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ABSTRAKPerubahan iklim merupakan isu yang sedang dihadapi oleh masyarakat
global, yang dipengaruhi oleh variabilitas curah hujan dan suhu udara. Penelitian
ini di lakukan di wilayah sungai Nasal-Padang Guci, dengan menganalisa
trendline curah hujan dan suhu udara, selama kurun waktu 1910-2010, sehingga
diketahui pengaruhnya terhadap neraca air. Penelitian ini menggunakan metode
Mann Kendall Test untuk mengetahui kecendrungan trendline nya, serta metode
Neraca Surplus Defisit untuk menganalisa neraca airnya. Dari hasil analisa
didapatkan bahwa suhu rata-rata bulanan naik sebesar 0,80C selama 54 tahun,
sedangkan kenaikan curah hujan pada tahun 1910-1978 sebesar 20 mm/69 tahun,
dan meningkat selama tahun 1979-2010 sebesar 125 mm/30 tahun. Kenaikan
curah hujan dan suhu udara mempengaruhi ketersediaan dan kebutuhan air di WS
Nasal-Padang Guci, dalam hal ini ketersediaan air dipengaruhi oleh curah hujan
dan evapotranspirasi yang merupakan fungsi dari suhu, sedangkan kebutuhan
airnya dipengaruhi oleh tataguna lahan dan jumlah penduduk. Dari perhitungan
neraca air diketahui bahwa ketersediaan air sungai pada tahun 2030 lebih kecil
dibandingkan dengan 2010, hal ini disebabkan karena pengaruh peningkatan suhu
udara, sehingga nilai evaporasinya semakin besar. Ketersediaan air pada tahun
2010 sebesar 3358,4 juta m3/tahun, sedangkan kebutuhan air untuk irigasi 669
juta m3/tahun (20%), RKI (rumah tangga, perkotaan dan industri) sebesar 87,2
juta m3/tahun (3%), dan sisanya 2602,2 juta m3/tahun (77%), tidak dapat
dimanfaatkan. Ketersediaan air pada tahun 2030 menurun dibandingkan dengan
2010 yaitu sebesar 2498,9 juta m3/tahun, untuk irigasi sebesar 1133,7 juta
m3/tahun (45%), RKI sebesar 136,5 juta m3/tahun (4%), sedangkan sisanya
1228,8 juta m3/tahun (51%) tidak dapat dimanfaatkan. Pada tahun 2010 air masih
bisa mencukupi kebutuhannya dan terjadi defisit pada tahun 2030, yaitu pada
bulan Agustus dan September, sehingga diperlukan bantuan waduk untuk
menyimpan air pada saat surplus, yang nantinya bisa digunakan kembali pada saat
defisit.
ABSTRACTClimate change is a global issue that is currently being faced by the global
comunity, which is strongly influenced by precipitation and air temperature
variability. The research examines the increase rainfall and air temperature, during
the period 1910-2010 in the Nasal-Padang Guci River Area, and its influences on
water balance. The study uses Mann Kendall Test to determine the trend line of
precipitation and air temperature, The methode used water surplus and defisit to
analyze water balance. The temperature rise of 0,80 C/54 years on the average.
Rainfall in the year 1910-1978 increase by 20 mm/69 years, this is considered
reasonable, and does not have any significant effect. However increases
significantly in the year 1979-2010 it amounted to 125 mm/30 years. The increase
of precipitation and air temperature variability affects water availability and water
demand, in the Nasal-Padang Guci river area, in this case water availability is
affected by rainfall and evapotranspiration which is a function of temperature,
while the water demand is influenced by land use and population. From the water
balance calculation the water availability in 2030 is less than 2010, this was due to
the effect of increasing air temperature increases, because increase of evaporation
rate. Water Aviability in the year 2010 amounted to 3358.4 million m3 / year,
while the water demand for irrigation is 669 million m3 / year (20%), household,
urban and industrial amounted to 87.2 million m3 / year (3%), and 2602.2 million
m3 / year (77%), can not be used. Water Aviability in 2030 decreased compared to
2010 amounted to 2498.9 million m3 / year, for irrigation amounted to 1133.7
million m3 / year (45%), household, urban and industrial at 136.5 million m3 / year
(4%), and 1228.8 million m3 / year (51%) con not be used. By 2010 the water was
still meet the demand while by 2030, there will be a deficit in the month of
August and September, so that is the necessary support from reservoirs to store
water surplus, which will be used during the defisit period.;Climate change is a global issue that is currently being faced by the global
comunity, which is strongly influenced by precipitation and air temperature
variability. The research examines the increase rainfall and air temperature, during
the period 1910-2010 in the Nasal-Padang Guci River Area, and its influences on
water balance. The study uses Mann Kendall Test to determine the trend line of
precipitation and air temperature, The methode used water surplus and defisit to
analyze water balance. The temperature rise of 0,80 C/54 years on the average.
Rainfall in the year 1910-1978 increase by 20 mm/69 years, this is considered
reasonable, and does not have any significant effect. However increases
significantly in the year 1979-2010 it amounted to 125 mm/30 years. The increase
of precipitation and air temperature variability affects water availability and water
demand, in the Nasal-Padang Guci river area, in this case water availability is
affected by rainfall and evapotranspiration which is a function of temperature,
while the water demand is influenced by land use and population. From the water
balance calculation the water availability in 2030 is less than 2010, this was due to
the effect of increasing air temperature increases, because increase of evaporation
rate. Water Aviability in the year 2010 amounted to 3358.4 million m3 / year,
while the water demand for irrigation is 669 million m3 / year (20%), household,
urban and industrial amounted to 87.2 million m3 / year (3%), and 2602.2 million
m3 / year (77%), can not be used. Water Aviability in 2030 decreased compared to
2010 amounted to 2498.9 million m3 / year, for irrigation amounted to 1133.7
million m3 / year (45%), household, urban and industrial at 136.5 million m3 / year
(4%), and 1228.8 million m3 / year (51%) con not be used. By 2010 the water was
still meet the demand while by 2030, there will be a deficit in the month of
August and September, so that is the necessary support from reservoirs to store
water surplus, which will be used during the defisit period., Climate change is a global issue that is currently being faced by the global
comunity, which is strongly influenced by precipitation and air temperature
variability. The research examines the increase rainfall and air temperature, during
the period 1910-2010 in the Nasal-Padang Guci River Area, and its influences on
water balance. The study uses Mann Kendall Test to determine the trend line of
precipitation and air temperature, The methode used water surplus and defisit to
analyze water balance. The temperature rise of 0,80 C/54 years on the average.
Rainfall in the year 1910-1978 increase by 20 mm/69 years, this is considered
reasonable, and does not have any significant effect. However increases
significantly in the year 1979-2010 it amounted to 125 mm/30 years. The increase
of precipitation and air temperature variability affects water availability and water
demand, in the Nasal-Padang Guci river area, in this case water availability is
affected by rainfall and evapotranspiration which is a function of temperature,
while the water demand is influenced by land use and population. From the water
balance calculation the water availability in 2030 is less than 2010, this was due to
the effect of increasing air temperature increases, because increase of evaporation
rate. Water Aviability in the year 2010 amounted to 3358.4 million m3 / year,
while the water demand for irrigation is 669 million m3 / year (20%), household,
urban and industrial amounted to 87.2 million m3 / year (3%), and 2602.2 million
m3 / year (77%), can not be used. Water Aviability in 2030 decreased compared to
2010 amounted to 2498.9 million m3 / year, for irrigation amounted to 1133.7
million m3 / year (45%), household, urban and industrial at 136.5 million m3 / year
(4%), and 1228.8 million m3 / year (51%) con not be used. By 2010 the water was
still meet the demand while by 2030, there will be a deficit in the month of
August and September, so that is the necessary support from reservoirs to store
water surplus, which will be used during the defisit period.]