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Proceedings of International Conference on Climate Change, Biodiversity and Ecosystem Services for the Sustainable Development Goals : Policy and Practice 27-29 June 2016 at the Sirindhorn International Environmental Park, Cha-am, Phetchaburi, Thailand

R95p Very wet days Annual total PRCP when RR>95th E.  Anomaly  and  Trend  Identification percentile To  evaluate  the  variation  of  climate  pattern,  anomalies  based  on  the  difference  between  mean  temperature  in  each  year  and  the  long-term  average  for  the  period  1975-2015  are  calculated.  The  observed  mean  annual  maximum  temperatures  (Tmaxmean)  or  annual  minimum  temperature  (Tminmean)  were  then  plotted  in  time  series.  The  statistical  significance  of  the  trends was  calculated  using  ordinary  least  square  method.  The  Thiel-Sen  nonparametric  method  is  used  to  estimate  the  slope  of  linear  trends  19.  This  method  is  frequently  applied  in  previous  climatological  studies  (e.g.  20,  21)  and  which  outperforms  the  least  squares  regression  in  computing  the  magnitude  of  linear  trends  when  the  sample  size  is  large  22.  The  95%  significant  levels  were  used  to  consider  a  trend  to  be  statistically  significant.  The  slope  estimates  of  N  pairs  of  data  are  first  computed  by;   Where,  xj  and  xk  are  data  values  at  times  j  and  k  (j>k),  respectively.  The  median  of  these  N  values  of  Qi  is  the  Sen’s  estimator  of  slope. III.  RESULTS  AND  DISCUSSION A.  Anomaly  and  Trend  Analysis 1)  Mean  Maximum  Temperature:  The  overall  trend  of  mean  maximum  temperature  anomalies  at  four  stations  in  Mandalay,  Meikthila,  Monywa,  and  Pyinmana  increased  throughout  the  latter  half  of  observed  periods  in  all  stations  except  Minbu.  The  anomalies  in  Minbu  were  varied,  moving  between  positive  and  negative  ones.  Most  of  the  station  reaches  the  highest  anomalies  about  +1.5°C  versus  the  normal  value.  The mean maximum  temperature  in  dry  zone  area  started  to  increase  since  1977.  The  continuous  positive  anomalies  started  from  1993  ranging  from  a  minimum  of  +0.01°C  (2001)  to  a  maximum  of  +1.12°C  (2010).  The  significant  positive  anomalies  can  be  observed  in  2009,  1998,  2005,  2014,  2012,  and  1979  (descending  order  of  anomalies  value)  (Fig.2)  and  almost  all  the  years  correspond  with  the  declining  phase  of  strong  El  Niño  events  23.  During  the  21st  century,  temperatures  have  continued  to  increase  from  2003  to  2015  except  in  2007  and  2011,  which  experienced  the  La  Niña  events  23. 296 Proceedings  of  the  International  Conference  on  Climate  Change,  Biodiversity  and  Ecosystem  Services  for  the Sustainable  Development  Goals  (SDGs):  Policy  and  Practice  27-29  June  2016,  Cha-am,  Phetchaburi,  Thailand mm R99p Extremely wet days Annual total PRCP when RR>99th percentile mm CDD Consecutive dry days Maximum number of consecutives days with RR<1mm Days CWD Consecutive wet days Maximum number of consecutives days with RR>=1mm Days For i= 1,…,NEq(2)  


Proceedings of International Conference on Climate Change, Biodiversity and Ecosystem Services for the Sustainable Development Goals : Policy and Practice 27-29 June 2016 at the Sirindhorn International Environmental Park, Cha-am, Phetchaburi, Thailand
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