climatic change

The long-term fluctuations in temperature, precipitation, wind, and all other aspects of the Earth's climate. External processes, such as solar-irradiance variations, variations of the Earth's orbital parameters (eccentricity, precession, and inclination), lithosphere motions, and volcanic activity, are factors in climatic variation. Internal variations of the climate system, e.g., changes in the abundance of greenhouse gases, also may produce fluctuations of sufficient magnitude and variability to explain observed climate change through the feedback processes interrelating the components of the climate system. (Source: GSFC)



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Huntley BJ 2019. Chapter 2: Angola in Outline: Physiography, Climate and Patterns of Biodiversity. Biodiversity of Angola - Science and Conservation: A Modern Synthesis 15-42
Jarre A, Hutchings L, Kirkman S, Kreiner A, Tchipalanga PCM, Kainge P, Uanivi U, Van der Plas A, Blamey L, Coetzee J, Lamont T, Samaai T, Verheye H, Yemane D, Axelsen BE, Ostrowski M, Stenevik EK, Loeng H 2015. Synthesis: Climate effects on biodiversity, abundance and distribution of marine organisms in the Benguela. Fisheries Oceanography (24) 122-149
Rohde RF, Hoffman MT, Durbach T, Venter Z, Jack S 2019. Vegetation and climate change in the Pro-Namib and Namib Desert based on repeat photography: Insights into climate trends. Journal of Arid Environments (165) 119-131
Andersson L, Wilk J, Todd MC, Hughes DA, Earle A, Kniveton D, Layberry R, Savenije HHG 2006. Impact of climate change and development scenarios on flow patterns in the Okavango River. Journal of Hydrology (331) 43-57
Siyambango N, Kanyimba AT, Mufune P 2015. Indigenous knowledge and climate change in rural Namibia: A gendered approach. Indigenous knowledge of Namibia 263-282
Naidoo S, Davis C, Archer van Garderen E 2013. Forests, rangelands and climate change in southern Africa.
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Forests_rangelands and climate change in southern Africa.pdf 1.26 MB
Marion Meyer JJ, Meyer AC, Meyer NL 2020. Sand circles in stony landscapes of Namibia are caused by large Euphorbia shrubs. South African Journal of Botany 130 25-29
Spear D, Zaroug MAH, Daron DD, Ziervogel G, Angula MN, Haimbili EN, Hegga SS, Baudoin M, New M, Kunamwene I, Togarepi C, Davies JE 2018. Vulnerability and responses to climate change in drylands: The case of Namibia. CARIAA-ASSAR Working Paper.
Keja-Kaereho C, Tjizu BR 2019. Climate change and global warming in Namibia: Environmental disasters vs. human life and the economy. Management and Economics Research Journal 5
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Climate Change and Global Warming in Namibia_2019.pdf 239.31 KB
Climate and Development Knowledge Network (CDKN) Opinion: What global warming of 1.5 ℃ and higher means for Botswana and Namibia. The release this week of the Intergovernmental Panel on Climate Change's (IPCC) special report on global warming of 1.5℃ above pre-industrial levels marks a critical point in climate negotiations. Billed in the media as "life changing", the report illustrates how crossing the ever-nearer threshold of 1.5℃ warming will affect the planet, and how difficult it will be to avoid overshooting this target. The special report takes a worldwide look at the growing impacts of climate change. But for countries like Botswana and Namibia, which are highly vulnerable to climate stresses, it's important to understand how surpassing the 1.5℃ global limit will play out at the local level. For these hot, dry and water-stressed countries, local warming and drying will be greater than the global average. So, even a 1.5°C increase in global temperature will have severe local impacts, ushering in intensified and longer droughts and many more heatwaves. Ironically, when rain does fall, it is expected to be much heavier, increasing the risk of heavy flooding within an overall drying climate.
Guo D, Guo R, Cui Y, Midgley GF, Altwegg R, Thiart C 2011. Climate Change Impact on Quiver Trees in Arid Namibia and South Africa. Climate Change - Geophysical Foundations and Ecological Effects 323-324
Hirooka Y, Shoji K, Watanabe Y, Izumi Y, Awala SK, Iijima M 2019. Ridge formation with strip tillage alleviates excess moisture stress for drought-tolerant crops. Soil and Tillage Research 195
Duncan J, Hoffman T, Hill L, Rhode R 2005. Is the flagship of the Richtersveld sinking?. (December 2005) 180-181
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Is the flagship of the Richtersveld sinking.pdf 1.25 MB
Lindsey P, Allan J, Brehony P, Dickman A, Robson A, Begg C, Bhammar H, Blanken L, Breuer T, Fitzgerald K, Flyman M, Gandiwa P, Giva N, Kaelo D, Nampindo S, Nyambe N, Steiner K, Parker A, Roe D, Thomson P, Trimble M, Caron A, Tyrrell P 2020. Conserving Africa's wildlife and wildlands through the COVID-19 crisis and beyond. Nature Ecology and Evolution 2020
Marufu VJ, Hitila M, Donner M, Iita KT, Iyambo KE, Kalili SN, Kamburona TU, Liyeke MM, Mundilo PVI, Nuuyuni SN, Shimwafeni JI, Tjituka V, Tshikesho RS, Seely MK, Throop HL 2016. Rapid soil respiration responses to simulated rainfall along the Namib Desert climate gradient. Journal of the Namibia Scientific Society 64 103-120
Herrick JE, Beh A, Barrios E, Bouvier I, Coetzee M, Dent D, Elias E, Hengl T, Karl JW, Liniger H, Matuszak J, Neff JC, Ndungu LW, Obersteiner M, Shepherd KD, Urama KC, van den Bosch R, Webb NP 2016. The Land-Potential Knowledge System (LandPKS): mobile apps and collaboration for optimizing climate change investments. Ecosystem Health and Sustainability 2 (3) e01209
Dewar G, Stewart BA 2016. Paleoenvironments, Sea Levels, and Land Use in Namaqualand, South Africa, During MIS 6-2. Africa from MIS 6-2: Population Dynamics and Paleoenvironments, Vertebrate Paleobiology and Paleoanthropology 195-211