Climate impact on seasonal patterns of diarrhea diseases in Tropical area

Similar documents
Available online Journal of Scientific and Engineering Research, 2018, 5(3): Research Article

Drought in Southeast Colorado

Seasonal Climate Outlook for South Asia (June to September) Issued in May 2014

Analysis of Historical Pattern of Rainfall in the Western Region of Bangladesh

Marche Region Climate Analysis by Danilo Tognetti 1

UPDATE OF REGIONAL WEATHER AND SMOKE HAZE (December 2017)

Average temperature ( F) World Climate Zones. very cold all year with permanent ice and snow. very cold winters, cold summers, and little rain or snow

11/30/2015 Source of Support: None, No Conflict of Interest: Declared

Drought Characterization. Examination of Extreme Precipitation Events

Colorado s 2003 Moisture Outlook

The Climate of Bryan County

Analysis of Rainfall and Other Weather Parameters under Climatic Variability of Parbhani ( )

PROPOSAL OF SEVEN-DAY DESIGN WEATHER DATA FOR HVAC PEAK LOAD CALCULATION

Physical Features of Monsoon Asia. 192 Unit 7 Teachers Curriculum Institute 60 N 130 E 140 E 150 E 60 E 50 N 160 E 40 N 30 N 150 E.

Atmospheric circulation analysis for seasonal forecasting

Will a warmer world change Queensland s rainfall?

UPPLEMENT A COMPARISON OF THE EARLY TWENTY-FIRST CENTURY DROUGHT IN THE UNITED STATES TO THE 1930S AND 1950S DROUGHT EPISODES

2003 Moisture Outlook

South Asian Climate Outlook Forum (SASCOF-6)

SEASONAL CLIMATE OUTLOOK VALID FOR JULY-AUGUST- SEPTEMBER 2013 IN WEST AFRICA, CHAD AND CAMEROON

Chapter 1 Climate in 2016

Interannual variation of MODIS NDVI in Lake Taihu and its relation to climate in submerged macrophyte region

CHAPTER-11 CLIMATE AND RAINFALL

WHEN IS IT EVER GOING TO RAIN? Table of Average Annual Rainfall and Rainfall For Selected Arizona Cities

Thai Meteorological Department, Ministry of Digital Economy and Society

The Climate of Marshall County

DROUGHT IN MAINLAND PORTUGAL

Chiang Rai Province CC Threat overview AAS1109 Mekong ARCC

The Climate of Grady County

The Climate of Pontotoc County

Cuba. General Climate. Recent Climate Trends. UNDP Climate Change Country Profiles. Temperature. C. McSweeney 1, M. New 1,2 and G.

UPDATE OF REGIONAL WEATHER AND SMOKE HAZE (February 2018)

El Niño 2015/2016 Impact Analysis

Verification of the Seasonal Forecast for the 2005/06 Winter

Assessment of the Impact of El Niño-Southern Oscillation (ENSO) Events on Rainfall Amount in South-Western Nigeria

South & South East Asian Region:

The Climate of Payne County

Changing Hydrology under a Changing Climate for a Coastal Plain Watershed

The Climate of Kiowa County

El Nino 2015 in South Sudan: Impacts and Perspectives. Raul Cumba

El Niño-Southern Oscillation (ENSO) Rainfall Probability Training

ARUBA CLIMATOLOGICAL SUMMARY 2017 PRECIPITATION

1. Introduction. 2. Verification of the 2010 forecasts. Research Brief 2011/ February 2011

The Climate of Seminole County

The Climate of Murray County

IMPACT OF CLIMATE CHANGE ON RAINFALL INTENSITY IN BANGLADESH

YACT (Yet Another Climate Tool)? The SPI Explorer

Country Presentation-Nepal

KUALA LUMPUR MONSOON ACTIVITY CENT

A Report on a Statistical Model to Forecast Seasonal Inflows to Cowichan Lake

The Climate of Texas County

Statistical Analysis of Temperature and Rainfall Trend in Raipur District of Chhattisgarh

Seasonal Climate Watch September 2018 to January 2019

St Lucia. General Climate. Recent Climate Trends. UNDP Climate Change Country Profiles. Temperature. Precipitation

Agricultural Science Climatology Semester 2, Anne Green / Richard Thompson

Fire Weather Drivers, Seasonal Outlook and Climate Change. Steven McGibbony, Severe Weather Manager Victoria Region Friday 9 October 2015

Seasonal Climate Watch February to June 2018

Sierra Weather and Climate Update

Constructing a typical meteorological year -TMY for Voinesti fruit trees region and the effects of global warming on the orchard ecosystem

Drought Monitoring in Mainland Portugal

"STUDY ON THE VARIABILITY OF SOUTHWEST MONSOON RAINFALL AND TROPICAL CYCLONES FOR "

South Asian Climate Outlook Forum (SASCOF-12)

REPORT ON SOWING PERIOD AND FLOODING RISKS IN DOUALA, CAMEROON. Cameroon Meteorological Department

Grenada. General Climate. Recent Climate Trends. UNDP Climate Change Country Profiles. Temperature. Precipitation

Antigua and Barbuda. General Climate. Recent Climate Trends. UNDP Climate Change Country Profiles. Temperature

ANNUAL CLIMATE REPORT 2016 SRI LANKA

MISSION DEBRIEFING: Teacher Guide

Chapter-3 GEOGRAPHICAL LOCATION, CLIMATE AND SOIL CHARACTERISTICS OF THE STUDY SITE

The Climate of Haskell County

Volume 6, Number 2, December, 2014 ISSN Pages Jordan Journal of Earth and Environmental Sciences

Becky Bolinger Water Availability Task Force November 13, 2018

Long Range Forecasts of 2015 SW and NE Monsoons and its Verification D. S. Pai Climate Division, IMD, Pune

Champaign-Urbana 2001 Annual Weather Summary

PROJECT REPORT (ASL 720) CLOUD CLASSIFICATION

Malawi. General Climate. UNDP Climate Change Country Profiles. C. McSweeney 1, M. New 1,2 and G. Lizcano 1

What is happening to the Jamaican climate?

Chapter 3. Regression-Based Models for Developing Commercial Demand Characteristics Investigation

APPENDIX G-7 METEROLOGICAL DATA

Seasonal Climate Watch July to November 2018

SEASONAL AND SECULAR VARIATIONS OF SUNSHINE DURATION AND NATURAL SEASONS IN JAPAN

8.1 Attachment 1: Ambient Weather Conditions at Jervoise Bay, Cockburn Sound

Introduction of Seasonal Forecast Guidance. TCC Training Seminar on Seasonal Prediction Products November 2013

CLIMATE VARIABILITY AND DISEASE PATTERNS IN TWO SOUTH EASTERN CARIBBEAN COUNTRIES. Dharmaratne Amarakoon, Roxann Stennett and Anthony Chen

What Is Climate Change?

Champaign-Urbana 2000 Annual Weather Summary

Appearance of solar activity signals in Indian Ocean Dipole (IOD) phenomena and monsoon climate pattern over Indonesia

What Does It Take to Get Out of Drought?

OPTIMIZATION OF GLOBAL SOLAR RADIATION OF TILT ANGLE FOR SOLAR PANELS, LOCATION: OUARGLA, ALGERIA

Variability and trends in daily minimum and maximum temperatures and in diurnal temperature range in Lithuania, Latvia and Estonia

INFLUENCE OF THE AVERAGING PERIOD IN AIR TEMPERATURE MEASUREMENT

2003 Water Year Wrap-Up and Look Ahead

Champaign-Urbana 1998 Annual Weather Summary

COUNTRY REPORT. Jakarta. July, th National Directorate of Meteorology and Geophysics of Timor-Leste (DNMG)

The Failed Science of Global warming: Time to Re-consider Climate Change

THE CLIMATE OVER SRI LANKA YALA SEASON 2017

Research note UDC: 911.2:511.58(497.16) DOI:

East-west SST contrast over the tropical oceans and the post El Niño western North Pacific summer monsoon

JOURNAL OF INTERNATIONAL ACADEMIC RESEARCH FOR MULTIDISCIPLINARY Impact Factor 1.393, ISSN: , Volume 2, Issue 4, May 2014

Dust storm variability over EGYPT By Fathy M ELashmawy Egyptian Meteorological Authority

Mozambique. General Climate. UNDP Climate Change Country Profiles. C. McSweeney 1, M. New 1,2 and G. Lizcano 1

Transcription:

Climate impact on seasonal patterns of diarrhea diseases in Tropical area Akari Teshima 1, Michio Yamada 2, *Taiichi Hayashi 1, Yukiko Wagatsuma 3, Toru Terao 4 (1: DPRI, Kyoto Univ., Japan, 2: RIMS, Kyoto Univ., Japan, 3: ICDDR,B:Center for Health and Population, Bangladesh, 4: Faculty of Informatics, Osaka Gakuin Univ., Japan) *Taiichi Hayashi, DPRI, Kyoto University, Japan, 611-0011, Gokasho, Uji, Kyoto, Japan. E-mail: hayashi@rcde.dpri.kyoto-u.ac.jp Abstract Statistical investigation has been made for the effect of the climate on the epidemic diseases using the time series of meteorological elements and the number of patients. We apply correlation and EOF analysis method to time series of diarrhea patients and meteorological elements in Bangladesh. The anomaly of the number of the diarrhea patients has different signs for the periods before and after June, corresponding to the two peaks of the number of the patients. Higher maximum temperature and more sunshine in the pre-monsoon period are found to have a tendency to enhance the first peak of the diarrhea occurrence. Key words: climate, diarrhea disease, correlation, EOF analysis, Bangladesh 1. Introduction Associated with the global warming, the climate impact on tropical infectious diseases is getting more attention recently. For example, malaria, cholera and dengue fever in tropical area in Asia and Africa are considered to prevail broadly in the middle latitude countries. In South Asia, such as India and Bangladesh, prevalence of diarrhea diseases is a serious problem of public health. Diarrhea patients have been increasing for a few decades (Fig. 1) and this seasonal variation has two peaks in the pre-monsoon (March and April) and at the end of the monsoon (September and October) in Dhaka (Fig. 2). Wagatsuma et al. (2002) that reported the correlation analysis shows the patient occurrence is related to the meteorological elements a few months before the peak of infection. There s also a research reporting that the distinct increase of diarrhea takes place in the years of El Nino and Southern Oscillation (Pascual M. et al. 2002). These researches clarified somewhat the qualitative relation between the variations of meteorological elements and the number of patients. In this paper, we apply the correlation and the EOF analysis to the time series of diarrhea patients and meteorological elements in Bangladesh, to understand the effects of the meteorological variation on the prevalence of diarrhea disease. 2. Data The International Centre for Diarrhoea Disease, Bangladesh: Centre for Health and Population research (ICDDR, B) in capital city Dhaka supplied the daily number of diarrhea diseases patient for 22 years from 1980 to 2001. The patients were classified to V.Cholera or Rota for 21 year from 1981 to 2001. The surface observation data for 22 years (1980-2001) in Dhaka are provided by Bangladesh Meteorological Department (BMD). Among maximum temperature, precipitation, sunshine, relative humidity, dry bulb temperature, minimum temperature, wind and cloud pressure, we used the first four elements for analysis: temperature and relative humidity were 3 hourly and the other daily. Since a deficit is found from 1990 to 1992 in sunshine data, the period has been removed from analysis. Fig.1 Time series of monthly diarrhea patients number in ICDDR,B from 1980 to2001.

Fig. 2 Seasonal variation of diarrhea patients in ICDDR,B. The number of patients are averaged for 22years from 1980-2001. Fig.3 Seasonal relationship of diarrhea patients to mean temperature. (Teshima A. and Hayashi T. et al. 2004) 3. Method of Analysis We made correlation analysis and the EOF analysis for the time series of patient and meteorological elements. We take averages every two weeks in each year from 1981 to 2001. That is, yearly data are divided to 26 portions and each portion contains 22 data for 22 years. The patient data are normalized by the yearly total patient number to remove the year-to year increasing trend. Two types of correlation analysis below were carried out for meteorological elements and patient number. A certain portion of climate precedes that of diarrhea occurrence. a) lag correlation of meteorological elements to one fixed portion of patient. b) lag correlation of patient number to one fixed portion of meteorological elements. The ith portion in wth year is expressed as X(w,i) for patient data, and Y1(w,i)~Y4(w,i) for meteorological 4 elements. We have applied the EOF analysis to X(w,i)~Y4(w,i) by correlation matrix of the anomaly = and =, where are averages on i. 4. Result Fig. 4(a-1) shows the lag correlation of meteorological elements to the fixed portion of total diarrhea patients in April. The time lag for the meteorological elements is set from October to April. The maximum temperature and the sunshine duration have positive correlation and the precipitation and relative humidity have the negative correlation. Generally correlation is not clear in October-January, then increases from February and reaches the peaks with correlation coefficient more than 0.5 in March in maximum temperature and the sunshine duration. The inverse correlations for the precipitation and the relative humidity also have peaks about -0.5 around February and March. Fig. 4(a-2) shows the similar correlation as Fig. 4(a-1) except for diarrhea patients in August. The signs of correlations are reverse compared with Fig. 4(a-1) with positive correlation in the precipitation and the relative humidity and negative one in the maximum temperature and the sunshine duration. The correlation coefficients increase from March and don t have large peaks. Fig. 4(b-1) is the lag correlation of the diarrhea patients to the fixed portion of the meteorological elements in April. The correlation coefficients more than absolute value 0.5 in April decreases gradually and crosses at zero in the middle of June. Therefore that indicates the similar effect of the meteorological elements lasts two months. Fig. 4(b-2) shows the similar correlations as Fig. 4(b-1) except for meteorological elements in September. The correlation coefficients are significant up to October and cross zero in November. Fig. 5 shows the result of the EOF analysis for the patients of total diarrhea, diarrhoeal cholera and rota. In the dominating component, the anomaly of the number of patients has different signs for specific month. In the first principle component of total diarrhea and in the second one of diarrhoeal cholera, the signs change in June and July. In the first principle component of diarrhoeal cholera and the second one of diarrhoeal rota signs change in February and in the first principle

component of diarrhoeal rota in December. This indicates the different characteristics of each type of diarrhea. Diarrhoeal cholera shows similar tendency to total diarrhea diseases, but the rota shows different characteristics with total diarrhea and cholera. 5. Summary The diarrhea patient in the first peak in April is sensitively correlated to climate elements in pre-monsoon. Climate in pre-monsoon has influence on total diarrhea patient through the spring peak (April-May) and the effect of climate in the August lasts through Aug-Oct, the autumn peak of patient. Meteorological elements play reverse role on the peak of spring and autumn diarrhea patient. Total diarrhea diseases and diarrhoeal cholera show common anomaly pattern but rota seems different. The characteristics of the former two change mainly in Jun-Jul, but that of the latter one changes in Jan-Feb. Reference Pascual M., Colwell, R. et al. Cholera Dynamics and El Nino-Southern Oscillation. Science,289, 1763-1766,2002 Wagatsuma Y., Hayashi T. et al. Relationship between pattern of infectious diseases and seasonal variation of surface meteorological elements in Bangladesh. Preprints, J. Meteor. Soc., 82, 279,2002 Teshima A., Hayashi T. et al. Impact of meteorological elements on diarrhea diseases in Bangladesh. Preprints, J. Meteor. Soc., 86, 257,2004 Fig.4 Correlations between the meteorological elements and the fixed diarrhea patients in Spring (a-1), and in August (a-2). Correlations between the diarrhea patients and the fixed meteorology in April (b-1), and in August (b-2).

Fig.5 The EOF analysis result for the meteorological elements and diarrhrea patients(a),chorela(b) or rota(c).