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57-635: The area along the Tati River was pit mined by the Bakalanga before the arrival of Europeans. It may have been one of the sources of wealth for the Great Zimbabwe empire (c. 1200 to 1450). In 1866, Karl Mauch discovered the Tati goldfield, making it the first one discovered by Europeans in southern Africa. This led to the first South African gold rush. The gold mineralization occurs in quartz veins, intruded into

114-446: A decrease below the minimum leading to direct danger for amphibian life), increased pollution of surface water , the drying out of wetlands , more and larger wildfires , higher deflation intensity, loss of biodiversity , worse health of trees and the appearance of pests and dendroid diseases. Drought-induced mortality of trees lacks in most climate models in their representation of forests as land carbon sink . Economic losses as

171-465: A disastrous drought soon struck Mapungubgwe, and the Shashe - Limpopo region was uninhabited between A.D 1300 and 1420, forcing the ordinary population to scatter. Mapungubgwe had become a ghost town by AD 1290. Its golden era lasted no more than 50 years culminating in the rise of Great Zimbabwe . Later, in the 15th century, the centre of power moved back west, from Great Zimbabwe to Khami/Nkami and in

228-487: A diverse climate, ranging from hot, dry regions to cooler, wetter highland regions. The region has considerable variability in seasonal rainfall and a very complex topography. In the northern parts of the region within the Nile basin (Ethiopia, Sudan), the rainfall is characterized by an unimodal cycle with a wet season from July to September. The rest of the region has a bimodal annual cycle, featuring long rains from March to May and

285-562: A drought developing, with subsequent increased wildfire risks. Heat waves can significantly worsen drought conditions by increasing evapotranspiration . This dries out forests and other vegetation, and increases the amount of fuel for wildfires. Drought is a recurring feature of the climate in most parts of the world, becoming more extreme and less predictable due to climate change , which dendrochronological studies date back to 1900. There are three kinds of drought effects, environmental, economic and social. Environmental effects include

342-434: A factor which increases the gap between developed and developing countries . Effects vary according to vulnerability. For example, subsistence farmers are more likely to migrate during drought because they do not have alternative food-sources. Areas with populations that depend on water sources as a major food-source are more vulnerable to famine. Further examples of social and health consequences include: Wind erosion

399-498: A high level of reflected sunlight and above average prevalence of high pressure systems , winds carrying continental, rather than oceanic air masses, and ridges of high pressure areas aloft can prevent or restrict the developing of thunderstorm activity or rainfall over one certain region. Once a region is within drought, feedback mechanisms such as local arid air, hot conditions which can promote warm core ridging, and minimal evapotranspiration can worsen drought conditions. Within

456-434: A longer duration. Precipitation can be divided into three categories, based on whether it falls as liquid water, liquid water that freezes on contact with the surface, or ice. Droughts occur mainly in areas where normal levels of rainfall are, in themselves, low. If these factors do not support precipitation volumes sufficiently to reach the surface over a sufficient time, the result is a drought. Drought can be triggered by

513-461: A multi-agency partnership, drought is generally defined as "a deficiency of precipitation over an extended period of time (usually a season or more), resulting in a water shortage". The National Weather Service office of the NOAA defines drought as "a deficiency of moisture that results in adverse impacts on people, animals, or vegetation over a sizeable area". Drought is a complex phenomenon − relating to

570-606: A result of droughts include lower agricultural, forests, game and fishing output, higher food-production costs, lower energy-production levels in hydro plants, losses caused by depleted water tourism and transport revenue, problems with water supply for the energy sector and for technological processes in metallurgy, mining, the chemical, paper, wood, foodstuff industries etc., disruption of water supplies for municipal economies. Further examples of common environmental and economic consequences of drought include: Droughts can cause land degradation and loss of soil moisture, resulting in

627-549: A result. This means even regions where overall rainfall is expected to remain relatively stable will experience these impacts. These regions include central and northern Europe. Without climate change mitigation, around one third of land areas are likely to experience moderate or more severe drought by 2100. Due to global warming droughts are more frequent and intense than in the past. Human activity can directly trigger exacerbating factors such as over-farming, excessive irrigation , deforestation , and erosion adversely impact

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684-646: A significant role in drought. ENSO comprises two patterns of temperature anomalies in the central Pacific Ocean , known as La Niña and El Niño . La Niña events are generally associated with drier and hotter conditions and further exacerbation of drought in California and the Southwestern United States , and to some extent the U.S. Southeast . Meteorological scientists have observed that La Niñas have become more frequent over time. Conversely, during El Niño events, drier and hotter weather occurs in parts of

741-570: A single dataset can be limiting, as it may not capture the full spectrum of drought characteristics and impacts. Careful monitoring of moisture levels can also help predict increased risk for wildfires. Mechanisms of producing precipitation include convective , stratiform , and orographic rainfall. Convective processes involve strong vertical motions that can cause the overturning of the atmosphere in that location within an hour and cause heavy precipitation, while stratiform processes involve weaker upward motions and less intense precipitation over

798-624: A southern Bantu ethnic group mainly inhabiting Matebeleland in Zimbabwe , northern Botswana, and parts of the Limpopo Province in South Africa . The BaKalanga of Botswana are the second largest ethnic group in the country, and their Ikalanga language being the second most spoken in the country (most prevalent in the North).The TjiKalanga language of Zimbabwe is the third most spoken language in

855-666: A water supply crisis across much of the country. As a result, many desalination plants were built for the first time ( see list ). By far the largest part of Australia is desert or semi-arid lands commonly known as the outback . A 2005 study by Australian and American researchers investigated the desertification of the interior, and suggested that one explanation was related to human settlers who arrived about 50,000 years ago. Regular burning by these settlers could have prevented monsoons from reaching interior Australia. In June 2008 it became known that an expert panel had warned of long term, maybe irreversible, severe ecological damage for

912-496: A widespread blanket deposit that covers areas of hundreds of square kilometers and tens of meters thick. Loess often stands in either steep or vertical faces. Loess tends to develop into highly rich soils. Under appropriate climatic conditions, areas with loess are among the most agriculturally productive in the world. Loess deposits are geologically unstable by nature, and will erode very readily. Therefore, windbreaks (such as big trees and bushes) are often planted by farmers to reduce

969-426: Is a similar concept to water scarcity . The different categories of droughts have different causes but similar effects: Several indices have been defined to quantify and monitor drought at different spatial and temporal scales. A key property of drought indices is their spatial comparability, and they must be statistically robust. Drought indices include: High-resolution drought information helps to better assess

1026-453: Is also negatively effected by drought stress, the reduction in crop yield results from a decrease in photosynthetic rate, changes in leaf development, and altered allocation of resources all due to drought stress. Crop plants exposed to drought stress suffer from reductions in leaf water potential and transpiration rate. Water-use efficiency increases in crops such as wheat while decreasing in others, such as potatoes. Plants need water for

1083-477: Is insufficient rainfall to support vegetation. Drought is one of the most complex and major natural hazards , and it has devastating impacts on the environment, economy, water resources, agriculture, and society worldwide. One can divide the impacts of droughts and water shortages into three groups: environmental, economic and social (including health). Environmental effects of droughts include: lower surface and subterranean water-levels, lower flow-levels (with

1140-488: Is much more severe in arid areas and during times of drought. For example, in the Great Plains , it is estimated that soil loss due to wind erosion can be as much as 6100 times greater in drought years than in wet years. Loess is a homogeneous, typically nonstratified, porous, friable , slightly coherent, often calcareous, fine-grained, silty , pale yellow or buff, windblown ( Aeolian ) sediment . It generally occurs as

1197-410: Is related to low runoff, streamflow, and reservoir and groundwater storage. An agricultural or ecological drought is causing plant stress from a combination of evaporation and low soil moisture . Some organizations add another category: socioeconomic drought occurs when the demand for an economic good exceeds supply as a result of a weather-related shortfall in water supply. The socioeconomic drought

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1254-462: Is the headquarters for the Hosanna's of Botswana, South Africa and Zimbabwe. Drought A drought is a period of drier-than-normal conditions. A drought can last for days, months or years. Drought often has large impacts on the ecosystems and agriculture of affected regions, and causes harm to the local economy . Annual dry seasons in the tropics significantly increase the chances of

1311-488: Is the heterogeneous distribution of hydrologic extremes in space and time. For instance, El Niño can cause droughts in one part of the region and floods in the other. This is also a common situation within a country, e.g., in Ethiopia. The recent years with consecutive droughts followed by floods are a testament to the need to better forecast these kinds of events and their impacts. Approximately 2.4 billion people live in

1368-1056: The Amazon River Basin, Colombia , and Central America . Winters during the El Niño are warmer and drier than average conditions in the Northwest, northern Midwest, and northern Mideast United States, so those regions experience reduced snowfalls. Conditions are also drier than normal from December to February in south-central Africa, mainly in Zambia , Zimbabwe , Mozambique , and Botswana . Direct effects of El Niño resulting in drier conditions occur in parts of Southeast Asia and Northern Australia , increasing bush fires , worsening haze , and decreasing air quality dramatically. Drier-than-normal conditions are also in general observed in Queensland , inland Victoria , inland New South Wales , and eastern Tasmania from June to August. As warm water spreads from

1425-519: The Amazon basin , Australia , the Sahel region and India . For example, in 2005, parts of the Amazon basin experienced the worst drought in 100 years. Australia could experience more severe droughts and they could become more frequent in the future, a government-commissioned report said on July 6, 2008. The long Australian Millennial drought broke in 2010. The 2020–2022 Horn of Africa drought has surpassed

1482-623: The Kingdom of Butua came as a result of a series of invasions, beginning with the Bangwato Kgosi Kgari's ill-fated incursion of around 1828 and culminating in the onslaught of Mzilikazi 's Amandebele . The Kalanga people are known for their rain-making abilities through their Supreme Being Mwali/Ngwali. These abilities have always been a part of the BaKalanga people history as well as all those other related groups. The rain-making has always been

1539-499: The drainage basin of the Himalayan rivers. India , China , Pakistan , Bangladesh , Nepal and Myanmar could experience floods followed by droughts in coming decades. More than 150 districts in India are drought vulnerable, mostly concentrated in the state of Rajasthan, Gujarat, Madhya Pradesh and its adjoining Chhattisgarh, Uttar Pradesh, northern Karnataka and adjoining Maharashtra of

1596-492: The 17th century to Danan'ombe (Dlodlo). The moves were accompanied by changes of the dominance from one clan to another. In the 17th century, the rozvi established southern BaKalanga became a powerful competitor, controlling most of the mining areas. The Rozvi even repelled Portuguese colonists from some of their inland posts. In south-western Zimbabwe (now Matabeleland ) and adjacent parts of present-day Botswana, Kalanga states survived for more than another century. The fall of

1653-508: The Horn of Africa during the period 2020–2023 leading to the third longest and most widespread drought on record with dire implications for food security (see Horn of Africa drought (2020–present) ). Conversely, other parts experienced extreme floods, e.g., the 2020 East Africa floods in Ethiopia, Rwanda, Kenya, Burundi, and Uganda, and the 2022 floods in South Sudan. A key feature in the region

1710-585: The Indian Ocean coast for goods such as glass beads and cotton clothes. The majority of these prehistoric Bakalanga villages have been discovered in Botswana and Zimbabwe in areas close to major rivers and were usually built on terraced hilltops with stone walls built around them. The Kalanga are linked to such early African States as Mapungubgwe , Khami, and the Rozvi Empire . The early Bakalanga people living in

1767-474: The Shashe-Limpopo basin monopolised trade due to their access to the Indian Ocean coast. By around AD 1220 a new and more powerful kingdom developed around Mapungubgwe Hill, near Botswana's border with South Africa. Some of the early Bakalanga people living in the lower Shashe-Limpopo valley probably moved towards or became part of this newly formed kingdom. But studies of climatic data from the area suggest that

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1824-478: The ability of the land to capture and hold water. In arid climates, the main source of erosion is wind. Erosion can be the result of material movement by the wind. The wind can cause small particles to be lifted and therefore moved to another region (deflation). Suspended particles within the wind may impact on solid objects causing erosion by abrasion (ecological succession). Wind erosion generally occurs in areas with little or no vegetation, often in areas where there

1881-526: The absence of water − which is difficult to monitor and define. By the early 1980s, over 150 definitions of "drought" had already been published. The range of definitions reflects differences in regions, needs, and disciplinary approaches. There are three major categories of drought based on where in the water cycle the moisture deficit occurs: meteorological drought, hydrological drought, and agricultural or ecological drought. A meteorological drought occurs due to lack of precipitation . A hydrological drought

1938-534: The country, however, being recognized as a Western Shona branch of the Shona group of languages. It is likewise used in mass media. The most notable Kalanga clans are the boSungwasha, boMndambeli, boNeswimbo, boNtombo, boKumbudzi, boKadzasha, and boPhizha na boNebukhwa. The native language of the Kalanga people is referred to as Ikalanga or TjiKalanga . The language has a number of tribal dialects depending on which part of

1995-448: The destruction of cropland productivity. This can result in diminished crop growth or yield productions and carrying capacity for livestock . Drought in combination with high levels of grazing pressure can function as the tipping point for an ecosystem, causing woody encroachment . Water stress affects plant development and quality in a variety of ways: firstly drought can cause poor germination and impaired seedling development. At

2052-421: The drying of wetlands , more and larger wildfires, loss of biodiversity . Economic impacts of drought result due to negative disruptions to agriculture and livestock farming (causing food insecurity ), forestry, public water supplies , maritime navigation (due to e.g.: lower water levels), electric power supply (by affecting hydropower systems) and impacts on human health. Social and health costs include

2109-567: The duty of the Hosanna's or AmaWosana (the high priests in Mwali/Ngwali's church). The traditional attire of the Kalanga/BaKalanga people clearly shows the importance of rain to BaKalanga. They put on black skirts which represent dark clouds heavy with rain, and the white shirts to represent rain droplets. This is the attire worn when they go and plead for rain at Njelele shrine in Zimbabwe, which

2166-459: The health of people who are directly exposed to this phenomenon (excessive heat waves ). Droughts can also cause limitations of water supplies, increased water pollution levels, high food-costs, stress caused by failed harvests, water scarcity , etc. Reduced water quality can occur because lower water-flows reduce dilution of pollutants and increase contamination of remaining water sources. This explains why droughts and water scarcity operate as

2223-419: The horrific drought in 2010–2011 in both duration and severity. More than 150 districts in India are drought vulnerable, mostly concentrated in the state of Rajasthan, Gujarat, Madhya Pradesh and its adjoining Chhattisgarh, Uttar Pradesh, northern Karnataka and adjoining Maharashtra of the country. Throughout history, humans have usually viewed droughts as disasters due to the impact on food availability and

2280-507: The lack of water in the plants, bushfires are common. Since water vapor becomes more energetic with increasing temperature, more water vapor is required to increase relative humidity values to 100% at higher temperatures (or to get the temperature to fall to the dew point). Periods of warmth quicken the pace of fruit and vegetable production, increase evaporation and transpiration from plants, and worsen drought conditions. The El Niño–Southern Oscillation (ENSO) phenomenon can sometimes play

2337-415: The negative effect on the health of people directly exposed to this phenomenon (excessive heat waves), high food costs, stress caused by failed harvests, water scarcity , etc. Drought can also lead to increased air pollution due to increased dust concentrations and wildfires . Prolonged droughts have caused mass migrations and humanitarian crisis . Examples for regions with increased drought risks are

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2394-515: The occurrence of droughts has increased as a result of the increase in temperature and atmospheric evaporative demand . In addition, increased climate variability has increased the frequency and severity of drought events. Moreover, the occurrence and impact of droughts are aggravated by anthropogenic activities such as land use change and water management and demand. The IPCC Sixth Assessment Report also pointed out that "Warming over land drives an increase in atmospheric evaporative demand and in

2451-535: The rainforest towards a " tipping point " where it would irreversibly start to die. It concludes that the rainforest is on the brink of being turned into savanna or desert , with catastrophic consequences for the world's climate. According to the WWF , the combination of climate change and deforestation increases the drying effect of dead trees that fuels forest fires. The 1997–2009 Millennium Drought in Australia led to

2508-543: The reduction in plant growth and yields. Another factor influencing reduced plant growth and yields include the allocation of resources; following drought stress plants will allocate more resources to roots to aid in water uptake increasing root growth and reducing the growth of other plant parts while decreasing yields. The most negative impacts of drought for humans include crop failure , food crisis , famine, malnutrition, and poverty , which lead to loss of life and mass migration of people. There are negative effects on

2565-451: The rest of society. People have viewed drought as a natural disaster or as something influenced by human activity , or as a result of supernatural forces. The IPCC Sixth Assessment Report defines a drought simply as "drier than normal conditions". This means that a drought is "a moisture deficit relative to the average water availability at a given location and season". According to National Integrated Drought Information System ,

2622-564: The same time plant growth relies on cellular division, cell enlargement, and differentiation. Drought stress impairs mitosis and cell elongation via loss of turgor pressure which results in poor growth. Development of leaves is also dependent upon turgor pressure, concentration of nutrients, and carbon assimilates all of which are reduced by drought conditions, thus drought stress lead to a decrease in leaf size and number. Plant height, biomass, leaf size and stem girth has been shown to decrease in maize under water limiting conditions. Crop yield

2679-460: The severity of drought events" and "Increased atmospheric evaporative demand increases plant water stress, leading to agricultural and ecological drought". There is a rise of compound warm-season droughts in Europe that are concurrent with an increase in potential evapotranspiration . Higher temperatures increase evaporation. This dries the soil and increases plant stress . Agriculture suffers as

2736-466: The short rains from October to December. The frequent occurrence of hydrological extremes, like droughts and floods , harms the already vulnerable population suffering from severe poverty and economic turmoil. Droughts prompted food shortages for example in 1984–85 , 2006 and 2011 . The Eastern African region experiences the impacts of climate change in different forms. For instance, below-average rainfall occurred for six consecutive rainy seasons in

2793-450: The spatial and temporal changes and variability in drought duration, severity, and magnitude at a much finer scale. This supports the development of site-specific adaptation measures. The application of multiple indices using different datasets helps to better manage and monitor droughts than using a single dataset, This is particularly the case in regions of the world where not enough data is available such as Africa and South America. Using

2850-693: The surrounding peoples of southern Africa . The BaKalanga are one of the largest ethnolinguistic groups in Botswana . The 1946 census indicated that there were 39,773 (49% of the numerically largest district) BaKalanga in the Bamangwato (Central) District. According to Huffman (2008), the original Bakalanga people descended from Leopard's Kopje farmers. These people occupied areas covering parts of north eastern Botswana , western and southern Zimbabwe , adjacent parts of South Africa and Mozambique by around AD 100. They traded in ivory , furs and feathers with

2907-749: The tribal territory you are situated. There are among others the Talaunda dialect, the Lilima dialect, Jawunda dialect, the Nanzwa dialect, Tjigwizi dialect as well as Tjindodondo dialect (dominant in Zimbabwe ). Together with the Nambya language , these varieties form the western branch of the shona group (Guthrie S.10) that also includes Central Shona . Kalanga-speakers once numbered over 1,900,000, though they are now reduced, often speaking Ndebele or Central Shona languages in Zimbabwe, Tswana in Botswana, and other local languages of

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2964-572: The tropics, distinct, wet and dry seasons emerge due to the movement of the Intertropical Convergence Zone or Monsoon trough . The dry season greatly increases drought occurrence, and is characterized by its low humidity, with watering holes and rivers drying up. Because of the lack of these watering holes, many grazing animals are forced to migrate due to the lack of water in search of more fertile lands. Examples of such animals are zebras , elephants , and wildebeest . Because of

3021-414: The uptake of nutrients from the soil, and for the transport of nutrients throughout the plant: drought conditions limit these functions leading to stunted growth. Drought stress also causes a decrease in photosynthetic activity in plants due to the reduction of photosynthetic tissues, stomatal closure, and reduced performance of photosynthetic machinery. This reduction in photosynthetic activity contributes to

3078-582: The volcano-sedimentary rocks of the Tati greenstone belt. Other economic minerals occur including nickel and copper. The major formation is the Selkirk Formation which is up to 1000 meters thick. The Selkirk is composed mostly of redeposited dacite and rhyolite , with some darker volcanics, and minor quartzites and quartzitic schists . 21°06′00″S 27°41′50″E  /  21.10000°S 27.69722°E  / -21.10000; 27.69722 Kalanga people The Kalanga or BaKalanga are

3135-459: The west Pacific and the Indian Ocean to the east Pacific, it causes extensive drought in the western Pacific. Singapore experienced the driest February in 2014 since records began in 1869, with only 6.3 mm of rain falling in the month and temperatures hitting as high as 35 °C on 26 February. The years 1968 and 2005 had the next driest Februaries, when 8.4 mm of rain fell. Globally,

3192-717: The whole Murray-Darling basin if it did not receive sufficient water by October 2008. Australia could experience more severe droughts and they could become more frequent in the future, a government-commissioned report said on July 6, 2008. Australian environmentalist Tim Flannery , predicted that unless it made drastic changes, Perth in Western Australia could become the world's first ghost metropolis , an abandoned city with no more water to sustain its population. The long Australian Millennial drought broke in 2010. East Africa , including for example Ethiopia, Eritrea, Kenya, Somalia, South Sudan, Sudan, Tanzania, and Uganda, has

3249-501: The wind erosion of loess. In 2005, parts of the Amazon basin experienced the worst drought in 100 years. A 2006 article reported results showing that the forest in its present form could survive only three years of drought. Scientists at the Brazilian National Institute of Amazonian Research argue in the article that this drought response, coupled with the effects of deforestation on regional climate, are pushing

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