S Sobirin’s scientific contributions

What is this page?


This page lists works of an author who doesn't have a ResearchGate profile or hasn't added the works to their profile yet. It is automatically generated from public (personal) data to further our legitimate goal of comprehensive and accurate scientific recordkeeping. If you are this author and want this page removed, please let us know.

Publications (1)


Figure 2. Agricultural drought area by classification (DN/digital number).
Area of agricultural drought by land use unit February 2015 Kebumen district (km 2 ).
Area of agricultural drought by land use unit June 2015 Kebumen district (km 2 ).
The potential of agricultural drought according to brightness and wetness index on Kebumen district
  • Article
  • Full-text available

April 2020

·

145 Reads

·

1 Citation

IOP Conference Series Earth and Environmental Science

A I Rasjiddin

·

S Sobirin

·

T Waryono

Drought is a phenomenon resulting irrelevancy or climate in General as a lack of rainfall in the area. Droughts also impact on the surface layer of the soil where the moisture content required to balance organic matter, soil biota, as well as the survival of vegetation. Its categorized by NOAA as drought farms/land. This research is finding potentially soil drought spatially and measured trough index algorithm with wetness and brightness index made by Jensen in Chen (2014) in the District of Kebumen, to see the condition of the organic matter and soil moisture as well as indicators of soil drought by 2015, as well as linked with meteorological drought by the method of standardized precipitation index (SPI) (30 years of rainfall data) statistically. Both the index (wetness and brightness) are calculated on the data of satellite imagery. The results say rain-fed rice land, pasture and moorland is tend to drier that average on months (February, June and December 2015). Those land use become vulnerable to agricultural drought when dry season occur.

Download

Citations (1)


... The interval in each drought class is done by adding up each score from each parameter. The highest score is then reduced by the lowest score divided by the number of classes used [18]. The highest and lowest scores are 15 and 3. ...

Reference:

Drought area of agricultural land using Tasseled Cap Transformation (TCT) method in Ciampel Subdistrict Karawang Regency
The potential of agricultural drought according to brightness and wetness index on Kebumen district

IOP Conference Series Earth and Environmental Science