1. Introduction
The survival and well-being of humans rely heavily on water, a precious natural resource and essential nutrient. Water is a fundamental building material of the human body, accounting for approximately 60% of an adult’s body mass, and widely distributed as body fluid in diverse cells, tissues, and organs [
1]. In addition to regulating the body temperature and maintaining electrolyte balance, water is also deeply involved in human metabolism. Any disruption in the water homeostasis within the body, either dehydration or hyperhydration, may lead to adverse health effects [
1].
Therefore, the brain closely monitors and regulates one’s plasma and serum osmolality in collaboration with the kidney and arginine vasopressin (AVP), a hormone released by the hypothalamus and posterior pituitary. When the body is dehydrated, either caused by excessive fluid loss or inadequate fluid intake, AVP is released to increase the water permeability of the distal tubule and collecting duct to promote water reabsorption. Meanwhile, thirst neurons in the anterior cingulate and insular cortex send out thirst signals that urge fluid intake behavior via a negative feedback loop [
2]. If the hydration persists, one could have impeded cognitive function, attention, and working memory in the short term. Excessive water intake or a decrease in plasma or serum osmolality would inhibit AVP release, enabling the excretion of excessive fluid through urination. Hyperhydration, in rare cases, could result in water intoxication characterized by headache, nausea, impaired memory, and even death [
3].
Current evidence suggests that dehydration is a significant threat to human health, yet it is frequently ignored or underestimated. In addition to the acute impacts of dehydration on one’s cognitive function as listed above, chronic dehydration can cause kidney problems and is associated with increasing incidences of a wide range of urological, gastrointestinal, circulatory, neurological, and metabolic disorders [
3]. Adequate and regular fluid intake is the most practical approach to prevent dehydration. However, Sims et al. [
4] reported that only 58% of US males, 48% of US females, 54% of Australian males, and 48% of Australian females met the recommended daily water intake, respectively. In an investigation conducted among young male athletes in China, only 56% and 37.6% of participants met the total drinking fluid (TDF) (1700 mL) and total water intake (TWI) (3000 mL) recommended by the Chinese Nutrition Society (CNS) [
5]. Similar issues seem worldwide even though the recommendation for adequate fluid intake may vary across countries and organizations, therefore urging more effort to improve hydration status and public knowledge of proper hydration, especially among vulnerable populations.
Under the influence of physiological, environmental, and cultural factors, one’s fluid intake behavior may vary, as well as fluid excretion and hydration state, as a consequence. Temperature and humidity, in particular, may significantly impact physical activity level, an important factor in the fluid intake behavior and hydration state. A study of 573 healthy European adults found that higher temperatures were associated with lower physical activity levels, increased plasma and urine osmolality, and induced non-renal water loss, such as perspiration and respiratory loss [
6]. As research evidence suggests, in addition to TWI and fluid loss, temperature and humidity may affect the distribution of different fluid sources. Tani et al. [
7] found that the TWI was the highest in the summer (2331 mL/d) and lowest in the winter (2134 mL/d) among Japanese citizens. As the temperature climbed, the amount of water from food decreased, and drinking fluid increased.
In addition to the increasing amount of insensible water loss through exhalation and perspiration as the temperature climbs and the humidity drops, the physiological adaptation to environmental change might also partially contribute to variations in fluid intake behaviors across seasons. Several studies have discussed the underlying hormonal changes. Timpka et al. [
8] found a J-shaped non-linear association between copeptin (CPP), a surrogate marker for circulating AVP, and the outdoor temperature that the log CPP z-score reached the nadir at 14.3 °C. Previously, they also discovered a distinct seasonal variation of CPP, with a peak in winter and a nadir in late summer [
9]. Goswami et al. [
10] found that concentrations of AVP and aquaporin-2 (AQP-2), a biomarker for the renal system response to AVP, were inversely correlated and significantly varied across seasons. They later concluded that the seasonal behavior of AVP and AQP-2 release is the premise of intracellular and extracellular fluid homeostasis [
11].
Ocean currents, wind zones, air pressure bands, and varied topography shape the unique climate of different continents and regions in the vast expanse of the Earth. However, research and data on the effects of environmental factors, including temperature, humidity, and seasonality, remain limited. Current recommendations for water intake are established based on a mild climate and light physical activity. Little evidence has found application in establishing and refining recommended water intake worldwide. Therefore, we assessed the fluid intake behavior across all four seasons among young adults in Baoding, Hebei, China, hoping to provide supporting data for refining recommended water intake based on environmental factors and to evaluate its intensity and direction of influence on fluid intake behaviors.
2. Materials and Methods
2.1. Study Designs
A prospective cohort study on fluid intake behaviors throughout the four seasons was implemented in 2021 in Baoding, Hebei, China. Each assessment lasted seven consecutive days and followed the same procedure. The four assessments were conducted once each season from 12 to 27 April, 5 to 11 June, 21 to 27 October, and 9 to 15 December, respectively. The division of seasons follows the national standard (GB/T 42074-2022), in which the 5 d moving average of temperatures in spring, summer, fall, and winter are 10–22 °C, ≥22 °C, 10–22 °C, and <10 °C, respectively [
12].
2.2. Ethics
This study has been registered with the Chinese Clinical Trial Registry. The registration number is ChiCTR2100045268.
The Peking University Institutional Review Committee has reviewed and approved the study protocol. The ethical approval project identification code is IRB00001052-21013.
2.3. Participants
Healthy male and female college students aged 18–25 from a university in Baoding, Hebei, China, were recruited by convenient and snowball sampling. Participants who were smokers, habitually consumed alcohol (>20 g/d), and who had gastrointestinal, oral, and other chronic diseases were excluded from this study. All participants gave informed consent.
Required sample sizes were calculated using the following formula for a cross-sectional study:
, in which
α = 0.05,
μα/2 = 1.96. According to previous studies on total drinking fluid among college students in Hebei, the total drinking fluid of the target population was 1135 ± 620 mL in spring and 342 ± 468 mL in winter [
13,
14]. Therefore, the estimated standard error (σ) of total fluid intake among college students in Hebei was 625, and
δ was 158, with an estimated 20% drop-out rate.
. The required sample size was 74.
2.4. Anthropometric Measurements
The height and weight of each participant were measured by trained investigators using a height–weight meter (HDM-300; Huaju, Zhejiang, China). Participants were required to wear light clothing and be barefoot. The height and weight were measured twice, and the mean was recorded to the nearest 0.1 cm and 0.1 kg, respectively. Each participant’s body mass index (BMI) was then calculated with the following equation: BMI = weight (kg)/height
2 (m). The classification of normal (18.5 ≤ BMI < 24.0), underweight (<18.5), overweight (24.0 ≤ BMI < 28.0), and obese (≥28.0) was based on the criteria suggested by the Working Group on Obesity in China [
15].
2.5. Temperature and Humidity
Temperature hygrometers (No.8813, Deli, Zhejiang, China) were placed on the sports ground, classroom, and dormitory. The indoor and outdoor measurements were recorded to the nearest 0.1 °C and 1% by trained investigators thrice daily at 10:00, 14:00, and 20:00.
2.6. Assessment of Fluid Intake
Total fluid intake is composed of drinking fluid and water from food. Drinking fluid intake was assessed for 7 d, and water from food was assessed for 3 d.
2.6.1. Drinking Fluid
For each assessment, participants completed a self-administrative 7 d, 24 h fluid intake questionnaire previously used and tested for reliability and validity [
16,
17]. The questionnaire records the type, volume, time, and place of drinking fluid as described in a previous study [
13]. TDF was classified into plain water and other beverages, including tea, sugar-sweetened beverages (SSBs), and alcohol. The classification of drinking fluid follows the General Standard for Beverages of China (GB/T 1-789-2015) [
18]. The volume of drinking fluid was measured to the nearest 5 mL with a graduated water bottle. Each participant was asked to use a 5-mL-scaled bottle designed for the study when they drank any fluid to ensure accuracy.
2.6.2. Water from Food
Each assessment measured and recorded water from food (WFF) for three consecutive days. The exact amount of each food item consumed was weighed to assess WFF. All consumed foods were weighed before and after participants consumed them. Duplicates of consumed food items were collected. Moisture in collected food samples was measured via the drying method, according to the national standard of GB 5009.3-2016 [
19]. WFF was then calculated using the amount of food consumed and the moisture content of each food item. Types of foods were classified as follows: staple food, dishes, porridge, soup, dairy, and snacks. The volume of dairy consumed (milk and yogurt) was recorded in the 7 d, 24 h fluid intake questionnaire. Moisture in dairy, fruits, and snacks was evaluated according to the China Food Composition Table (6th edition) [
20].
2.7. Statistics
SPSS 26.0 was used for statistical analysis of baseline characteristics and fluid intake. All statistical tests were two-sided; a significance level of <0.05 represents a statistically significant difference. Continuous variables were analyzed using the t-test, one-way analysis of variance (ANOVA), and the non-parametric Kruskal–Wallis H-test. Results are presented as mean ± standard deviation ( ± S).
Repeated-measure analysis of variance (RMANOVA) was implemented to assess the impact of seasons on repeatedly measured variables that were normally or approximately normally distributed. For variables that did not follow a normal distribution, Friedman’s M test, the non-parametric RMANOVA, was implemented to assess the between-group differences by ranks. The Bonferroni-adjusted p-value was applied to post hoc comparisons.
To assess the association between environmental factors and total drinking fluid (TDF), we calculated the daily average of TDF, frequency, volume consumed each time, plain water intake, and beverage intake for the overall, male, and female participants based on data collected from the 4 × 7 d assessment on drinking fluid intake. Spearman rank correlations were then conducted between the collected 4 × 7 d of environmental measurements and the variables computed above. Scatter plots were also built. The general estimating equations (GEEs) with the working correlation matrix set to be the exchangeable mode were implemented to access the exact direction and the strength of the association between the environmental factors and TDF of participants while controlling for confounders.
4. Discussion
In the current study, we assessed the fluid intake behaviors of the same group of participants four times throughout 2021, one in each season. Recruited participants were young adults aged 19–21 at a university in Hebei, China.
In each assessment, participants’ anthropometric measurements were also obtained. When analyzing participants’ anthropometric measurements, we found significant seasonal variations in participants’ weight, height, and BMI as consequences. The variations in participants’ height and weight could also be due to minor deviations in the timing and instrumental reading while measuring in different seasons. Significant variations in fluid intake behaviors of participants with different weight statuses were found when conducting one-way ANOVA, and obese participants tended to have higher TDF and TWI than the rest. However, the association between BMI and TDF could be potentially confounded by gender due to the significant differences in the BMI of male and female participants and the strong collinearity of gender and BMI while we conducted the GEE analysis.
Participants’ fluid intake behaviors, including the TDF, WFF, and TWI, exhibited significant gender differences in all four seasons. Male participants in our study tended to have higher TDF and WFF than females, resulting in a higher TWI. In line with the results from the present study, a recent survey among 2233 Chinese residents in 27 cities reported a significantly higher TFI in males than females regardless of age group [
21]. Wu et al. [
22] also found a significant difference in daily TWI between US males and females based on the National Health and Nutrition Examination Survey 2011–2014 data. According to the results of the GEE analysis, gender was significantly associated with TDF. Males exhibited higher coefficients than females, ranging from 221.0 ± 87.8 to 428.2 ± 105.0 depending on the other variable in the model built.
The higher muscle contents in the body composition of males might contribute to the gender differences in fluid intake behaviors and requirements. Established guidelines of fluid intake worldwide also embody the gender difference. For instance, the recommended TWI by the CNS is 3000 mL/d for males and 2700 mL/d for females. The recommended TDF by the CNS were 1700 mL/d and 1400 mL/d for males and females [
23]. European Food Safety Authority (EFSA) recommended a TWI of 2500 mL/d for males and 2000 mL/d for females [
24]. However, neither the mean TDF of males nor females across the four seasons in the current study met the recommendation of CNS and EFSA. The mean TWI for both male and female participants was also lower than that recommended by CNS throughout the year, urging attention to the importance of adequate fluid intake and establishing an optimal fluid intake habit among the general population.
Regarding environmental factors, we measured and recorded indoor and outdoor temperature and humidity of all 28 survey days. The mean and differences between indoor and outdoor temperature and humidity were also calculated. The statistical analysis suggested that all measurements of temperature significantly varied across different seasons but not that of humidity. Only the difference in indoor and outdoor humidity in summer significantly differed from the rest of the seasons. That could partially explain the negligible influence of humidity on TDF in our study.
According to the results of correlational analysis among daily temperature, humidity, and TDF, the temperature significantly impacted participants’ fluid intake behaviors, including the volume, frequency, and type of fluid consumed. Outdoor temperature, indoor temperature, and MT were all positively correlated with TDF. The GEE analysis indicated that TDF would increase as outdoor temperature, ΔT, or MT climbed. However, only indoor humidity was found to have a weak association with the volume consumed each time among all participants and the plain water intake among females. ΔH was also weakly correlated with the volume consumed each time and plain water intake among males.
Similarly, a previous study in Japan found that the temperature but not humidity were associated with water intake, that for every 1 °C increase in the mean air temperature, the expected TDF would increase by 8.4 g/d when controlled for BMI and gender [
7]. The correlational analysis suggested a correlation between the temperature and humidity. For instance, indoor humidity correlated with indoor temperature (r = 0.375,
p = 0.049) and ΔT (r = −0.460,
p = 0.014). Even though the correlations were weak, summing up with the strong collinearity we discovered later in the GEE analysis, temperature might still confound the correlation between indoor humidity and TDF.
Fluid intake behaviors may also vary according to seasons, especially the volume and the composition of TWI. The results of MANOVA showed significant differences in TDF (
F(2.62) = 9.36,
p < 0.001), WFF (
F(2.61) = 17.21,
p < 0.001), and TWI (
F(2.37) = 42.29,
p < 0.001) across the four seasons. TDF in summer (1219 ± 502) was significantly higher than in fall (1082 ± 475,
p = 0.015) and winter (1082 ± 475,
p = 0.009) but did not significantly differ from that in spring (1182 ± 594,
p = 1.000). As results from GEE analysis showed, when controlled for gender, summer (β = 236.1,
p < 0.001) had the leading β among all seasons with winter as the reference. The β of spring and fall were 178.7 (
p < 0.001) and 79.0 (
p = 0.018), respectively. Consistent with our findings, Malisova et al. [
25] concluded that there was no significant difference in the water balance between summer and winter among Greek residents, while TDF was significantly higher in summer than in winter, and the proportion of WFF in winter outran that in summer.
We also analyzed the volume and proportion of specific sources of fluid intake. The results indicated that the proportion of TWI from TDF was significantly higher in summer than in fall and winter. The volume but not the proportion of WFF in spring, specifically the volume of water from dishes and porridge, was significantly higher than in the resting seasons. However, Tani et al. [
7] concluded that for every 1 °C increase in the mean air temperature, the expected WFF would decrease by 3.1 g/d. The contradicting results might be attributed to the significant increase in other beverage intake in summer. Correspondingly, a survey conducted in Korea showed that plain water and beverage intake increases by 19.7% and 7.6% in summer compared to spring, though we did not find a significant difference in the volume of plain water intake between spring and summer [
26]. Possibly due to differences in dietary habits and culture, the proportion of WFF in TWI in the present study was also higher across the four seasons in our study than the data from previous assessments worldwide. For instance, only 18% of the TWI intake of US citizens were WFF based on 1999–2006 NHANES data [
27]. The proportion of WFF in TWI among UK and French citizens was 27% and 36%, respectively [
28].
Previous studies exploring the impact of seasonality, temperature, and humidity on fluid intake behaviors rarely conducted assessments in all four seasons. Otherwise, data from national-based dietary surveys were utilized and analyzed. Limitations and imprecisions could be found in measuring and estimating the exact amount of fluid intake. In the present study, composed of four assessments of the same group of participants, we employed a specifically designed 7 d, 24 h fluid intake questionnaire that had been proven reliable and valid in our past study. Participants were also trained to record the type, volume, time, and place of drinking fluid immediately after. The exact amount of WFF was calculated by weighting the consumed amount of each food item and measuring moisture in the duplicate of each food item via the drying method, significantly improving the accuracy and precision of TWI measurement. In addition, the current study analyzed the seasonal differences of TWI, TDF, and WFF and further investigated the association between participants’ fluid intake behaviors and environmental factors, including indoor and outdoor temperature and humidity. Limitations of the present study are that participants were prescribed to only participate in light physical activity for quality control. However, physical activity is essential in fluid intake behaviors and might be significantly influenced by the environment. By minimizing the confounding effect of physical activity, we also lose the chance to explore the impact of physical activity on participants’ fluid intake behaviors and the underlying interaction of environmental factors and physical activities, as little evidence has been established on the interactive effects of physical activity and environmental factors on one’s fluid intake behavior and overall hydration state.
5. Conclusions
The current study verified the association between fluid intake behaviors and environmental factors. Even though it was possibly due to the relatively steady humidity in our survey site across the year, no significant association was found between humidity and fluid intake behaviors, and seasonality and temperature could still significantly impact the total volume of fluid intake and the proportion of different fluid sources in TWI. Gender was the other factor significantly associated with fluid intake behaviors. Even though previous research suggested that overweight and obesity were associated with higher TWI, urine osmolality, and risk of dehydration, gender possibly confounded the correlation between BMI and fluid intake behaviors in the current study.
In subsequent studies, an in-depth exploration of one’s anthropometric measurements, including height, weight, BMI, body surface area, and blood pressure, should be completed, along with analyses of their association and water homeostasis within the body. TDF increases as temperature elevates and is the highest in summer. Males tended to have higher TWI, WFF, and TDF across all four seasons. Their TDF could also be impacted by temperature to a greater extent than that of females.
Future studies could incorporate biomarkers of hydration status into the analysis to obtain a more comprehensive and systematic understanding of how environmental factors may affect one’s hydration status and water homeostasis, thereby finding implications in refining the recommendation of fluid intake in different seasons.