Key points Ascent to high altitude imposes an acid‐base challenge in which renal compensation is integral for maintaining pH homeostasis, facilitating acclimatization and helping prevent mountain sicknesses. The time‐course and extent of plasticity of this important renal response during incremental ascent to altitude is unclear. We created a novel index that accurately quantifies renal acid‐base compensation, which may have laboratory, fieldwork and clinical applications. Using this index, we found that renal compensation increased and plateaued after 5 days of incremental altitude exposure, suggesting plasticity in renal acid‐base compensation mechanisms. The time‐course and extent of plasticity in renal responsiveness may predict severity of altitude illness or acclimatization at higher or more prolonged stays at altitude. Abstract Ascent to high altitude, and the associated hypoxic ventilatory response, imposes an acid‐base challenge, namely chronic hypocapnia and respiratory alkalosis. The kidneys impart a relative compensatory metabolic acidosis through the elimination of bicarbonate (HCO3−) in urine. The time‐course and extent of plasticity of the renal response during incremental ascent is unclear. We developed an index of renal reactivity (RR), indexing the relative change in arterial bicarbonate concentration ([HCO3−]a) (i.e. renal response) against the relative change in arterial pressure of CO2 (P aC O2) (i.e. renal stimulus) during incremental ascent to altitude (Δ[ HC normalO3−]normala/ΔP aC normalO2). We aimed to assess whether: (i) RR magnitude was inversely correlated with relative changes in arterial pH (ΔpHa) with ascent and (ii) RR increased over time and altitude exposure (i.e. plasticity). During ascent to 5160 m over 10 days in the Nepal Himalaya, arterial blood was drawn from the radial artery for measurement of blood gas/acid‐base variables in lowlanders at 1045/1400 m and after 1 night of sleep at 3440 m (day 3), 3820 m (day 5), 4240 m (day 7) and 5160 m (day 10) during ascent. At 3820 m and higher, RR significantly increased and plateaued compared to 3440 m (P < 0.04), suggesting plasticity in renal acid‐base compensations. At all altitudes, we observed a strong negative correlation (r ≤ −0.71; P < 0.001) between RR and ΔpHa from baseline. Renal compensation plateaued after 5 days of altitude exposure, despite subsequent exposure to higher altitudes. The time‐course, extent of plasticity and plateau in renal responsiveness may predict severity of altitude illness or acclimatization at higher or more prolonged stays at altitude.

Neurovascular coupling (NVC) is the link between neuronal metabolic activity and regional cerebral blood flow. NVC is responsible for ensuring adequate delivery of nutrients (O2 and glucose) during periods of increased neuronal metabolic demand. Exposure to high‐altitude (HA) elicits ventilatory and acid‐base adjustments for maintaining blood pH. Acute exposure to HA causes hypoxic vasodilation. Hypoxia also drives a ventilatory response, inducing hypocapnia, a potent vasoconstrictor. Whether these dynamic and conflicting responses affect NVC during incremental ascent to HA is unclear.The aim of this project was to assess whether changes in arterial blood gases (ABGs) associated with ascent to HA influences the NVC response. Given that CBF is particularly sensitive to changes in PaCO2, we hypothesized that hypocapnic vasoconstriction during ascent would decrease the NVC response with ascent.10 healthy study participants (21.7±1.3 yrs, 70.46±13.65kg, mean±SD) were recruited as part of a research expedition to Everest base camp, Nepal. Resting posterior cerebral artery velocity (PCAv), ABGs (PaO2, PaCO2), SaO2, arterial blood pH and bicarbonate [HCO3−] were measured at four locations: Calgary (1045m; baseline; BL), Namche (3440m), Deboche (3820m) and Pheriche (4370m). Resting PCAv was measured using transcranial Doppler ultrasound. Arterial blood draws were taken from the radial artery and analysed using a portable blood gas/electrolyte analyser used to monitor changes in ABGs (PaCO2, PaO2, SaO2), pH and [HCO3−] during ascent. NVC was tested via visual stimulation (VS; Strobe light; 6Hz; 30sec on/off ×3). The NVC response was averaged across three VS trials at each location. NVC was quantified as the change (delta) in mean and peak PCAv from baseline, during VS.A one‐factor‐repeated measures analysis of variance (ANOVA) was used to assess for differences in baseline PCAv, NVC, ABGs, blood pH and [HCO3−] between locations. PaO2, PaCO2 and SaO2 were significantly decreased from BL at each altitude (P<0.001, P<0.016 and P<0.013, respectively). No significant differences were found for pH at any location compared to BL (P>0.05) due to reductions in arterial [HCO3−] (P<0.043). No significant differences were found in baseline PCAv between locations (P>0.05) or for mean or peak NVC responses (P>0.085 and P>0.08 respectively).As expected, incremental ascent to HA induced a state of hypoxic hypocapnia, as demonstrated by significant reductions in PaO2, SaO2 and PaCO2, whereas arterial pH was maintained via reductions in [HCO3−]. Our data suggests that NVC remains remarkably intact during incremental ascent to HA in healthy acclimatized individuals. Despite the array of superimposed stressors associated with ascent to HA, CBF and NVC regulation may be a unique function of arterial pH maintenance.This abstract is from the Experimental Biology 2018 Meeting. There is no full text article associated with this abstract published in The FASEB Journal.

Neurovascular coupling (NVC) is the temporal link between neuronal metabolic activity and regional cerebral blood flow (CBF), supporting adequate delivery of nutrients. Exposure to high altitude (HA) imposes several stressors, including hypoxia and hypocapnia, which modulate cerebrovascular tone in an antagonistic fashion. Whether these contrasting stressors and subsequent adaptations affect NVC during incremental ascent to HA is unclear. The aim of this study was to assess whether incremental ascent to HA influences the NVC response. Given that CBF is sensitive to changes in arterial blood gasses, in particular PaCO2, we hypothesized that the vasoconstrictive effect of hypocapnia during ascent would decrease the NVC response. 10 healthy study participants (21.7 ± 1.3 years, 23.57 ± 2.00 kg/m2, mean ± SD) were recruited as part of a research expedition to HA in the Nepal Himalaya. Resting posterior cerebral artery velocity (PCAv), arterial blood gasses (PaO2, SaO2, PaCO2, [HCO3-], base excess and arterial blood pH) and NVC response of the PCA were measured at four pre-determined locations: Calgary/Kathmandu (1045/1400 m, control), Namche (3440 m), Deboche (3820 m) and Pheriche (4240 m). PCAv was measured using transcranial Doppler ultrasound. Arterial blood draws were taken from the radial artery and analyzed using a portable blood gas/electrolyte analyzer. NVC was determined in response to visual stimulation (VS; Strobe light; 6 Hz; 30 s on/off × 3 trials). The NVC response was averaged across three VS trials at each location. PaO2, SaO2, and PaCO2 were each significantly decreased at 3440, 3820, and 4240 m. No significant differences were found for pH at HA (P > 0.05) due to significant reductions in [HCO3-] (P < 0.043). As expected, incremental ascent to HA induced a state of hypoxic hypocapnia, whereas normal arterial pH was maintained due to renal compensation. NVC was quantified as the delta (Δ) PCAv from baseline for mean PCAv, peak PCAv and total area under the curve (ΔPCAv tAUC) during VS. No significant differences were found for Δmean, Δpeak or ΔPCAv tAUC between locations (P > 0.05). NVC remains remarkably intact during incremental ascent to HA in healthy acclimatized individuals. Despite the array of superimposed stressors associated with ascent to HA, CBF and NVC regulation may be preserved coincident with arterial pH maintenance during acclimatization.

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