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Siklus hidrologi

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Siklus hidrologi

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About this activity

Ilmu Pengetahuan Alam

Created by

hafizha qolbu azkiya
hafizha qolbu azkiya
Indonesia

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Siklus hidrologi
 

Siklus hidrologiOnline version

Ilmu Pengetahuan Alam

by hafizha qolbu azkiya
1 Tunjukkan bagian Transpirasi 2 Tunjukkan bagian Infiltrasi 3 Tunjukkan bagian Presipitasi 4 Tunjukkan bagian Evapotranspirasi 5 Tunjukkan bagian Evaporasi 6 Perahu

Penjelasan

Transpirasi yaitu perubahan air menjadi uap air melalui jaringan hidup tanaman yang terletak di atas permukaan tanah, seperti stomata, lubang kutikula, dan lentisel. Faktor yang memengaruhi transpirasi adalah suhu, pergerakan angin, kelembapan udara, kelembaban tanah, dan jenis tanaman.

Infiltrasi adalah proses masuknya air (biasanya air hujan atau air permukaan) ke dalam tanah melalui pori-pori tanah, celah-celah, atau retakan, atau akar tanaman.

Presipitasi adalah proses mencairnya awan menjadi butiran air akibat suhu udara yang tinggi. Pada tahap ini akan terjadi salah satu gejala alam yang dinamakan dengan hujan atau jatuhnya butiran air ke permukaan bumi. Semakin rendah suhu udara, maka hujan yang dihasilkan menjadi hujan es atau salju (biasanya di bawah 0°C).

Evapotranspirasi adalah gabungan proses penguapan air dari permukaan tanah dan dari makhluk hidup (evaporasi + transpirasi). Proses ini dipengaruhi oleh suhu, radiasi matahari, angin, dan kelembapan. Laju evapotranspirasi meningkat saat suhu, cahaya, dan angin naik, dan menurun saat kelembapan udara tinggi.

Evapotranspirasi yaitu proses penguapan air dari permukaan tanah ke atmosfer yang berarti penguapan dari seluruh air dan makhluk hidup (kombinasi dari evaporasi dan transpirasi). Tahap evapotranspirasi merupakan tahap yang paling berpengaruh dalam siklus hidrologi karena berkaitan dengan tahapan yang saling terangkai atau saling memengaruhi. Laju evapotranspirasi akan bertambah jika suhu, radiasi matahari, dan pergerakan angin meningkat. Laju evapotranspirasi akan berkurang jika kelembapan bertambah.

 
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