Introduction: Cardiovascular diseases (CVD) are drastically affected by environmental changes, and this makes it extremely important to understand how its deleterious health effects happen and identify possible vulnerable populations. Higher concentrations of low-density lipoprotein (LDL-C) are found in periods of lower temperatures, and this acts directly in the formation of atherosclerotic plaques. Objectives: To assess the impact of cold waves on LDL-C concentrations in patients who sought medical attention in Campinas-SP, from 2008 to 2018. Our secondary aim was to predict future cold waves. Methods: Results of LDL-C exams, from the Campinas Municipal Laboratory and data of minimum and maximum air temperature (°C) were evaluated. Cold waves were defined as at least 3 consecutive days with Tmin and Tmax below its 10th percentiles, considering temperature data from 1961 to 1990. The data were stratified into sex and age groups. We separated the data into cold wave and control days and compared LDL-C levels above reference value (LARV) using Mann-Whitney U and probability density plots. We also compared the control group with lags from 0 to 10 to analyse retarded effects of the cold wave. Regarding the prediction of cold waves, we modelled historical weather data using an auto-regressive model and used a regional climate model (ETA) to predict the occurrences of cold waves in the future. Results: In the evaluated period, 9 cold waves were found, which impacted an increase of 3.32% more people with LARV in the group of adult women for lag 2, 9.27% for elderly women in lag 0 and 11.45% for elderly men in lag 4. Prediction of cold waves using historical data is computationally expensive and inaccurate if time series residues are not considered. Use of a regionalized climate model showed better results. Conclusion: These analyses point to the influence of cold waves on LDL-C concentrations in adult women and also in elderly men and women. Cold waves tend to be less frequent in the future.
Introdução: As doenças cardiovasculares (DCV) são drasticamente afetadas pelas mudanças ambientais, e isso torna extremamente importante entender como seus efeitos deletérios à saúde acontecem e identificar possíveis populações vulneráveis. Maiores concentrações de lipoproteína de baixa densidade (LDL-C) são encontradas em períodos de temperaturas mais baixas, e isso atua diretamente na formação de placas ateroscleróticas. Objetivo: Avaliar o impacto das ondas de frio nas concentrações de LDL-C em pacientes que procuraram atendimento médico em Campinas-SP, de 2008 a 2018. Estabelecemos como objetivo secundário a predição de ondas de frio. Métodos: Foram avaliados os resultados dos exames de LDL-C, do Laboratório Municipal de Campinas, e os dados de temperatura mínima (Tmin) e máxima (Tmax) do ar (°C). Ondas de frio foram definidas como pelo menos 3 dias consecutivos com Tmin e Tmax abaixo de seus percentis 10, considerando dados de temperatura de 1961 a 1990. Os dados foram estratificados em sexo e faixa etária. Separamos os dados em dias de onda de frio e dias controle e comparamos os níveis de LDL-C acima do valor de referência (AVR), usando o teste U de Mann-Whitney e gráficos de densidade de probabilidade. Também comparamos o grupo controle com efeito lag de 0 a 10 dias para analisar os efeitos de atraso da onda de frio. Em relação à predição das ondas de frio, foi feita uma modelagem dos dados climáticos históricos por meio de um modelo auto-regressivo. Além disso, utilizamos um modelo climático regional (ETA) para prever as próximas ocorrências de ondas de frio. Resultados: No período avaliado, foram encontradas 9 ondas de frio, o que impactou em um aumento de 3,32% a mais de pessoas com os níveis de LDL-C AVR no grupo de mulheres adultas para o lag 2, 9,27% para idosas no lag 0 e 11,45% para homens idosos no lag 4. Predição de ondas de frio utilizando dados históricos tem um elevado custo computacional e pode ser ineficaz caso os resíduos da série temporal não sejam considerados. O modelo climático regionalizado mostrou melhores resultados. Conclusão: Essas análises apontam para a influência das ondas de frio nas concentrações de LDL-C em mulheres adultas e também em homens e mulheres idosos. As ondas de frio tendem a ser menos frequentes no futuro.
- Daniela Souza de Oliveiraa, b
- Júlia Perassolli De Lázarib
- Thiago Ribas Bellab, c
- Welington Corozollac
- Paula Dornhofer Paro Costab
- Ana Maria Heuminski de Avilaa
- Eliana Cotta de Fariac
a Center for Meteorological and Climatic Research Applied to Agriculture - UNICAMP, Brasil
b Department of Computer Engineering and Industrial Automation - FEEC/UNICAMP, Brasil
c Department of clinical pathology - FCM/UNICAMP, Brasil
The reports of the Brazilian Panel on Climate Change (PBMC) and the Intergovernmental Panel on Climate Change (IPCC) were unanimous in revealing that South America and Brazil already have records of climate change predicted in climate models (1) and highlight that the changes associated with global warming can alter the frequency, intensity, duration and timing of extreme events, resulting in extreme environmental conditions, even never seen before (2).
The World Health Organization (WHO) concluded that climate change is expected to cause approximately 250,000 additional deaths per year between 2030 and 2050 (3). Studies show that the impacts of climate change are disproportionately affecting the health of populations, and especially of the vulnerable population (4).
Cardiovascular diseases (CVD) are drastically affected by environmental changes, and this makes it extremely important to understand how and what are the components of the environment that increase cardiovascular risk (5,6).
Classified as the leading cause of death in the world, CVDs represent almost 32% of all causes of death in women and 27% in men (7). Low temperature-related mortality places a major burden on public health spending (8) and cardiovascular events, such as acute myocardial infarction (AMI) and stroke, present a seasonal pattern, with higher rates in winter than in other seasons (9,10). In the northern and southern hemispheres, cholesterol concentrations of low-density lipoprotein (LDL-C), also popularly known as “bad cholesterol” are slightly higher in winter when compared to other seasons (11,12) and plasma lipids and lipoproteins are essential components in the pathogenesis and progression of atherosclerosis (a chronic inflammatory disease that affects the wall of large and medium-sized arteries, characterized by a long asymptomatic phase (which can last for decades) resulting from the accumulation of lipids), especially those situations of increased LDL-C (13).
The formation of atherosclerotic plaque begins with the aggression to the vascular endothelium by several risk factors, such as dyslipidemia (increased or reduced concentrations of lipids or lipoproteins), hypertension or smoking. As a consequence, endothelial dysfunction increases the permeability of the intima layer to plasma lipoproteins, favoring their retention in the subendothelial space. Retained, the LDL particles undergo oxidation, causing the exposure of several neoepitopes, making them immunogenic. The deposition of lipoproteins in the arterial wall, a key process at the beginning of atherogenesis, occurs in proportion to the concentration of these lipoproteins in the plasma (13).
Even in patients at low risk for cardiovascular disease, studies suggest that LDL-C at concentrations above the reference value (≥160 mg/dL) is associated with a 50% increase in the relative risk of CVD mortality (14), large clinical trials indicate that the reduction of LDL-C by 1 mmol/L (± 39 mg/dL) would reduce the risk for some cardiovascular outcomes by 22% (15) and that the 20 °C variation in air temperature may result in a change of about 20% in plasma lipid levels (16).
In a scenario where the effects of climate change and the frequency of extreme events make it more evident and intense, there is an urgent need to investigate and develop analytical tools and predictive models that reveal their effects on human health, as well as being able to provide information accessible to health professionals and public health policymakers, which can be used as indicators to define strategies for the perception of the problem by society and for the implementation of actions to prevent and mitigate its pathological effects.
In this context, this study aimed to analyse the impact of cold waves on LDL-C concentrations of patients who sought medical care at basic health units (UBS) in the city of Campinas-SP, from 2008 to 2018, comprising an 11-year time series. Additionally, we modelled historical weather data and used climate models to predict the occurrences of cold waves in the future.
Question: Do cold waves increase LDL-C levels?
Null Hypothesis: Cold waves do not increase LDL-C levels.
Hypothesis: Cold waves increase LDL-C levels.
To assess the impact of cold waves on LDL-C concentrations in patients who sought medical attention in Campinas-SP, from 2008 to 2018. Our secondary aim was to predict future cold waves.
Database | Web Address | Description and Usage |
---|---|---|
Campinas Municipal Laboratory | LDL Database | Database with LDL-c concentrations data from LMC-Campinas (2008-2018) |
Agronomic Institute of Campinas | - | Database with cold waves using IAC data (1961 - 2018) |
Agronomic Institute of Campinas | - | Database with heat waves using IAC data (1961 - 2018) |
Projections from ETA | https://bit.ly/ETA_TMIN | Database with predicted minimum temperatures from PROJETA (2019 - 2050) - ETA 5km RCP4.5, sudesteD2-BR, HADGEM2-ES |
Projections from ETA | https://bit.ly/ETA_TMAX | Database with predicted maximum temperatures from PROJETA (2019 - 2050) - ETA 5km RCP4.5, sudesteD2-BR, HADGEM2-ES |
Tool | Web Address | Description and Usage |
---|---|---|
Google Colab | https://colab.research.google.com | Jupyter notebooks environment from google, used to write shared scripts |
LDL-C concentrations data from the Campinas Municipal Laboratory of Clinical Pathology (LMC-Campinas) between the years 2008 to 2018, where laboratory tests are performed on individuals seen at 63 basic health units in Campinas.
The database used in this work consisted of daily minimum (Tmin) and maximum temperatures (Tmax) from the weather station of the Agronomic Institute of Campinas (located at latitude 22°52’ S and longitude 47°4’ W) from 1961 to 2018. First, to estimate the impact of cold waves on LDL-C concentrations, data from the period of 2008 to 2018 was used. Further, the period of 1989 to 2018 was used to forecast the temperature time series. The detection of cold waves was based on the data from 1961 - 1990 (climatological normal).
Daily Tmax and Tmin projections for the period of 2018 - 2050 (Latitude: 22°51' S, Longitude: 47°3' W) were obtained from the regionalized ETA climate model available on the PROJETA platform for the climatic scenario: 05 km, RCP4.5, sudesteD2-BR, HADGEM2-ES.
Cold waves were defined as at least 3 consecutive days with Tmin and Tmax below its 10th percentiles. We calculated the percentiles (P10-Tmin and P10-max) for each day using the historical time series from 1961 to 1990 and a time window of 15 days, centered in the day of interest. For example, to calculate the P10-Tmin for 08/01 we used a time window from 01/01 to 15/01, for all 30 years in the historical series (see supplement). We used a Python library to compute cold waves: Extreme_Waves.py.
Patients were stratified into different age groups: young (<20 years old), adults (20 - 65 years old), Elderly (>65 years old), Male and Female.
We separated the data into two groups: days under influence of a cold wave and control days. Control days were defined as the ones without influence of hot or cold waves. We used a density probability plot to analyse the percentage of exams with LDL-C above reference level. We applied the Mann Whitney U test, a nonparametric test, to compare these groups because our data distribution was not normal. We also compared the control group with stratified LDL-C results collected k days after a cold spell, with k ranging from 0 to 10, in order to analyse retarded effects of the cold wave.
All analysis were done using Python and the libraries scipy, numpy, pandas, matplotlib and statsmodels.
In order to estimate the occurrences of cold waves in the future, we applied two different approaches: (1) use of historical data from IAC weather station to model future climate data; (2) use of data from the ETA regionalized model for geographic coordinates near IAC.
For the first method, we divided the data in training (1989 to 2013) and test datasets (2014 - 2018) and converted it into weekly aggregation. Seasonal ARIMA (Auto-Regressive Integrated Moving Average) was applied to the training set, using the Akaike information criterion (AIC) to choose the best model and selecting a period of 52 weeks to account for data yearly seasonality. After the implementation of the model for both maximum and minimum temperatures, we calculated the error between the original data and the test set and estimated the daily temperatures for the next 10 years (2019 to 2028). Using the predicted temperatures, we applied the algorithm for detection of cold waves. Noise was also added to the model to make it more realistic.
For the second method, we computed cold waves using daily temperature data obtained from the ETA climate model. Cold wave metrics of quantity (CWN - number of cold wave events per year), duration (CWD - longest duration in days of cold waves per year) and frequency (CWF - number of days under cold waves per year) were generated considering historical data (2008 - 2018) and projections (2019 - 2050).
The analysis can be found at the 03_LDL_above_average.
Exclusively the female group showed significant differences for our analysis, being them on lags 2, 7 and 9. Intriguingly, the difference between the group on cold waves and the control showed peculiar results, suggesting that the group under cold waves has lower number of people with LDL-C concentrations above reference value when compared to the control group: -11.42%, -7.43% and -8.17% for lags 2, 7 and 9 respectively. Numerous mechanisms of lipid transport and metabolism may be involved. It is known that children and adolescents undergo considerable sex-specific changes during physical growth and sexual maturation and differ significantly between pubertal stages. This phase is marked by metabolic instability with large hormonal fluctuations in growth and sexual maturation, directly affecting lipid and lipoprotein concentrations (17). It is likely that this group is not influenced by thermal stress under cold waves, but there is nothing clear in the literature to corroborate these findings.
SUBSET | lag | Cold | n1 | Nor. | n2 | Diff | p |
---|---|---|---|---|---|---|---|
Under 20 female | 2 | 25.58 | 83 | 37.00 | 18771 | -11.42 | 0.017 |
Under 20 female | 7 | 29.57 | 106 | 37.00 | 18771 | -7.43 | 0.012 |
Under 20 female | 9 | 28.82 | 99 | 37.00 | 18771 | -8.17 | 0.021 |
Significant difference was found only for lag 2. This indicates that the physiological response of the group had greater proportions two days after the beginning of the wave. The group under cold waves showed a higher number of people (3.32% more) with LDL-C concentrations above reference value, when compared to the control group.
We emphasize that only the female group presented a significant difference in our analysis, showing that they are more susceptible to cold waves. The possible mechanism behind these findings is related to the cardioprotective function of testosterone present in higher concentrations in male group. Testosterone levels are inversely correlated with LDL-C and recent epidemiological studies indicate that low serum testosterone levels are associated with more atherosclerotic and CVD events (18,19).
SUBSET | lag | Cold | n1 | Nor. | n2 | Diff | p |
---|---|---|---|---|---|---|---|
Between 20 and 65 female | 2 | 46.88 | 879 | 43.56 | 157878 | 3.32 | 0.004 |
For females, significant difference, 9.27%, 7.39% and 4.06%, was found for lags 0, 2 and 7, respectively. These findings indicate that the physiological outcomes in response to thermal stress caused by the cold wave start simultaneously. It is worth mentioning that the physiological response continues to happen until the seventh day after the beginning of the cold wave. The male group exhibits significant difference only for lag 4.
By aging the deterioration of the organism damages several functions necessary for the survival and adaptation to the environment and its oscillations (20).
In addition to functional limitations, such as a decline in muscle strength, coordination and cognitive function due to illness, chronic illness or injury, changes in concentrations of growth hormone, adrenocorticotropic, thyroid-stimulating, dehydroepiandrosterone and aldosterone hormones occur; there is also loss of skeletal striated muscles that may reduce basal metabolic rate in men and women (21). Ovarian secretion of estrogen in women, and to a lesser extent, of androgen, decrease abruptly from the sixth decade of life; also, from the 75 years of age, serum concentrations of follicle stimulating hormone and luteinizing hormone gradually decline (21,22). For males, the testicular function gradually declines with increasing age, with reduction in concentrations of serum and total and free testosterone (21,23).
It should be emphasized that with advancing age, the metabolism reduces its plasticity and the ability to maintain homeostasis in response to climatic variations (24,25), calling attention and highlighting possible risk groups, the elderly women.
SUBSET | lag | Cold | n1 | Nor. | n2 | Diff | p |
---|---|---|---|---|---|---|---|
Over 65 male | 4 | 47.26 | 87 | 35.81 | 40448 | 11.45 | 0.025 |
Over 65 female | 0 | 52.76 | 253 | 43.49 | 52007 | 9.27 | 0.000 |
Over 65 female | 2 | 50.89 | 228 | 43.49 | 52007 | 7.39 | 0.016 |
Over 65 female | 7 | 47.55 | 290 | 43.49 | 52007 | 4.06 | 0.026 |
Modeling can be found at the Climate_modelling.
Computation of cold waves can be found at Future_ColdWaves.
After converting training (1989 - 2013) and test (2014 - 2018) datasets of daily temperatures (maximum and minimum) into weekly aggregation, we performed a search using ‘auto-arima’ function in Python and selected the parameters for our model according to the best (smaller) AIC. A SARIMA model has seven hyper-parameters, three are trend parameters (p, d, q) and four are seasonal parameters (P, D, Q, S). The S was chosen according to the yearly seasonality of our data (S = 52 weeks). Two models were generated, one for Tmax and another for Tmin, and the search resulted in the same parameters for both models: (1,1,1)x(0,1,1,52). After implementing the model, we found AIC for Tmax equal to 5252 and for Tmin equal to 4266. When the model predictions were compared to the test dataset we found mean squared errors of 2.52 and 1.72, respectively, for Tmax and Tmin.
Further, we used the generated models to estimate the daily temperatures for the next 10 years (2019 to 2028), using interpolation to convert data back to daily. With the predicted temperatures, we applied the algorithm for detection of cold waves using the climatological normal of 1961 - 1990 which resulted in no cold waves because our model did not consider the data residues. Due to this problem, we decided to add a random noise to the data, to check if we could detect cold waves. The noise was estimated from the data and added to the temperature time series. After that, the computation of cold waves was successful.
Data processing of ETA model and computation of cold waves can be found at Future_ColdWaves.
After computation of cold waves using the projections of daily temperature data obtained from ETA regionalized climate (2019 - 2050), the annual cold wave metrics were calculated (CWN, CWD and CWF). Those metrics are presented in the following figures, along with the cold wave metrics from 2008 - 2018 in order to provide a comparison between those periods. Analysing the metrics, we can observe longer periods with an absence of cold waves (12 years, 2017 - 2028 and 8 years, 2035 - 2042) in comparison to the beginning of the time series. There is also a reduction in the number of cold waves and in the total sum of days under cold waves along the years. The duration of cold waves is higher in the first years of the series (2010 and 2011) and then it becomes stable. In summary, our results show that in the future there might be a reduction in the frequency and the number of cold waves.
Changes in lipid concentrations in the cold are often associated with the difference in energy intake from food in different seasons. However, this is a reductionist simplification, since the influence of dietary cholesterol on cholesterolemia is complex (24). Human beings produce cholesterol endogenously and about 25% of serum cholesterol comes from diet and the rest from cell biosynthesis (26–28).
Several mechanisms are involved in the differences in lipid concentration. Exposure to cold causes physiological changes, such as adaptive thermogenesis. This mechanism promotes energy dissipation in the form of heat by external stimuli, being involved in the energy balance and in the regulation of body temperature. In short, the energy generated in the mitochondria during the Krebs cycle gains an “alternative path”, preventing the generation of ATP (adenosine triphosphate) and allowing this energy to be dissipated in heat (29,30). This regulatory mechanism is extremely efficient, but it triggers high metabolic rates that can adversely modify lipid and lipoprotein concentrations, such as LDL-C (29).
The impact of cold waves on LDL-C can influence the increase in cardiovascular risk in colder months (12) and can also influence the treatment of patients who have been diagnosed with dyslipidemia close to periods that have cold waves, the patient can be classified as Normal or Pathological if his lipid profile is evaluated during a cold wave. This can cause additional costs to the Health System unnecessarily.
Initially we only intended to assess the influence of cold waves on LDL-C concentrations but afterwards we decided to work with predictive climate models in order to estimate the impact of our findings in the next years. One of our difficulties was related to producing these models, to predict daily data is computationally expensive, and we had to add noise to the model, so we could predict the next cold waves.
We also intended to analyze the impact of each cold wave, to then relate it with the predictive models, but our data was insufficient to perform such analysis.
We had the intention to conduct a similar analysis to assess the influence of high thermal amplitude on LDL-C concentrations. Days with thermal amplitude above the 90th percentile, based on the historical series, were considered high thermal amplitude days. The results indicated a lower percentage of LARV for days with high thermal amplitude, which was not the expected as it differed from the literature. We concluded that in order to perform a good analysis, we needed to consider more factors and for this reason we chose to focus the analysis only on the cold waves.
Cold waves have an adverse influence on LDL-C concentrations in vulnerable groups, such as adult women, elderly men and elderly women. These findings can be used to alert health experts when making treatment decisions and diagnosing patients. Predicted cold waves found in our analyses may impact LDL-C concentrations in the future and, at the same time, cardiovascular risk. Being able to estimate the next occurrences of cold waves can help in the development of early warning systems.
Based on our findings, some future research that could be done is to improve the climate model based on historical data by modeling the noise of the time series; to use a predictive model to estimate the impact of cold waves in the LDL-C concentrations; and to reproduce this analysis for other lipid parameters.
This project was funded by grant #2017/20013-0, São Paulo Research Foundation (FAPESP)
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