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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

C.  Impact  of  climatic  variation  on  the  relationships  between  variations  of  GPP,  ET  and WUE The  monthly  patterns  of  total  GPP  and  ET  had  similar  relationships  with  net  radiation, relative  humidity  (%  RH),  soil  water  content  (SWC),  vapor  pressure  deficit  (VPD),  air  temperature  and  precipitation  (Fig.4).  GPP  and  ET  had  strongly  significant  relationships  with  net  radiation  (P<0.01)  and  dominated  both  by  about  70%  (Fig.4a)  and  the  rest  had  positive  relationships  with%  RH,  SWC,  air  temperature and  precipitation  (Fig.4b,  4d,  4f)  respectively.  However  the  reduction  in  GPP  and  ET  was  obvious  when  higher  temperature  occurs  (Fig.4e).  Furthermore,  under  high  VPD  condition,  the  GPP  and  ET  declined  (Fig.4c),  because  the  maximum  photosynthesis  in  dry dipterocarp  forest  flux  site  at  the  Ratchaburi site  Thailand  (DFR  site)  occurred  under  with  VPD.  The  exponential  relationship  between  GPP,  ET  and  VPD  in  such  periods  coincided  with  less  rainfall  and  SWC  (<10%VWC)  (Fig.1)  and  are  in  phase  with  the  results  reported  by  Tong,  et  al.  (2014).Moreover  in  the  dry  season,  WUE  in  dry  dipterocarp  forest  decreased  significantly  with  an  increase  of  VPD  (P<0.01)  while  in  wet  season  this  was  not  important  (Fig.5).  Typically, the  VPD  involved  photosynthesis  and  respiration  processes;  if  VPD  was  very  high  (lower  air  humidity)  that  means  we  have  extensive  dry  conditions  and  thus  a  response  by  the  plant  stomata,  which  were  closed  and  less  transpiration  and  soil  evaporation  occurs. With  lower  stomatal  conductance  the  net  photosynthesis  rate  drops  steeply  but  the  on-going  needs  of  evapotranspiration  ensures  that  water  loss  continues.  This  leads  to  a  reduction  in WUE  (Fig.5a).  During  the  study  period  (2013  to  2015)  the  seasonal  average  WUE  in  DDF  was  negatively  related  to  lower  soil water  content  in  the  dry  season.  This  returned  to  a  positive  relationship  in  the  wet  season  (Fig.5b). D.  Conclusions The  major  aim  of  the  study  was  to  apply  eddy  covariance  technique  to  estimate  the  ecosystem WUE  in  dry  dipterocarp  forest  in  northern  Thailand.  It  was  found  that  WUE  at  above  canopy  ranged  from  1.39  to  3.39  g  C kg-1  H2O.  The  technique  here  can  be  useful.  The  monthly  and  seasonal  variability  of  GPP  and  ET  had  similar  relationships  to  net  radiation  (70%).  VPD  was  driver  of WUE  in  dry  season,  while  soil  water  content  was  the  main  factor  to  control WUE  throughout  the  year.  It  is  hoped  that  these  findings  will  contribute  to  improving  forest  management  practices. Proceedings  of  the  International  Conference  on  Climate  Change,  Biodiversity  and  Ecosystem  Services  for  the 271 Sustainable  Development  Goals  (SDGs):  Policy  and  Practice  27-29  June  2016,  Cha-am,  Phetchaburi,  Thailand


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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