In order to evaluate left ventricular (LV) diastolic filling properties at high
altitude, 19 healthy mountaineers were studied by Doppler echocardiography
in a high altitude research laboratory at 4,559 m above sea level. Baseline
examinations were carried out at 490 m. Measurements comprised mitral
inflow velocity parameters and pulmonary artery pressure (PAP, mm Hg).
The two-dimensional (2-D) cross-sectional parasternal short axis view of the
left ventricle revealed a characteristic bulging of the interventricular septum
towards the LV cavity in all subjects at high altitude. Accordingly, end-diastolic
and end-systolic excentricity indexes B/A from 2-D parasternal short
axis view increased significantly. Heart rate, M-mode LV fractional shortening
(FS, %), and PAP increased significantly at 4,559 m. Isovolumic relaxation
time (IVRT, ms), early LV diastolic filling velocity (E, cm/s), deceleration
time of early LV diastolic filling (DT, ms) and late LV diastolic flow velocity
(A, cm/s), all normalized for the corresponding diastolic time interval,
increased significantly at 4,559 m. E/A ratio was significantly depressed at
4,559 m. PAP correlated significantly with LV end-diastolic excentricity index
(r = 0.54, p < 0.001), LV end-systolic excentricity index (r = 0.53, p < 0.01),
IVRT (r = 0.55, p < 0.001) and E/A (r = -0.37, p < 0.05). It is concluded that
the acute rise in PAP at 4,559 m leads to a significant alteration in LV diastolic
mitral inflow velocity properties which is associated to the concomitant
change in LV geometry and the consecutively prolonged LV isovolumic relaxation.