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The Monsoons and Climate Change pp 163–185Cite as

The East African Monsoon System: Seasonal Climatologies and Recent Variations

Part of the Springer Climate book series (SPCL)

Abstract

This chapter briefly reviews the complex climatological cycle of the East African monsoon system, paying special attention to its connection to the larger Indo-Pacific-Asian monsoon cycle. We examine the seasonal monsoon cycle, and briefly explore recent circulation changes. The spatial footprint of our analysis corresponds with the “Greater Horn of Africa” (GHA) region, extending from Tanzania in the south to Yemen and Sudan in the north. During boreal winter, when northeast trade winds flow across the northwest Indian Ocean and the equatorial moisture transports over the Indian Ocean exhibit strong westerly mean flows over the equatorial Indian Ocean, East African precipitation is limited to a few highland areas. As the Indian monsoon circulation transitions during boreal spring, the trade winds over the northwest Indian Ocean reverse, and East African moisture convergence supports the “long” rains. In boreal summer, the southwesterly Somali Jet intensifies over eastern Africa. Subsidence forms along the westward flank of this jet, shutting down precipitation over eastern portions of East Africa. In boreal fall, the Jet subsides, but easterly moisture transports support rainfall in limited regions of the eastern Horn of Africa. We use regressions with the trend mode of global sea surface temperatures to explore potential changes in the seasonal monsoon circulations. Significant reductions in total precipitable water are indicated in Kenya, Tanzania, Rwanda, Burundi, Uganda, Ethiopia, South Sudan, Sudan, and Yemen, with moisture transports broadly responding in ways that reinforce the climatological moisture transports over the Indian Ocean. Over Kenya, southern Ethiopia and Somalia, regressions with velocity potential indicate increased convergence aloft. Near the surface, this convergence appears to manifest as a surface high pressure system that modifies moisture transports in these countries as well as Uganda, Tanzania, Rwanda, and Burundi. An analysis of rainfall changes indicates significant declines in parts of Tanzania, Rwanda, Burundi, Uganda, Kenya, Somalia, Ethiopia, and Yemen.

Keywords

  • East Africa monsoon system
  • Precipitation
  • CHIRPS

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Author information

Authors and Affiliations

  1. US Geological Survey Center for Earth Resources and Observation (EROS) Center, Reston, USA

    Chris Funk

  2. Santa Barbara Climate Hazards Group, University of California, Santa Barbara, CA, USA

    Chris Funk, Andrew Hoell, Shraddhanand Shukla, Greg Husak & Joel Michaelsen

Authors
  1. Chris Funk
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  2. Andrew Hoell
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  3. Shraddhanand Shukla
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  4. Greg Husak
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  5. Joel Michaelsen
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Corresponding author

Correspondence to Chris Funk .

Editor information

Editors and Affiliations

  1. Dept. of Geography and Earth Res. Inst., University of California, SANTA BARBARA, California, USA

    Leila Maria Véspoli de Carvalho

  2. Earth Research Institute, University of California, Santa Barbara, California, USA

    Charles Jones

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Funk, C., Hoell, A., Shukla, S., Husak, G., Michaelsen, J. (2016). The East African Monsoon System: Seasonal Climatologies and Recent Variations. In: de Carvalho, L., Jones, C. (eds) The Monsoons and Climate Change. Springer Climate. Springer, Cham. https://doi.org/10.1007/978-3-319-21650-8_8

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