat flow due to more shallow-seated magma, and (ii) pressure build-up in a sealed hydrothermal system.

The theoretical analyses show that all the concepts except for the entransy increase rate decrease monotonically with increasing COP, while only the entransy increase rate increases monotonically with increasing heat flow pumped into the high temperature heat sink.

The amplitude of boiling heat transfer coefficient of test section increases with increasing heat flux and flow rate, while decreases with increasing system pressure.

For example, the Pacific-Arctic Gateway through the Bering Strait would be an ideal monitoring area because of increased heat and freshwater flow, increased marine mammal migration, declining sea ice cover, increased oil and gas exploration, exploratory fisheries in the last decade, and flow of pollutants, especially persistent organic pollutants largely from Asia.

Based on the fabricated device, the sensor has been further developed to include heat-exchanging fingers extending down into the integrated flow channel for increased heat transfer.

The 201 Ma Central Atlantic Magmatic Province (CAMP), a Large Igneous Province (LIP), increased lithospheric heat flow at the end of rifting, produced uplift and doming, and also contributed to deformation and subsequent continental breakup.