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The wet season (sometimes called the rainy season) is the time of year when most of a region's average annual rainfall occurs. Generally, the season lasts at least a month. The term green season is also sometimes used as a euphemism by tourist authorities. Areas with wet seasons are dispersed across portions of the tropics and subtropics.
Under the Köppen climate classification, for tropical climates, a wet season month is defined as a month where average precipitation is 60 millimetres (2.4 in) or more. In contrast to areas with savanna climates and monsoon regimes, Mediterranean climates have wet winters and dry summers. Dry and rainy months are characteristic of tropical seasonal forests: in contrast to tropical rainforests, which do not have dry or wet seasons, since their rainfall is equally distributed throughout the year. Some areas with pronounced rainy seasons will see a break in rainfall mid-season, when the intertropical convergence zone or monsoon trough moves to higher latitudes in the middle of the warm season.
When the wet season occurs during a warm season, or summer, precipitation falls mainly during the late afternoon and early evening. In the wet season, air quality improves, fresh water quality improves, and vegetation grows substantially, leading to crop yields late in the season. Rivers overflow their banks, and some animals retreat to higher ground. Soil nutrients diminish and erosion increases. The incidence of malaria and dengue increases in areas where the rainy season coincides with high temperatures, particularly in tropical areas. Some animals have adaptation and survival strategies for the wet season. Often, the previous dry season leads to food shortages in the wet season, as the crops have yet to mature.
Character of the rainfall
In areas where the heavy rainfall is associated with a wind shift, the wet season is known as the monsoon season. Many tropical and subtropical climates experience monsoon rainfall patterns. Rainfall in the wet season is mainly due to daytime heating, which leads to diurnal thunderstorm activity within a pre-existing moist airmass , so the rain mainly falls in late afternoon and early evening in savannah and monsoon regions. Further, much of the total rainfall each day occurs in the first minutes of the downpour, before the storms mature into their stratiform stage. Most places have only one wet season, but areas of the tropics can have two wet seasons, because the monsoon trough, or Intertropical Convergence Zone, can pass over locations in the tropics twice per year. However, since rain forests have rainfall spread evenly through the year, they do not have a wet season.
Areas with a savanna climate in Sub-Saharan Africa, such as Ghana, Burkina Faso, Darfur, Eritrea, Ethiopia, and Botswana have a distinct rainy season. Also subtropical areas like Florida, South and Southeast Texas, and southern Louisiana have a rainy season. Monsoon regions include the Indian subcontinent, Southeast Asia (including Indonesia and Philippines), northern sections of Australia's North, Polynesia, Central America, western and southern Mexico, the Desert Southwest of the United States, southern Guyana, and northeast Brazil.
Northern Guyana has two wet seasons: one in early spring and the other in early winter. In western Africa, there are two rainy seasons across southern sections, but only one across the north. Within the Mediterranean climate regime, the west coast of the United States, the southwest coast of Australia and South Africa, the Mediterranean coastline of Italy, Spain, Greece, Lebanon, Syria, Algeria, Morocco, Tunisia, Israel and Turkey, as well as areas further inland in Western Asia which include Jordan, Northern Iraq and most parts of Iran, experience a wet season in the winter months. Similarly, the wet season in the Negev desert of Israel extends from October through May. At the boundary between the Mediterranean and monsoon climates lies the Sonoran desert, which receives the two rainy seasons associated with each climate regime.
The wet season is known by many different local names throughout the world. For example, in Mexico it is known as "storm season". Different names are given to the various short "seasons" of the year by the Aboriginal tribes of Northern Australia: the wet season typically experienced there from December to March is called Gudjewg. The precise meaning of the word is disputed, although it is widely accepted to relate to the severe thunderstorms, flooding, and abundant vegetation growth commonly experienced at this time.
In tropical areas, when the monsoon arrives, high daytime high temperatures drop and overnight low temperatures increase, thus reducing diurnal temperature variation. During the wet season, a combination of heavy rainfall and, in some places such as Hong Kong, an onshore wind, improve air quality. In Brazil, the wet season is correlated with weaker trade winds off the ocean. The pH level of water becomes more balanced due to the charging of local aquifers during the wet season. Water also softens, as the concentration of dissolved materials reduces during the rainy season. Erosion is also increased during rainy periods. Arroyos that are dry at other times of the year fill with runoff, in some cases with water as deep as 10 feet (3.0 m). Leaching of soils during periods of heavy rainfall depletes nutrients. The higher runoff from land masses affects nearby ocean areas, which are more stratified, or less mixed, due to stronger surface currents forced by the heavy rainfall runoff.
High rainfall can cause widespread flooding, which can lead to landslides and mudflows in mountainous areas. Such floods cause rivers to burst their banks and submerge homes. The Ghaggar-Hakra River, which only flows during India's monsoon season, can flood and severely damage local crops. Floods can be exacerbated by fires that occurred during the previous dry season, which cause soils which are sandy or composed of loam to become hydrophobic, or water repellent. In various ways governments may help people deal with wet season floods. Flood plain mapping identifies which areas are more prone to flooding. Instructions on controlling erosion through outreach[clarification needed] are also provided by telephone or the internet.
The wet season is the main period of vegetation growth within the Savanna climate regime. However, this also means that wet season is a time for food shortages before crops reach their full maturity. This causes seasonal weight changes for people in developing countries, with a drop occurring during the wet season until the time of the first harvest, when weights rebound. Malaria incidence increases during periods of high temperature and heavy rainfall.
Cows calve, or give birth, at the beginning of the wet season. The onset of the rainy season signals the departure of the monarch butterfly from Mexico. Tropical species of butterflies show larger dot markings on their wings to fend off possible predators and are more active during the wet season than the dry season. Within the tropics and warmer areas of the subtropics, decreased salinity of near shore wetlands due to the rains causes an increase in crocodile nesting. Other species, such as the arroyo toad, spawn within the couple of months after the seasonal rains. Armadillos and rattlesnakes seek higher ground.
- Glossary of Meteorology (2013). Rainy season. Archived 2009-02-15 at the Wayback Machine American Meteorological Society. Retrieved on 2008-12-27.
- Costa Rica Guide (2005). When to Travel to Costa Rica. ToucanGuides. Retrieved on 2008-12-27.
- Michael Pidwirny (2008). CHAPTER 9: Introduction to the Biosphere. PhysicalGeography.net. Retrieved on 2008-12-27.
- "Updated world Köppen-Geiger climate classification map" (PDF).
- Elisabeth M. Benders-Hyde (2003). World Climates. Blue Planet Biomes. Retrieved on 2008-12-27.
- J. S. 0guntoyinbo and F. 0. Akintola (1983). Rainstorm characteristics affecting water availability for agriculture. Archived 2009-02-05 at the Wayback Machine IAHS Publication Number 140. Retrieved on 2008-12-27.
- "Malaria Fact Sheet". The World Health Organization. April 2016. Retrieved April 24, 2016.
- Glossary of Meteorology (2009). Monsoon. Archived 2008-03-22 at the Wayback Machine American Meteorological Society. Retrieved on 2009-01-16.
- Robert A. Houze Jr (1997). Stratiform Precipitation in Regions of Convection: A Meteorological Paradox? Bulletin of the American Meteorological Society, pp. 2179. Retrieved on 2008-12-27.
- Patrick Laux et al. (2008): Predicting the regional onset of the rainy season in West Africa. International Journal of Climatology, 28 (3), 329–342.
- Patrick Laux et al. (2009): Modelling daily precipitation features in the Volta Basin of West Africa. International Journal of Climatology, 29 (7), 937–954.,
- David Vandervort (2009). Darfur: getting ready for the rainy season. International Committee of the Red Cross. Retrieved on 2009-02-06.
- Mehari Tesfazgi Mebrhatu, M. Tsubo, and Sue Walker (2004). A Statistical Model for Seasonal Rainfall Forecasting over the Highlands of Eritrea. New directions for a diverse planet: Proceedings of the 4th International Crop Science Congress. Retrieved on 2009-02-08.
- Alex Wynter (2009). Ethiopia: March rainy season "critical" for southern pastoralists. Thomson Reuters Foundation. Retrieved on 2009-02-06.
- The Voice (2009). Botswana: Rainy Season Fills Up Dams. allAfrica.com. Retrieved on 2009-02-06.
- Randy Lascody (2008). The Florida Rain Machine. National Weather Service. Retrieved on 2009-02-06.
- OCHA Partnership for Humanity (2008). OCHA Field Situation Report: Indonesia – Rainy Season 1 December 2008. Archived 18 February 2009 at the Wayback Machine United Nations Office for the Coordination of Humanitarian Affairs. Retrieved on 2009-02-06.
- Burarra Gathering (2006). Burarra Gathering. Archived 2012-03-20 at the Wayback Machine Burarra Gathering. Retrieved on 2009-02-06.
- Tahiti Sun Travel Network (2007). About Bora Bora Island. Retrieved on 2009-02-06.
- Joint Typhoon Warning Center (2006). 2.4 Analysis & Forecasting "Thumb Rules" for the Rainy Season. United States Navy. Retrieved on 2009-02-06.
- Remote Sensing for Migratory Creatures (2002). Phenology and Creature Migration: Dry season and wet season in West Mexico. Arizona Remote Sensing Center. Retrieved on 2009-02-06.
- J. Horel (2006). Normal Monthly Precipitation, Inches. Archived 2006-11-13 at the Wayback Machine University of Utah. Retrieved on 2008-03-19.
- Horace Burton (2006). The climate of Guyana. Archived 2009-01-24 at the Wayback Machine Caribbean Institute for Meteorology and Hydrology. The Outfield, August 2006, pp. 3. Retrieved on 2009-02-08.
- James Brian Elsner (1988). Analysis of Wet Season Rainfall Over the Nordeste of Brazil, South America. University Of Wisconsin-Milwaukee. Retrieved on 2009-02-06.
- C. H. Mari, G. Cailley, L. Corre, M. Saunois, J. L. Attie, V. Thouret, and A. Stohl (2007). Biomass burning plumes during the AMMA wet season experiment. Atmospheric Chemistry and Physics Discussions, pp. 17342. Retrieved on 2009-02-06.
- Greek Embassy London (2008). Welcome to Greece. Government of Greece. Retrieved on 2009-02-06.
- D. Bozkurt, O.L. Sen and M. Karaca (2008). Wet season evaluation of RegCM3 performance for Eastern Mediterranean. EGU General Assembly. Retrieved on 2009-02-06.
- Ron Kahana; Baruch Ziv; Yehouda Enzel & Uri Dayan (2002). "Synoptic Climatology of Major Floods in the Negev Desert, Israel" (PDF). International Journal of Climatology. 22 (7): 869. Bibcode:2002IJCli..22..867K. doi:10.1002/joc.766. Archived from the original (PDF) on 2011-07-19.
- Michael J. Plagens (2009). What and Where is the Sonoran Desert? Arizonensis. Retrieved on 2009-02-07.
- "The Six Seasons". Australian Government, Department of the Environment. Retrieved April 25, 2016.
- Official Web Site of District Sirsa, India (2001). District Sirsa. Archived 2010-12-28 at the Wayback Machine National Informatice Center. Retrieved on 2008-12-27.
- Mei Zheng (2000). The sources and characteristics of atmospheric particulates during the wet and dry seasons in Hong Kong. University of Rhode Island. Retrieved on 2008-12-27.
- S. I. Efe, F. E. Ogban, M. J. Horsfall, E. E. Akporhonor (2005). Seasonal Variations of Physico-chemical Characteristics in Water Resources Quality in Western Niger Delta Region, Nigeria. Journal of Applied Scientific Environmental Management. Retrieved on 2008-12-27.
- C. D. Haynes, M. G. Ridpath, M. A. J. Williams (1991). Monsoonal Australia. Taylor & Francis, pp. 90. ISBN 978-90-6191-638-3. Retrieved on 2008-12-27.
- United States War Department (1909). Road Notes, Cuba. 1909. United States Department of War. Retrieved on 2009-01-16.
- K.W. Choi and J.H.W. Lee (2000). Wet Season Tidal Circulation and flushing in Three Fathoms Cove. Archived 2009-02-27 at the Wayback Machine 4th International Conference on Hydro-Science and Engineering. Retrieved on 2008-12-27.
- Overseas Security Advisory Council (2009). Warden Message: Guyana Rainy Season Flood Hazards.[permanent dead link] Overseas Security Advisory Council. Retrieved on 2009-02-05.
- National Flood Insurance Program (2009). California's Rainy Season. Archived 2012-12-04 at the Wayback Machine Federal Emergency Management Agency. Retrieved on 2009-02-05.
- AFP (2009). Bali Hit By Wet Season Floods. ABC News. Retrieved on 2009-02-06.
- "Sirsa District Disaster Management Plan, 2015-2016" (PDF). District Sirsa. Government of Haryana Department of Revenue and Disaster Management, Haryana Institute of Public Administration. 2015. Archived from the original (PDF) on 2016-03-28. Retrieved April 25, 2016.
- Jack Ainsworth & Troy Alan Doss. Natural History of Fire & Flood Cycles. California Coastal Commission. Retrieved on 2009-02-05.
- FESA (2007). Flood. Archived 2009-05-31 at the Wayback Machine Government of Western Australia. Retrieved on 2009-02-06.
- King County Department of Development and Environmental Services (2009). Erosion and Sediment Control for Construction Sites. King County, Washington Government. Retrieved on 2009-02-06.
- Charles Darwin University (2009). Characteristics of tropical savannas. Archived 2009-02-17 at the Wayback Machine Charles Darwin University. Retrieved on 2008-12-27.
- A. Roberto Frisancho (1993). Human Adaptation and Accommodation. University of Michigan Press, pp. 388. ISBN 978-0-472-09511-7. Retrieved on 2008-12-27.
- Marti J. Van Liere, Eric-Alain D. Ategbo, Jan Hoorweg, Adel P. Den Hartog, and Joseph G. A. J. Hautvast. The significance of socio-economic characteristics for adult seasonal body-weight fluctuations: a study in north-western Benin. British Journal of Nutrition: Cambridge University Press, 1994.
- African Centre of Meteorological Application for Development (2008). Ten Day Climate Bulletin: Dekad of 01 to 10 April, 2008. Archived 2009-02-27 at the Wayback Machine ACMAD. Retrieved on 2009-02-08.
- John P. McNamara, J. France, D. E. Beever (2000). Modelling Nutrient Utilization in Farm Animals. CABI, pp. 275. ISBN 978-0-85199-449-9. Retrieved on 2009-02-06.
- Dr. Lincoln Brower (2005). Precipitation at the Monarch Overwintering Sites in Mexico. Archived 2012-03-22 at WebCite Journey North. Retrieved on 2009-02-06.
- Paul M. Brakefield and Torben B. Larsen (1983). The evolutionary significance of dry and wet season forms in some tropical butterflies. Biological Journal of the Linnean Society, pp. 1–12. Retrieved on 2008-12-27.
- Phil Hall (1989). Crocodiles, Their Ecology, Management, and Conservation. International Union for Conservation of Nature and Natural Resources Crocodile Specialist Group, pp. 167. Retrieved on 2008-12-27.
- San Diego Natural History Museum (2009). Bufo californicus: Arroyo Toad. San Diego Natural History Museum. Retrieved on 2009-01-16.
- Linda Deuver (1978). Dry season, wet season. Archived 2009-01-20 at the Wayback Machine Audubon Magazine, November 1978, pp. 120–130. Retrieved on 2009-02-06.