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A significant fraction of the solar radiation that reaches the water surface is lost through reflection and backscattering.
If liquid metal front does not continue to expand at all points on its surface and if surface is lost, that is, if any part of the surface experiences contraction, then some entrainment of the surface necessarily occurs.
Therefore, most of infrared radiation emitted from the fiber's inner surface is lost while transmitting in the fiber.
When the properties of a surface patch are encoded as a vector, the information of how these properties distribute over the surface is lost.
In the presence of mCoA (15 μM), application of H2O2 causes little or no change initially, but upon its removal membrane area begins to decline robustly within 1 min and on average more than 25% of the cell surface is lost over 10 min. This pattern suggests that ROS have an acute inhibitory effect on MEND, which is rapidly relieved when H2O2 is removed.
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There is, of course, one potential offset to this — even as the Earth's surface is losing carbon from soils, it also appears to be putting at least some back again due to an increased growth in vegetation, which is being fertilized by more carbon dioxide in the atmosphere, in tern enhancing plant photosynthesis.
Melting polar ice kicks off an ice-albedo (albedo is a measure of how much radiation is reflected) feedback effect, which means as more ice melts, massive areas of reflective surface are lost, speeding up melting and ultimately raising global temperatures and affecting sea levels and global weather patterns.
In some instances, daughter cells with a small apical surface are lost from the epithelial layer.
As w S increased, the more detailed apertures on the grain surface were lost because they were lighter in saturation.
There was irregular increase in density of the distal and inferior portion of the proximal fragment, which was due to newly formed bone, but the superior and posterior portions bordering on the ankle joint were reduced in volume and irregularly in density,' and the shadow of articular surface was lost in almost its entire extent.
Transitioning from aquatic to terrestrial habitats is likely easier than the reverse for sciomyzids because morphological characters associated with air-breathing while under the water's surface are lost rather than gained, and sciomyzids originated and diversified during a general drying period in Earth's history.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com