A Gaussian model approach to determine the commencement, termination and length of the major growing season over the dry zone of Sri Lanka
Author:
Funder
Sabaragamuwa University of Sri Lanka Research Grant
Publisher
Springer Science and Business Media LLC
Subject
Atmospheric Science
Link
https://link.springer.com/content/pdf/10.1007/s00704-022-03964-2.pdf
Reference40 articles.
1. Adejuwon JO, Odekunle TO (2006) Variability and the Severity of the “Little Dry Season” in Southwestern Nigeria. J Clim 19:483–493. https://doi.org/10.1175/JCLI3642.1
2. Adejuwon JO, Balogun EE, Adejuwon SA (1990) On the annual and seasonal patterns of rainfall fluctuations in sub-Saharan West Africa. Int J Climatol 10:839–848. https://doi.org/10.1002/joc.3370100806
3. Ampitiyawatta AD, Wijeratne AW (2015) Impact of temporal changes of rainfall on major climatic zones of Sri Lanka. Trop Agric Res Ext 18:148–152
4. Basnayake BRSB (2007) Climate change. In: The National Atlas of Sri Lanka. Survey Department of Sri Lanka, Colombo, Sri Lanka, pp 54–55
5. Benoit P (1977) The start of the growing season in Northern Nigeria. Agric Meteorol 18:91–99. https://doi.org/10.1016/0002-1571(77)90042-5
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