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UBC‐Nepal Expedition: Haemoconcentration underlies the reductions in cerebral blood flow observed during acclimatization to high altitude

New Findings What is the central question of this study? The aim was to evaluate the degree to which increases in haematocrit alter cerebral blood flow and cerebral oxygen delivery during acclimatization to high altitude. What is the main finding and its importance? Through haemodilution, we determi...

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Published in:Experimental physiology 2019-12, Vol.104 (12), p.1963-1972
Main Authors: Howe, Connor A., Ainslie, Philip N., Tremblay, Joshua C., Carter, Howard H., Patrician, Alex, Stembridge, Mike, Williams, Alex, Drane, Aimee L., Delorme, Eric, Rieger, Mathew G., Tymko, Michael M., Gasho, Chris, Santoro, Antoinette, MacLeod, David B., Hoiland, Ryan L.
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cited_by cdi_FETCH-LOGICAL-c4504-49e1f3a7a7462f77600c312c4834cacb8477caf5259fe7d37f40abdf37e9aa393
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container_end_page 1972
container_issue 12
container_start_page 1963
container_title Experimental physiology
container_volume 104
creator Howe, Connor A.
Ainslie, Philip N.
Tremblay, Joshua C.
Carter, Howard H.
Patrician, Alex
Stembridge, Mike
Williams, Alex
Drane, Aimee L.
Delorme, Eric
Rieger, Mathew G.
Tymko, Michael M.
Gasho, Chris
Santoro, Antoinette
MacLeod, David B.
Hoiland, Ryan L.
description New Findings What is the central question of this study? The aim was to evaluate the degree to which increases in haematocrit alter cerebral blood flow and cerebral oxygen delivery during acclimatization to high altitude. What is the main finding and its importance? Through haemodilution, we determined that, after 1 week of acclimatization, the primary mechanism contributing to the cerebral blood flow response during acclimatization is an increase in haemoglobin and haematocrit. The remaining contribution to the cerebral blood flow response during acclimatization is likely to be attributable to ventilatory acclimatization. At high altitude, an increase in haematocrit (Hct) is achieved through altitude‐induced diuresis and erythropoiesis, both of which result in increased arterial oxygen content. Given the impact of alterations in Hct on oxygen content, haemoconcentration has been hypothesized to mediate, in part, the attenuation of the initial elevation in cerebral blood flow (CBF) at high altitude. To test this hypothesis, healthy men (n = 13) ascended to 5050 m over 9 days without the aid of prophylactic acclimatization medications. After 1 week of acclimatization at 5050 m, participants were haemodiluted by rapid saline infusion (2.10 ± 0.28 l) to return Hct towards pre‐acclimatization values. Arterial blood gases, Hct, global CBF (duplex ultrasound) and haemodynamic variables were measured after initial arrival at 5050 m and after 1 week of acclimatization at high altitude, before and after the haemodilution protocol. After 1 week at 5050 m, the Hct increased from 42.5 ± 2.5 to 49.6 ± 2.5% (P 
doi_str_mv 10.1113/EP087663
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The aim was to evaluate the degree to which increases in haematocrit alter cerebral blood flow and cerebral oxygen delivery during acclimatization to high altitude. What is the main finding and its importance? Through haemodilution, we determined that, after 1 week of acclimatization, the primary mechanism contributing to the cerebral blood flow response during acclimatization is an increase in haemoglobin and haematocrit. The remaining contribution to the cerebral blood flow response during acclimatization is likely to be attributable to ventilatory acclimatization. At high altitude, an increase in haematocrit (Hct) is achieved through altitude‐induced diuresis and erythropoiesis, both of which result in increased arterial oxygen content. Given the impact of alterations in Hct on oxygen content, haemoconcentration has been hypothesized to mediate, in part, the attenuation of the initial elevation in cerebral blood flow (CBF) at high altitude. To test this hypothesis, healthy men (n = 13) ascended to 5050 m over 9 days without the aid of prophylactic acclimatization medications. After 1 week of acclimatization at 5050 m, participants were haemodiluted by rapid saline infusion (2.10 ± 0.28 l) to return Hct towards pre‐acclimatization values. Arterial blood gases, Hct, global CBF (duplex ultrasound) and haemodynamic variables were measured after initial arrival at 5050 m and after 1 week of acclimatization at high altitude, before and after the haemodilution protocol. After 1 week at 5050 m, the Hct increased from 42.5 ± 2.5 to 49.6 ± 2.5% (P &lt; 0.001), and it was subsequently reduced to 45.6 ± 2.3% (P &lt; 0.001) after haemodilution. Global CBF decreased from 844 ± 160 to 619 ± 136 ml min−1 (P = 0.033) after 1 week of acclimatization and increased to 714 ± 204 ml min −1 (P = 0.045) after haemodilution. Despite the significant changes in Hct, and thus oxygen content, cerebral oxygen delivery was unchanged at all time points. Furthermore, these observations occurred in the absence of any changes in mean arterial blood pressure, cardiac output, arterial blood pH or oxygen saturation pre‐ and posthaemodilution. 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To test this hypothesis, healthy men (n = 13) ascended to 5050 m over 9 days without the aid of prophylactic acclimatization medications. After 1 week of acclimatization at 5050 m, participants were haemodiluted by rapid saline infusion (2.10 ± 0.28 l) to return Hct towards pre‐acclimatization values. Arterial blood gases, Hct, global CBF (duplex ultrasound) and haemodynamic variables were measured after initial arrival at 5050 m and after 1 week of acclimatization at high altitude, before and after the haemodilution protocol. After 1 week at 5050 m, the Hct increased from 42.5 ± 2.5 to 49.6 ± 2.5% (P &lt; 0.001), and it was subsequently reduced to 45.6 ± 2.3% (P &lt; 0.001) after haemodilution. Global CBF decreased from 844 ± 160 to 619 ± 136 ml min−1 (P = 0.033) after 1 week of acclimatization and increased to 714 ± 204 ml min −1 (P = 0.045) after haemodilution. Despite the significant changes in Hct, and thus oxygen content, cerebral oxygen delivery was unchanged at all time points. Furthermore, these observations occurred in the absence of any changes in mean arterial blood pressure, cardiac output, arterial blood pH or oxygen saturation pre‐ and posthaemodilution. 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The aim was to evaluate the degree to which increases in haematocrit alter cerebral blood flow and cerebral oxygen delivery during acclimatization to high altitude. What is the main finding and its importance? Through haemodilution, we determined that, after 1 week of acclimatization, the primary mechanism contributing to the cerebral blood flow response during acclimatization is an increase in haemoglobin and haematocrit. The remaining contribution to the cerebral blood flow response during acclimatization is likely to be attributable to ventilatory acclimatization. At high altitude, an increase in haematocrit (Hct) is achieved through altitude‐induced diuresis and erythropoiesis, both of which result in increased arterial oxygen content. Given the impact of alterations in Hct on oxygen content, haemoconcentration has been hypothesized to mediate, in part, the attenuation of the initial elevation in cerebral blood flow (CBF) at high altitude. 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Despite the significant changes in Hct, and thus oxygen content, cerebral oxygen delivery was unchanged at all time points. Furthermore, these observations occurred in the absence of any changes in mean arterial blood pressure, cardiac output, arterial blood pH or oxygen saturation pre‐ and posthaemodilution. 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source Wiley Online Library Open Access
subjects Acclimatization
Altitude
Blood flow
Blood pressure
Cerebral blood flow
Diuresis
Erythropoiesis
Gases
haematocrit
haemodilution
Hematocrit
high‐altitude
hypoxia
Ultrasound
title UBC‐Nepal Expedition: Haemoconcentration underlies the reductions in cerebral blood flow observed during acclimatization to high altitude
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