UNLABELLED: Study Type--Prognosis (cohort series) Level of Evidence 2b. What's known on the subject? and What does the study add? Epidemiologic studies have shown that warmer climates are associated with increased incidence of nephrolithiasis. Many hypothesize that this is due to dehydration and lower urine volumes. The current study of stone formers reports that greater temperatures are associated with significant increases in urine calcium which may shed light on the mechanism underlying the increased stone incidence associated with increased ambient temperature. OBJECTIVE: • To understand the effects of temperature, humidity and season of year on 24-h urine composition in patients with nephrolithiasis. PATIENTS AND METHOD: • A retrospective review was performed of patients evaluated at four metabolic stone clinics. • Multivariate linear regression models examined the relationship between mean temperature, average humidity, season of year and 24-h urine composition. • Multivariate models adjusted for known risk factors for stone disease. • Mean temperature and average humidity data were obtained from http://www.weatherunderground.com based on patient-provided addresses. RESULTS: • A total of 599 patients were included in the study, comprising 239 women and 360 men with a mean age of 53.6 years (sd 15.0). • Mean temperature was 16.9 °C (sd 4.8, range -21.1 to 38.3 °C) and average humidity was 58.1% (sd 23.5, range 11-100%). • On multivariate linear regression, increasing temperature was associated with increasing urine calcium (β = 11.3, 95% CI 2.2-20.0), super-saturation of calcium oxalate (β = 0.6, 95% CI 0.2-0.9), super-saturation of calcium phosphate (β = 0.14, 95% CI 0.03-0.2), and decreasing urine sodium (β = -5.2, 95% CI -10.3 to -0.1). • As seasons become warmer (i.e. from winter to autumn to spring to summer), changes were increased urine volume (β = 0.09, 95% CI 0.01-0.2) and decreased super-saturation of calcium phosphate (β = -0.2, 95% CI -0.3 to -0.03). • There were no associations between quintile of humidity and any 24-h urine constituents. CONCLUSIONS: • Increasing temperature may increase stone risk by increasing urine excretion of calcium, and the super-saturation of calcium oxalate and calcium phosphate. • These findings were independent of humidity and of season of year. • This appears to be related to a physiological impact of temperature itself, rather than to geographic location.
UNLABELLED: Study Type--Prognosis (cohort series) Level of Evidence 2b. What's known on the subject? and What does the study add? Epidemiologic studies have shown that warmer climates are associated with increased incidence of nephrolithiasis. Many hypothesize that this is due to dehydration and lower urine volumes. The current study of stone formers reports that greater temperatures are associated with significant increases in urine calcium which may shed light on the mechanism underlying the increased stone incidence associated with increased ambient temperature. OBJECTIVE: • To understand the effects of temperature, humidity and season of year on 24-h urine composition in patients with nephrolithiasis. PATIENTS AND METHOD: • A retrospective review was performed of patients evaluated at four metabolic stone clinics. • Multivariate linear regression models examined the relationship between mean temperature, average humidity, season of year and 24-h urine composition. • Multivariate models adjusted for known risk factors for stone disease. • Mean temperature and average humidity data were obtained from http://www.weatherunderground.com based on patient-provided addresses. RESULTS: • A total of 599 patients were included in the study, comprising 239 women and 360 men with a mean age of 53.6 years (sd 15.0). • Mean temperature was 16.9 °C (sd 4.8, range -21.1 to 38.3 °C) and average humidity was 58.1% (sd 23.5, range 11-100%). • On multivariate linear regression, increasing temperature was associated with increasing urine calcium (β = 11.3, 95% CI 2.2-20.0), super-saturation of calcium oxalate (β = 0.6, 95% CI 0.2-0.9), super-saturation of calcium phosphate (β = 0.14, 95% CI 0.03-0.2), and decreasing urine sodium (β = -5.2, 95% CI -10.3 to -0.1). • As seasons become warmer (i.e. from winter to autumn to spring to summer), changes were increased urine volume (β = 0.09, 95% CI 0.01-0.2) and decreased super-saturation of calcium phosphate (β = -0.2, 95% CI -0.3 to -0.03). • There were no associations between quintile of humidity and any 24-h urine constituents. CONCLUSIONS: • Increasing temperature may increase stone risk by increasing urine excretion of calcium, and the super-saturation of calcium oxalate and calcium phosphate. • These findings were independent of humidity and of season of year. • This appears to be related to a physiological impact of temperature itself, rather than to geographic location.
Authors: Kai B Dallas; Simon Conti; Joseph C Liao; Mario Sofer; Alan C Pao; John T Leppert; Christopher S Elliott Journal: J Endourol Date: 2017-09-21 Impact factor: 2.942
Authors: Robert L Haddock; David R Olson; Lorraine Backer; Josephine Malilay Journal: Int J Environ Res Public Health Date: 2016-05-24 Impact factor: 3.390
Authors: Byung Hoon Chi; In Ho Chang; Se Young Choi; Dong Churl Suh; Chong Won Chang; Yun Jung Choi; Seo Yeon Lee Journal: J Korean Med Sci Date: 2017-06 Impact factor: 2.153