Abstract:
The Turkana Jet in northern Kenya is shown to modulate the climate of southwest Ethiopia’s Omo River
Valley using in situ hydrometeorological data, satellite measurements, and atmospheric reanalyses from decadal to diurnal
time scales. Temporal statistics from lowland (2.58–58N, 358–388E) and highland (68–98N, 358–388E) areas show that
850-hPa westward airflow over Lake Turkana is stronger in March and October but is weakened when western Indian
Ocean sea temperatures become warmer than usual at intervals of 2–7 years. A case study on 24 March 2019 reveals how a
stronger Turkana Jet induces warming and drying of the Omo Valley. A second case study on 27 September 2018 reveals
Hadley cell subsidence over the southern flank of the Turkana Jet. We demonstrate how nocturnal airflow draining off the
mountains joins the channelized jet. Satellite and atmospheric reanalyses exhibit realistic diurnal cycles in the east Omo
mountains, but some products have incorrect phase and warm bias. Omo Valley soil moisture and runoff exhibit little trend
in historical records and model projections; however, unpredictable multiyear wet and dry spells and a growing demand for
water are ongoing concerns.
