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Trends in extreme events of rainfall
in low country wet zone of Sri Lanka




                          HERATH H.M.L.K.
                          SIHILELLA J.P.W.P.
                          ABEYSINGHE D.C.
                          DHANUSHIKA M.P.      1
2
• Climate is changing

• Climate change affects both growth and the
  production of plants




                                               3
• Rubber and tea are main
  revenue earners among
  plantation crops in Sri Lanka

• Most of rubber plantation and
  Low grown tea plantations;
  Mainly confined in low country
  wet zone region of the Island


                                   4
• Both rubber and tea plantations have direct
  relationships with the climate

• Require well spread-out rainfalls
  Tea    - 1000 to 1250mm
  Rubber - 1650 to 3000mm



                                                5
Changes in the                          600

amount and the                          500




                        Rainfall (mm)
                                        400
distribution of                         300

rainfall in Sri Lanka                   200
                                        100
are not very                              0




                                              May
                                              Mar




                                              Dec
                                               Jan




                                              Jun
                                              Apr




                                              Aug
                                              Feb




                                              Sep
                                              Oct
                                              Nov
                                                Jul
apparent




                                                      6
Variability in climatic parameters: Variability
due climate change may overwhelmed by the
random variability
                        5000
                        4500
        Rainfall (mm)




                        4000
                        3500
                        3000
                        2500
                        2000
                        1500
                                      1945




                                                                                              1985
                               1940


                                             1950
                                                    1955
                                                           1960
                                                                  1965
                                                                         1970
                                                                                1975
                                                                                       1980


                                                                                                     1990
                                                                                                            1995
                                                                                                                   2000
                                                                                                                          2005
                                                                                                                                 2010
                                                                           Year

                                                                                                                                        7
to identify trends in extreme events of rainfall
in low country wet zone of the Island




                                                   8
9
Daily rainfall data
from 8 Agro
meteorological
stations for the
period of 1941-2010
were used




                      10
Agro ecological region, elevation, latitude and longitudes of
Agro meteorological stations under investigation

 Agro- met     AER    Elevation (m) Latitude     Longitude
 station
 Awissawella   WL1        134       6057’11’’N   80013’6’’E
 Dartonfield   WL1        152       6031’0’’N    80010’0’’E
 Ratnapura     WL1        259       6058’N       80046’E
 Ambanpitiya   WL2        297       7014’0’’N    80020’0’’E
 Galle         WL3        105       7046’N       80017’E
 Hanwella      WL4         81       6054’23’’N   8005’23’’E
 Kalutara      WL4         15       6035’24’’N   79057’36’’E
 Matara        WL4         2        14041’3’’N   39024’52’’E

                                                                11
At each location,
• Annual, monthly and weekly rainfalls

• Number of rainy days
     A rainy day is defined as a day receiving ≥0.5mm rainfall


• Wet spells

• Dry spells

                                                                 12
• Extreme events were identified using the
  boundary line technique

• Regression techniques to identify trends




                                             13
Boundary Line Approach

                  Upper boundary




                  Lower boundary




                                   14
15
 Amount and the distribution of rainfall
 Linear trend and the respective R2 values of total
  annual rainfalls at each location
     Location               Trend       R2 value
     Ambanpitiya            -10.43       0.155
     Awissawella             -3.99       0.023
     Dartonfield            -4.334       0.011
     Galle                  -7.127       0.101
     Hanwella               -1.705       0.005
     Kalutara                -1.33       0.003
     Matara                 -5.825       0.073
     Ratnapura              -3.166       0.017
                                                      16
 Trends of all the locations were not
  significant

 But the signs of the trends were negative

 The temporal variations of daily rainfall
  variability were random in all the locations


                                                 17
Ambanpitiya
                4000             Linear (Ambanpitiya)
                3500
Rainfall (mm)




                3000
                2500
                2000
                1500
                1000
                 500
                   0
                       1941
                       1945
                       1949
                       1953
                       1957
                       1961
                       1965
                       1969
                       1973
                       1977
                       1981
                       1985
                       1989
                       1993
                       1997
                       2001
                          Year


 Temporal variation of annual rainfall in Ambanpitiya
                                                        18
Boundary line analysis on annual rainfall

 Trends and the R2   Location                Trend        R2
 values for the      Ambanpitiya             -65.8 *      0.35
 lower boundary      Awissawella              -29.2       0.07
                     Dartonfield              -18.7       0.03
                     Galle                   -26.6 *      0.24
                     Hanwella                 -12.0       0.05
                     Kalutara                   1.2       0.00
                     Matara                  -34.4*       0.17
                     Ratnapura                 10.3       0.06
                                * Significant at p<0.05
                                                                 19
3000
                                                                               Minimum               Linear trend
                2500
Rainfall (mm)


                2000

                1500

                1000

                500

                   0
                       1943
                              1948
                                     1953
                                            1958
                                                   1963
                                                          1968
                                                                 1973
                                                                        1978
                                                                               1983
                                                                                      1988
                                                                                             1993
                                                                                                    1998
                                                                                                           2003
                                                                                                                  2008
                                                                 year


Temporal variations of lower boundary of annual
rainfall in Ambanpitiya
                                                                                                                         20
 The temporal variation of maximum and
  minimum occurrences of annual rainfalls
  events in some locations were statistically
  significant

 This is an indication of having some years
  with comparatively low annual rainfalls


                                                21
 Temporal variations in wet and dry days

Linear trend and the     Location                 Trend          R2
respective R2 values     Ambanpitiya           -1.026***       0.54
of wet days at each      Awissawella           -0.611***       0.22
location                 Dartonfield             -0.211        0.05
                         Galle                  -0.327**       0.156
                         Hanwella               -0.458**       0.142
                         Kalutara               -0.524**       0.132
                         Matara                -0.827***       0.421
                         Ratnapura               -0.004        0.001
                       ** Significant at p<0.01, ***Significant at p<0.001

                                                                             22
250

                  200                                                                     Wet days                    Linear trend
No. of Wet days




                  150

                  100

                  50

                   0



                                                                                1973
                                                                                       1977
                        1941
                               1945
                                      1949
                                             1953
                                                    1957
                                                           1961
                                                                  1965
                                                                         1969



                                                                                              1981
                                                                                                     1985
                                                                                                            1989
                                                                                                                   1993
                                                                                                                          1997
                                                                                                                                 2001
                                                                                                                                        2005
                                                                                                                                               2009
                                                                                Year


Temporal variation of annual wet days together with
its linear trend in Ambanpitiya
                                                                                                                                                      23
 Trends in lower and upper boundary of
  annual wet days were statistically significant




                                                   24
250
                                                                         Upper boundary                      Linear trend
                  200
No. of wet days




                  150
                  100
                   50
                   0
                                      1953
                        1943
                               1948


                                             1958
                                                    1963
                                                           1968
                                                                  1973
                                                                          1978
                                                                                 1983
                                                                                        1988
                                                                                               1993
                                                                                                      1998
                                                                                                              2003
                                                                                                                     2008
                                                                  Year

Upper boundary line the trend fitted to annual wet
days in Ambanpitiya
                                                                                                                            25
160
                  140                                                       Lower boundary                   Linear trend
                  120
No. of wet days




                  100
                   80
                   60
                   40
                   20
                    0
                        1943
                               1948
                                      1953
                                             1958
                                                    1963
                                                           1968
                                                                  1973
                                                                         1978
                                                                                1983
                                                                                       1988
                                                                                              1993
                                                                                                     1998
                                                                                                            2003
                                                                                                                   2008
                                                                   Year

          lower boundary line the trend fitted to annual wet
          days in Ambanpitiya
                                                                                                                            26
 significant decline in number of wet days

 A risk of aggregating heavy showers




                                              27
 Temporal variation of maximum dry run

 Linear trend and the     Location             Trend          R2
 respective R2 values     Ambanpitiya          0.58**        0.35
 of annual maximum        Awissawella          0.36**        0.31
 dry run in each          Dartonfield           -0.41        0.12
 location                 Galle                 0.08         0.01
                          Hanwella             0.38**        0.26
                          Kalutara              0.25         0.07
                          Matara               0.73**        0.40
                          Ratnapura            0.14*         0.13
                        * Significant at p<0.05, **Significant at p<0.01

                                                                           28
70    Max. dry run
  Maximum dry run (days)

                           60    Linear trend
                           50
                           40
                           30
                           20
                           10
                            0
                                1961
                                1941
                                1945
                                1949
                                1953
                                1957

                                1965
                                1969
                                1973
                                1977
                                1981
                                1985
                                1989
                                1993
                                1997
                                2001
                                2005
                                2009
                                     Year

Temporal variation of maximum dry run with its
linear trend in Ambanpitiya
                                                 29
 Risk of having lengthy dry spells in some
  locations in the Low country wet zone




                                              30
 No significant change in annual rainfall
  (Cumulative rainfall)

 Significant tendency of having incidences of
  aggregated heavy showers in the low
  country wet zone

 Signs of lengthy dry spells
                                                 31
 Adverse impacts on some operations like
 crop establishment and fertilizer application




 Favorable for latex exploitation




                                                 32
• Director of the Rubber Research Institute of Sri Lanka
  (RRISL)

• Dr. (Mrs.) Wasana Wijesekara, Head of the Biometry
  Section of RRISL

• Mr. Vidura Abeywardena, technical officer of the
  Biometry Section of RRISL

• Department of Meteorology
                                                           33
34

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Trends in extreme events of rainfall in low country wet zone of Sri Lanka

  • 1. Trends in extreme events of rainfall in low country wet zone of Sri Lanka HERATH H.M.L.K. SIHILELLA J.P.W.P. ABEYSINGHE D.C. DHANUSHIKA M.P. 1
  • 2. 2
  • 3. • Climate is changing • Climate change affects both growth and the production of plants 3
  • 4. • Rubber and tea are main revenue earners among plantation crops in Sri Lanka • Most of rubber plantation and Low grown tea plantations; Mainly confined in low country wet zone region of the Island 4
  • 5. • Both rubber and tea plantations have direct relationships with the climate • Require well spread-out rainfalls Tea - 1000 to 1250mm Rubber - 1650 to 3000mm 5
  • 6. Changes in the 600 amount and the 500 Rainfall (mm) 400 distribution of 300 rainfall in Sri Lanka 200 100 are not very 0 May Mar Dec Jan Jun Apr Aug Feb Sep Oct Nov Jul apparent 6
  • 7. Variability in climatic parameters: Variability due climate change may overwhelmed by the random variability 5000 4500 Rainfall (mm) 4000 3500 3000 2500 2000 1500 1945 1985 1940 1950 1955 1960 1965 1970 1975 1980 1990 1995 2000 2005 2010 Year 7
  • 8. to identify trends in extreme events of rainfall in low country wet zone of the Island 8
  • 9. 9
  • 10. Daily rainfall data from 8 Agro meteorological stations for the period of 1941-2010 were used 10
  • 11. Agro ecological region, elevation, latitude and longitudes of Agro meteorological stations under investigation Agro- met AER Elevation (m) Latitude Longitude station Awissawella WL1 134 6057’11’’N 80013’6’’E Dartonfield WL1 152 6031’0’’N 80010’0’’E Ratnapura WL1 259 6058’N 80046’E Ambanpitiya WL2 297 7014’0’’N 80020’0’’E Galle WL3 105 7046’N 80017’E Hanwella WL4 81 6054’23’’N 8005’23’’E Kalutara WL4 15 6035’24’’N 79057’36’’E Matara WL4 2 14041’3’’N 39024’52’’E 11
  • 12. At each location, • Annual, monthly and weekly rainfalls • Number of rainy days A rainy day is defined as a day receiving ≥0.5mm rainfall • Wet spells • Dry spells 12
  • 13. • Extreme events were identified using the boundary line technique • Regression techniques to identify trends 13
  • 14. Boundary Line Approach Upper boundary Lower boundary 14
  • 15. 15
  • 16.  Amount and the distribution of rainfall Linear trend and the respective R2 values of total annual rainfalls at each location Location Trend R2 value Ambanpitiya -10.43 0.155 Awissawella -3.99 0.023 Dartonfield -4.334 0.011 Galle -7.127 0.101 Hanwella -1.705 0.005 Kalutara -1.33 0.003 Matara -5.825 0.073 Ratnapura -3.166 0.017 16
  • 17.  Trends of all the locations were not significant  But the signs of the trends were negative  The temporal variations of daily rainfall variability were random in all the locations 17
  • 18. Ambanpitiya 4000 Linear (Ambanpitiya) 3500 Rainfall (mm) 3000 2500 2000 1500 1000 500 0 1941 1945 1949 1953 1957 1961 1965 1969 1973 1977 1981 1985 1989 1993 1997 2001 Year Temporal variation of annual rainfall in Ambanpitiya 18
  • 19. Boundary line analysis on annual rainfall Trends and the R2 Location Trend R2 values for the Ambanpitiya -65.8 * 0.35 lower boundary Awissawella -29.2 0.07 Dartonfield -18.7 0.03 Galle -26.6 * 0.24 Hanwella -12.0 0.05 Kalutara 1.2 0.00 Matara -34.4* 0.17 Ratnapura 10.3 0.06 * Significant at p<0.05 19
  • 20. 3000 Minimum Linear trend 2500 Rainfall (mm) 2000 1500 1000 500 0 1943 1948 1953 1958 1963 1968 1973 1978 1983 1988 1993 1998 2003 2008 year Temporal variations of lower boundary of annual rainfall in Ambanpitiya 20
  • 21.  The temporal variation of maximum and minimum occurrences of annual rainfalls events in some locations were statistically significant  This is an indication of having some years with comparatively low annual rainfalls 21
  • 22.  Temporal variations in wet and dry days Linear trend and the Location Trend R2 respective R2 values Ambanpitiya -1.026*** 0.54 of wet days at each Awissawella -0.611*** 0.22 location Dartonfield -0.211 0.05 Galle -0.327** 0.156 Hanwella -0.458** 0.142 Kalutara -0.524** 0.132 Matara -0.827*** 0.421 Ratnapura -0.004 0.001 ** Significant at p<0.01, ***Significant at p<0.001 22
  • 23. 250 200 Wet days Linear trend No. of Wet days 150 100 50 0 1973 1977 1941 1945 1949 1953 1957 1961 1965 1969 1981 1985 1989 1993 1997 2001 2005 2009 Year Temporal variation of annual wet days together with its linear trend in Ambanpitiya 23
  • 24.  Trends in lower and upper boundary of annual wet days were statistically significant 24
  • 25. 250 Upper boundary Linear trend 200 No. of wet days 150 100 50 0 1953 1943 1948 1958 1963 1968 1973 1978 1983 1988 1993 1998 2003 2008 Year Upper boundary line the trend fitted to annual wet days in Ambanpitiya 25
  • 26. 160 140 Lower boundary Linear trend 120 No. of wet days 100 80 60 40 20 0 1943 1948 1953 1958 1963 1968 1973 1978 1983 1988 1993 1998 2003 2008 Year lower boundary line the trend fitted to annual wet days in Ambanpitiya 26
  • 27.  significant decline in number of wet days  A risk of aggregating heavy showers 27
  • 28.  Temporal variation of maximum dry run Linear trend and the Location Trend R2 respective R2 values Ambanpitiya 0.58** 0.35 of annual maximum Awissawella 0.36** 0.31 dry run in each Dartonfield -0.41 0.12 location Galle 0.08 0.01 Hanwella 0.38** 0.26 Kalutara 0.25 0.07 Matara 0.73** 0.40 Ratnapura 0.14* 0.13 * Significant at p<0.05, **Significant at p<0.01 28
  • 29. 70 Max. dry run Maximum dry run (days) 60 Linear trend 50 40 30 20 10 0 1961 1941 1945 1949 1953 1957 1965 1969 1973 1977 1981 1985 1989 1993 1997 2001 2005 2009 Year Temporal variation of maximum dry run with its linear trend in Ambanpitiya 29
  • 30.  Risk of having lengthy dry spells in some locations in the Low country wet zone 30
  • 31.  No significant change in annual rainfall (Cumulative rainfall)  Significant tendency of having incidences of aggregated heavy showers in the low country wet zone  Signs of lengthy dry spells 31
  • 32.  Adverse impacts on some operations like crop establishment and fertilizer application  Favorable for latex exploitation 32
  • 33. • Director of the Rubber Research Institute of Sri Lanka (RRISL) • Dr. (Mrs.) Wasana Wijesekara, Head of the Biometry Section of RRISL • Mr. Vidura Abeywardena, technical officer of the Biometry Section of RRISL • Department of Meteorology 33
  • 34. 34