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The pathophysiology involved in an embolic phenomenon is the passage of the embolus to the pulmonary circulation, initially creating a high ventilation/ perfusion ratio which reduces the end tidal carbon dioxide.
While moving northwestward, the circulation initially remained broad and disorganized, located east of the cycling convection.
Strong flow from across the equator was drawn into the Roger's wind circulation, initially preventing significant development of the precursor disturbance to Tip.
Our data strongly indicate that TG and synthesized cholesterol in the liver are transported into the circulation initially by VLDL and secondarily by LDL.
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In the bubbly flow, slug flow, churn flow and annular flow pattern, with the gas mass flow rate increasing, the natural circulation capability initially increased and then declined.
The entire circulation may initially have a diameter of less than 160 km.
The system had a broad circulation, and initially moved slowly to the east-southeast.
The circulation was initially broad, and dry air temporarily entrained the northwest quadrant of the storm.
Its circulation was initially broad and ill defined, with patches of disorganized convection due to dry air.
However, the low-level circulation was initially poorly defined and difficult to find via weather satellite imagery.
The circulation was initially located east of the main convection, due to the presence of wind shear.
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