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January 20, 2016 Newswires
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Association Between Low Temperature During Winter Season and Hospitalizations for Ischemic Heart Diseases in New York State

Journal of Environmental Health

Abstract

Most prior research investigating the health effects of extreme cold has been limited to temperature alone. Only a few studies have assessed population vulnerability and compared various weather indicators. The study described in this article intended to evaluate the effects of cold weather on hospital admissions due to ischemic heart disease, especially acute myocardial infarction (AMI), and to examine the potential interactive effects between weather factors and demographics on AMI. The authors found that extremely low universal apparent temperature in winter was associated with increased risk of AMI, especially during lag4-lag6. Certain demographic groups such as the elderly, males, people with Medicaid insurance, people living in warmer areas, and areas with high PM2.5 concentration showed higher vulnerabilities to cold-AMI effects than other groups.

Introduction

With climate change, extreme weather events such as heat waves and cold spells will become more frequent and longer in duration (Intergovernmental Panel on Climate Change [IPCC], 2007). The relationship among low ambient temperature and extreme cold events and ischemic heart disease (1HD) is not well understood. Most prior studies of the cold weather-IHD relationship have focused on mortality, finding statistically significant increased risks of 1.16-1.44 (Bhaskaran et al., 2009). In the cold weather season, December and January had the highest frequency of death (Kloner, Poole, & Perritt, 1999; Sheth, Nair, Muller, & Yusuf, 1999).

Even fewer studies have evaluated the association between cold temperature and 1HD hospital admissions as an indicator of morbidity. A comprehensive review by Bhaskaran and co-authors (2009) reported a statistically significant short-term increased risk of myocardial infarction (MI) at lower temperatures in winter in 8 of 12 studies; relative risks (RR) ranged from 1.01 to 1.40 and the strongest association was observed at lags of 2-7 and 8-14 days (Bhaskaran et al., 2009, 2010). Other research observed a seasonal variation for acute myocardial infarction (AMI) hospitalization that peaked in winter (Lee et al, 2010; Marchant, Ranjadayalan, Stevenson, Wilkinson, & Timmis, 1993; Spielberg, Falkenhahn, Willich, Wegscheider, & Voller, 1996). Old age and previous heart conditions increased vulnerability to cold effects (Analitis et al., 2008; Barnett et al, 2005; Bhaskaran et al, 2010; Danet et al., 1999; Morabito et al., 2005; Wichmann, Ketzel, Ellermann, & Loft, 2012). Other studies, however, observed no clear cold temperature1HD morbidity association (Hajat & Haines, 2002; Schwartz, Samet, & Patz, 2004).

Gaps identified in scientific literature include lack of sensitive weather indicators of low temperature on health, lack of consideration of other weather factors in addition to temperature, relative paucity of data on cardiovascular morbidities, no assessment of population vulnerability, and no assessment of interaction between low temperature and air pollution. Our study fills these knowledge gaps by evaluating the effects of various cold indicators and temperature ranges in the winter on IHD hospitalizations, cold temperatures individual and cumulative lag effect, and identifying potential vulnerable population groups to help inform climate adaptation planning.

Materials and Methods

Study Population and Study Design

The study population consisted of subjects hospitalized for IHD, which included AMI (International Classification of Disease 9th Revision [ICD9] codes, ICD9 410), angina pectoris (AP) (ICD9 413), chronic IHD (CIHD) (ICD9 414), and other IHD (OIHD) (ICD9 411, 412) from 1991 to 2004 in New York State (NYS) during the cold weather season. A time-stratified case-crossover design was employed to assess the weather-health relationships (Madure & Mittleman, 2000). Time was divided into two disjointed strata and exposure indicators in the hazard period and exposure indicators in multiple reference periods were compared within strata of time (Janes, Sheppard, & Lumley, 2005). Cases serve as their own controls and exposure indicators were assigned on 1-6 days before hospital admission (during hazard period). Cases were compared to exposure indicators at the same lags between the hazard and control period. Time-stratified selection of referents provided three referents per case per month on average.

Sources of Data

Hospital admission data were obtained from the NYS Department of Health (NYSDOH) Statewide Planning and Research Cooperative System (SPARCS), which collects inpatient information for all NYS hospitals except psychiatric and federal hospitals. The SPARCS database includes >95% of acute care hospitalizations (Lin et al., 2008). Meteorological data, including hourly observations for temperature (T), dew point (DP), barometric pressure (P), and wind speed (W) were provided by the Data Support Section of the Computational and Information System Laboratory and the National Center for Atmospheric Research of the National Weather Service. These data were used to derive daily maximum, mean, and minimum for each variable.

Exposure Definition

The cold weather season was defined as December 24 to February 18 of each year as the mean daily average universal apparent temperature (UAT) during this period was relatively stationary. Steadmans UAT was calculated using the formula:

UAT = -2.7 + 1.04*T + 2.0*VP - 0.65*W,

where T is measured in °C, VP in kPa, and W in m*s'1. VP was derived from DP:

VP = 0.6105 * EXPU7.27 * DP[°C] / (237.7 + DP[°C]).

Maximum, average, and minimum UAT values were calculated (Steadman, 1984). UAT is used in our study as it combines temperature, humidity, and wind, which more accurately represents the overall winter atmosphere and environment than temperature alone (Madrigano et al., 2013).

Fourteen weather regions were assigned in NYS. These regions were created by overlaying and merging the National Climate Data Center's 10 NYS climate divisions with 11 ozone regions developed for NYS (Chinery & Walker, 2009; Guttman & Quayle, 1996). Small regions that did not coincide completely were merged with the adjacent regions they were most similar to. This resulted in 14 regions of relatively homogeneous weather exposure. Although ozone exposure is not of interest in the winter season, we used temperature-ozone regions to be able to compare this study with our other studies of other diagnoses and in different seasons. Each hospitalization was geocoded by address and assigned to one region using MapMarker Plus.

We created three temperature indicators: mean of the daily average UAT (UATavg), three-day moving average of UATavg, and extreme temperature (10th percentile of UATavg distribution). We also assessed the effects of daily minimum UAT (UATmin) and daily maximum UAT (UATmax) on IHD hospitalizations. Since temperature did not have a linear relationship with IHD hospitalizations, 5°F interval groups were created for the mean of UATavg and the three-day moving UATavg, UATmin, and UATmax. For the stratified analysis we grouped temperature in 10°F intervals to avoid small sample size problems. In both analyses the temperature group closest to and above water's freezing point (32°F) was selected as the reference.

Confounders and Effect Modifiers

Potential sociodemographic confounders were controlled for by the study design. Casecrossover design is one kind of time-series analysis and a special type of matched casecontrol design where cases serve as their own controls. This design controls for confounding due to time-invariant variables, by having constant subject characteristics such as sex, race-ethnicity, age, and source of treatment in both exposure and control periods, which also controls for seasonality as both periods occur within the same month (Madure, 1991). Barometric pressure was also included as a confounding factor in the analysis. Stratified analysis was conducted for the following variables: sex, race-ethnicity, age, source of treatment payment, weather region, and particulate matter <2.5 pm (PM,5). Five categories were created for race-ethnicity: whiteHispanics, white non-Hispanics, black-Hispanics, black non-Hispanics, and other. Age was categorized as follows: 18-24, 25-44, 45-64, 65-74, and >75. Three sources of payment were considered: Medicare, Medicaid, and other programs. PM25 was categorized in two groups based on the U.S. Environmental Protection Agency (U.S. EPA) annual National Ambient Air Quality Standard: <15 pg/m3 and >15pg/m3. In December 2012, after our study period, U.S. EPA strengthened the annual fine particle standard from 15.0 pg/m3 to 12.0 pg/m3.

Statistical Analysis

Conditional logistic regression models using the SAS PHREG procedure were employed to analyze the data. Initially, crude analyses were stratified by sex, race-ethnicity, age, source of payment, weather region, and PM,_. Separate multivariate analyses were conducted for each exposure variable (mean of daily average and UATmax, mean of three-day moving average of UATavg, and extreme temperature). These models included potential effect modifiers along with product terms between main exposure variables and potential effect modifiers. Reduced models were built through a backward elimination process and limited to variables with complete information (Agresti, 2007). Effect modification on the multiplicative scale was assessed as deviation from perfect multiplicatively as determined by the likelihood ratio test with an alpha of .05 and results supported in stratified analysis. Odds ratio (OR) estimates were adjusted for atmospheric pressure by including it in the conditional logistic regression model.

Statewide analyses of AMI hospitalizations were conducted for UATavg, UATmax, and UATmin separately on the day of hospitaliza- tion (lagO) and each of the previous six days (lagl-lag6). Similarly, statewide analyses for AP, CIHD, and OIHD were also related to UATavg on the day of hospitalization (lagO) and each of the previous six days (lagl-lagó). The effect of extreme temperatures on hospitalizations of all categories of IHD was also analyzed. Data management and analysis were conducted using SAS version 9.2.

Results

Our analysis included 232,905 IHD hospitalizations (AMI: 83,650 [35.92%], AP: 10,794 [4.63%], CIHD: 100,496 [43.15%], and OIHD: 37,965 [16.3%]). The statewide mean of the UATavg in the NYS cold weather season, 1991-2004, was 18.0°F with a range of -30°F to 60°F, and varied among weather regions with the highest mean in New York City (24.4°F) and the lowest in the Adirondack region (7.5°F) (data not shown). The Adirondack, Mohawk Valley, Rochester, Binghamton, and Buffalo regions had the lowest UATavg in NYS. Consistent with low temperature trends, the rates of IHD admissions were highest in the Mohawk Valley (18.0/1,000 population), followed by the Buffalo region (15.7/1,000) (data not shown). A large heterogeneity in race-ethnicity distribution occurred with the highest percentage of whites in the northern, central, and western weather regions of the state and a higher percentage of Hispanics in New York City. The mean age in the study population was 66.4 years (data not shown).

Table 1 shows the results of the conditional regression analysis that examines the association between low UATavg and hospital admissions due to AMI by lag (Iag0-lag6) in NYS. Compared to the reference temperature group (35°F-40°F), temperatures below 35°F were associated with increased admissions due to AMI in Iag4-lag6. The most elevated association was observed for the -20°F to -15°F temperature group, with statistically significant ORs ranging from 1.25 (95% confidence interval [Ci] 1.00,1.57) to 1.29 (95% Cl 1.03, 1.61) at lag4 and lag5, respectively. For temperatures ranging between -5°F and 35°F, the statistically significant ORs for hospital admissions due to AMI varied between OR = 1.05 (95% CI 1.01, 1.10) for 5°F-10°F and 10°F-15°F temperature groups at lag4, 0°F-5°F and 5°F-10°F temperature groups at lag5, and OR = 1.14 (95% CI 1.06, 1.21) for -5°F to 0°F temperature group at lag4. The most consistent detrimental effect occurred at lag4. The association was not statistically significant for Iag0-lag3.

Table 2 shows results of analysis using the three-day moving average of UATavg. For temperatures below the reference (35°F-40°F), no significant effects were observed for the major- ity of the temperature groups of the moving averages except for the -15°F to -10°F temperature group with OR = 1.36 (95% Cl 1.08, 1.71) at Iag4-lag6 and for the 0°F-5°F temperature group with OR = 1.06 (95% Cl 1.00, 1.12) at Iag2-lag4. Although not statistically significant, ORs at Iag2-lag4 showed detrimental effect with values ranging from 1.01 (95% Cl 0.96, 1.06) to 1.17 (95% Cl 0.91,1.50).

Table 3 displays the results of the stratified analyses of the association between UATavg and AMI by demographics, weather region, and PM,5 concentration. Since the UATavgAMI hospitalization association was statistically significant and most consistent at lag4, we conducted the stratified analysis at lag4 only. In general, statistically significant results were consistently observed for temperature group 0°F-10°F Temperatures below 30°F increased the odds of hospitalizations among males: OR = 1.07 (95% Cl 1.02,1.11) for 0°F10°F and OR = 1.03 (95% Cl 1.00, 1.07) for 10°F-20°F temperature group; people of races other than whites or blacks: OR = 1.17 (95% Cl 1.05, 1.29) for 0°F-10°F and OR = 1.09 (95% Cl 1.00, 1.20) for 10°F-20°F; among subjects aged 25-64: OR range 1.05-1.14 for 0°F-10°F; and among subjects aged 65-74: OR = 1.06 (95% Cl 1.01, 1.12) for 20°F-30°F temperature group. Stratification by source of payment categories showed increased ORs for hospitalizations among Medicaid patients (OR range 1.13-1.61). With respect to weather region, the most elevated association was observed in Binghamton in the -20°F to -10°F interval, OR = 2.99, (95% CI 1.27, 7.03). Elevated ORs were also consistently observed for temperature group 0°F-10°F in NYC-LGA, Staten Island, Long Island, and Hudson Valley South. In the Buffalo region the odds of hospital admissions were consistently and significantly less than one for 0°F-30°F temperatures. PM,5 concentration above the U.S. EPA annual standard concentration increased the risk of hospitalization of AMI for temperature group 0°F-10°E

We further examined the association between extremely low UAT (<10th percentile) and various IHD categories in Iag0-lag6; Figure 1 describes the statistically significant estimates for different types of IHD at lag4lag6. We observed a statistically significant harmful effect on hospital admissions of AMI at Iag4-lag6 and for CIHD at lag6. Conversely, extreme low temperature displayed a protective effect on hospitalization due to AP and OIHD at lagO and lagl, and for CIHD at lagl, lag2, and lag4. We also further examined the associations between UATavg and various IHD subtypes including AP, CIHD, and OIHD. We did not find any significant relationships between low temperature and IHD other than AMI such as AP, CIHD, and OIHD (data not shown).

We analyzed the effect of UATmax on AMI hospital admissions by different lag periods as described in Table 4. Consistently increased ORs were observed in Iag5-lag6. The strongest association was observed at lag6 in the -15°F to -10°F interval (OR = 1.42 [95% Cl 1.03, 1.971). For temperature groups between 0°F and 35°F at lag5 and lag6, the ORs of AMI hospitalization varied between OR = 1.04 (95% Cl 1.00, 1.07) and OR = 1.07 (95% Cl 1.03, 1.11). With respect to UATmin, no increased risk of hospitalization was observed for UATmin <35°F (data not shown).

Discussion

The present study found that low ambient temperature in winter was associated with increased odds of hospital admissions due to AMI. We found that the association was statistically significant at UAT <35°E The effect is consistent when using multiple exposure indicators (UATavg, extreme UATavg, UATmax). The increases in risk of AMI hospital admission for all indicators range from 4% to 29%, which is within the range of findings from previous studies (Bhaskaran et al, 2010; Danet et al, 1999; Hopstock et al., 2012). Bhaskaran and co-authors (2010) examined the short-term relationship between ambient temperature and MI risk in 15 conurbations in England and Wales and found that each 1°C reduction in daily mean temperature was associated with a 2% (95% Cl 1.1%, 2.9%) cumulative increase in risk of MI. Another study assessing the effects of atmospheric temperature and pressure on occurrence of Ml and coronary deaths conducted by Danet and co-authors (1999) found that for a 10°C temperature decrease, the increase in disease rates was 13% for all age groups (p < .0001). Similar findings on the effect of daily weather conditions on Ml incidence in cold weather areas were reported by Hopstock and coauthors (2012), who found that the Ml risk increased by 47% when comparing the lower and upper limits of the temperature distribution (-10°C versus 20°C). The actual impact of cold temperature on AMI could be larger as difficulties in getting to the hospital during temperature extremes might lead to more out-of-hospital MI deaths, which would not have been included in our study.

Several explanatory mechanisms have been suggested for the higher occurrence of IHD in winter. Cold causes constriction of skin vessels, which increases blood pressure and consequently increases oxygen demand (Kloner, 2006). Cold may induce an increase in coronary artery resistance that can, in turn, result in coronary artery vasospasm (Kloner, 2006). Additionally, cold causes an increase in red and white blood cell and platelet concentrations, an increase in plasmatic fibrinogen and blood viscosity, and a shift of protein C to the extracellular space (Kloner, 2006; Nayha, 2005). Protein C along with changes in blood pressure and thrombosis may be responsible for acute heart conditions after exposure to cold temperature (Nayha, 2002).

We found that the effect of UATavg on AMI hospitalizations showed a delayed pattern, with an effect occurring four days after cold temperature. Our results are consistent with the findings of Wolf and co-authors (2009), who observed the strongest association between daily average temperature and nonfatal MI for a lag of three days, as well as Donaldson and Keatinge (1997), who found that the increase in IHD-related deaths was maximal at three days after the peak of cold. Compared to morbidity, other studies found an even longer delay between exposure and cardiovascular mortality, ranging from a lag of 2 weeks to 20 days (Analitis et ah, 2008; Carder et ah, 2005). The lagged effect may be due to inclement weather accompanying extreme cold, effectively reducing access to a hospital or inclination to be admitted (Schwartz et ah, 2004). The peak observed in odds of hospitalization several days after extreme low temperatures might be related to persons postponing admissions. Compared to respiratory diseases, cold-related IHD hospitalizations showed a longer latency, i.e., 4-6 days after low ambient temperature. Longer latency may be a secondary consequence of respiratory infections, which may be triggers for IHD by affecting blood coagulation and potentially damaging the vessel walls and promoting atherosclerosis (Nayha, 2002).

When comparing four cold temperature indicators, we found that UATmax has the highest and most significant effect on AMI (OR: 1.42) at lag6, and followed by threeday moving UATavg (highest OR: 1.36). The effects of UATavg (highest OR: 1.29) and extreme cold (<10th percentile, OR: 1.04) on AMI and different IHD are slightly lower. In a review of 12 studies investigating low ambient temperature on MI, most prior studies used mean temperature as the indicator, a few used maximum temperature, and only one or two considered winter wind chill and dew point (Bhaskaran et ah, 2010). The effects of cold temperature on MI seemed to be larger in the studies using maximum temperature than those using mean temperature, which is consistent with our findings. Few or no studies using moving average or extreme indicators are available to compare our results. The different findings among various studies could be due to differences in adaptation to extreme low temperature of people living in different climates, humidity, and wind patterns. Since almost all previous studies examining cold and IHD focused on AMI, no previous literature is available to compare with our findings for other IHD admissions. While low UATmax with 4-5 single day lag had shown strongest AMI effect, we cannot neglect the cumulative effect of low UAT from lag4 to lag6 days on AMI although little to no previous literature is available to compare with our findings. Our study also diverges from other studies in its use of UAT, which includes dew point and wind chill in addition to temperature to represent the real atmosphere in winter.

Our analyses showed subjects age 65 and older had higher odds of AMI hospitalization, which is consistent with previous findings by Bhaskaran and co-authors (2010), Hopstock and co-authors (2012), and Morabito and co-authors (2005), showing the highest risks and a same day effect in the elderly population compared to delayed lag in other age groups. The increased risk in older age can be explained by the deterioration of effective body thermoregulation. Our findings of slight but persistent increased AMI risks of cold temperature among males compared to females is supported by the studies of Wichmann and co-authors in Denmark (2012), Kysely and co-authors in Czech Republic (2009), and Loughnan and co-authors in Australia (2008). This gender difference may be explained by occupational exposure in winter by men as men are more likely than women to work outdoors. Other studies reported contradictory findings, however, with increased risks among women (Barnett et al., 2005; Panagiotakos et al., 2004). Our study also found that people using Medicaid were more susceptible to the cold effect on IHD, which is supported by prior studies identifying low socioeconomic status as a risk factor of vulnerability to cold (Wichmann et al., 2012; Wolf et al., 2009). We also found that warmer/southern areas of NYS (i.e., Binghamton, Western Plateau) showed higher AMI risks to cold weather than other areas, which is consistent with prior studies showing increased vulnerability to cold days in locations with higher mean temperatures (Bhaskaran et ah, 2009). No prior research has assessed the modifying effect of air pollution on cold-AMI to compare with our findings of an interaction between PM,_ and cold weather 2.3 on AMI.

Study Strengths

This is one of the few studies examining the association between cold weather conditions and IHD morbidity, especially AMI, over a long period in NYS, a state with multiple subclimate regions. The unique contributions of this project include comparing the IHD effects using different cold weather indicators, in different temperature ranges during winter, by different lag periods, short-term vs. cumulative effects, and assessing different subgroups of IHD. Using UAT allowed us to consider multiple weather factors including temperature, dew point, and wind simultaneously. Since both health outcome and exposure data (weather and air pollution data) are objective, routinely collected datasets, recall bias is unlikely. By examining potential interactions between low temperature and pollution/sociodemographics, we were able to identify vulnerable populations, which is useful for future adaptation planning.

Study Limitations

This study used hospital admission data as health endpoints and thus may have captured only the most severe IHD cases. To minimize case under-ascertainment, we focused on AMI, a condition that requires immediate medical attention and treatment through hospital admission. Another limitation is that meteorological data were obtained from fixed monitoring sites, which assumes uniformity across regions. Although some factors such as daily activity patterns, family history of IHD, seasonal weight gain, and sociodemographic factors are important confounders, the case-crossover design automatically controls for these factors by using cases as their own controls. In addition, some factors such as quality of housing, heating use, insulation, and influenza are potential confounders that are unavailable in our current study and will be examined through surveys in the future.

Conclusion

The present study found that extreme low UAT in winter was associated with increased risk of AMI, especially during Iag4-lag6, but not associated with other IHD subgroup diseases. We also found that low UATmax in winter was a more sensitive indicator to AMI than mean and UATmin. This study also found that certain demographic groups such as the elderly, males, people with Medicaid insurance, and people living in warmer areas and areas with high PM25 concentration showed higher vulnerabilities to cold-AMI effects than other groups. Further studies should validate our findings by adjusting heating and ventilation confounders. Interventions based on these findings, such as targeting vulnerable areas/populations and monitoring sensitive cold indicators and AMI should be considered in climate change adaptation efforts. Hil

Acknowledgements/Disclaimers: This work was supported by a grant from the Centers for Disease Control and Prevention Award #5U01EH000396. The authors declare they have no actual or potential competing financial interests. We would like to thank Nazia Saiyed and Donghong Gao for their help with editing and proofreading.

Prepublished online September 2015, National Environmental Health Association.

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Shao Un, MD, PhD

New York State Department of Health

Department of Environmental

Health Science

University at Albany School

of Public Health

Aida Soim, MD, PhD

New York State Department of Health

Department of Epidemiology

and Biostatistics

University at Albany School

of Public Health

Kevin A. Gleason

New York State Department of Health

Syni-An Hwang, PhD

New York State Department of Health

Department of Epidemiology

and Biostatistics

University at Albany School

of Public Health

Corresponding Author: Shao Lin, New York State Department of Health, Bureau of Environmental and Occupational Epidemiology, Empire State Plaza, Corning Tower, Room 1203, Albany, NY 12237.

E-mail: [email protected]

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