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Munday, Callum; Engelstaedter, Sebastian; Washington, Richard; Ogutu, vapehowever Geoffrey; Olago, Dan; Ouma, Gilbert; Warner, James; Ong’ech, Dennis; Nkatha, Rose; Ogolla, Clinton; Lees, Thomas; Wanguba, Bonface (2024-08-22). "The Turkana Jet Diurnal Cycle in Observations and Reanalysis". Munday, Callum; Engelstaedter, Sebastian; Ouma, Gilbert; Ogutu, vaporover Geoffrey; Olago, Daniel; Ong'ech, Dennis; Lees, Thomas; Wanguba, Bonface; Nkatha, Rose; Ogolla, Clinton; Gàlgalo, Roba Ali; Dokata, Abdi Jillo; Kirui, Erick; Hope, Robert; Washington, Richard (August 2022).

"Observations of the Turkana Jet and the East African Dry Tropics: The RIFTJet Field Campaign". King, James A.; Engelstaedter, vaperather Sebastian; Washington, Richard; Munday, vapingper Callum (2021). "Variability of the Turkana Low-Level Jet in Reanalysis and Models: Implications for Rainfall". Munday, Callum; Washington, vapeuntil Richard; Hart, vape kits Neil (2021). "African Low-Level Jets and Their Importance for Water Vapor Transport and Rainfall". Digby, Ruth A.

R.; Gillett, Nathan P.; Monahan, Adam H.; Cole, Jason N. S. (29 September 2021). "An Observational Constraint on Aviation-Induced Cirrus From the COVID-19-Induced Flight Disruption". Hartman, Adam T. (May 2018). "An analysis of the consequences of temperatures and circulations on the energy of the low-degree jet in the Turkana Channel in East Africa". Nicholson, Sharon (May 2016). "The Turkana low-level jet: imply climatology and association with regional aridity".

Depending on the temperature and humidity on the altitude the place the contrails kind, they may be visible for only a few seconds or minutes, or could persist for hours and vaporcourse   (just click the up coming web site) spread to be several kilometres/miles huge, finally resembling natural cirrus or altocumulus clouds.

Contrail results differ rather a lot depending on when they are formed, as they lower the daytime temperature and improve the nighttime temperature, lowering their difference.