Seasonal and Diurnal Variability in Near‐Surface Air and Ground Temperature Regimes of the Alpine Zone of Mount Kenya

Abstract Mountains near the equator have very unique temperature regimes due to the tropical latitude and alpine altitude. How climate change will impact these temperature regimes is not clear as there are so few temperature records in these environments. This study attempts to characterize the near...

Full description

Bibliographic Details
Main Authors: Timothy A. Downing, Daniel O. Olago, Tobias Nyumba
Format: Article
Language:English
Published: American Geophysical Union (AGU) 2024-02-01
Series:Earth and Space Science
Subjects:
Online Access:https://doi.org/10.1029/2023EA003410
_version_ 1797290134450733056
author Timothy A. Downing
Daniel O. Olago
Tobias Nyumba
author_facet Timothy A. Downing
Daniel O. Olago
Tobias Nyumba
author_sort Timothy A. Downing
collection DOAJ
description Abstract Mountains near the equator have very unique temperature regimes due to the tropical latitude and alpine altitude. How climate change will impact these temperature regimes is not clear as there are so few temperature records in these environments. This study attempts to characterize the near‐surface air and ground temperature regime for the Teleki Valley (3,200–4,200 m. a.s.l) on the western slope of Mount Kenya using a set of six temperature loggers placed at 200 m elevation intervals. Temperature was recorded at 30 min intervals from September 2021 to October 2022. The mean diurnal temperature range varied from 6°C to 14°C, with maximum daily swings in excess of 25°C. There was a distinct seasonality in temperature, with a hot season during the months of January‐March, where it was roughly 3°C warmer than the coolest months. Diurnal temperature swings were also highest in March. This seasonality is driven by radiation and moisture: higher radiation during the vernal equinox combined with clear skies during the dry season made for higher temperatures. Elevation was the dominant spatial gradient determining temperature regimes, but rock and vegetation cover played a large role in modifying near‐surface air and ground temperature. The highest elevation logger (4,200 m. a.s.l), measuring ground temperature, showed muted seasonal and diurnal swings, creating for warmer temperatures than lower elevation loggers. This demonstrates the importance of thermal refugia at these high elevations. This also makes predictions of plant and animal responses to climate change difficult, as uniform upward shifts would not necessarily maintain thermal niches.
first_indexed 2024-03-07T19:16:03Z
format Article
id doaj.art-6071276fcd144b9d929aa3a4e7943c46
institution Directory Open Access Journal
issn 2333-5084
language English
last_indexed 2024-03-07T19:16:03Z
publishDate 2024-02-01
publisher American Geophysical Union (AGU)
record_format Article
series Earth and Space Science
spelling doaj.art-6071276fcd144b9d929aa3a4e7943c462024-02-29T13:15:57ZengAmerican Geophysical Union (AGU)Earth and Space Science2333-50842024-02-01112n/an/a10.1029/2023EA003410Seasonal and Diurnal Variability in Near‐Surface Air and Ground Temperature Regimes of the Alpine Zone of Mount KenyaTimothy A. Downing0Daniel O. Olago1Tobias Nyumba2Department of Earth and Climate Sciences University of Nairobi Nairobi KenyaDepartment of Earth and Climate Sciences University of Nairobi Nairobi KenyaDepartment of Environment and Geography University of York York UKAbstract Mountains near the equator have very unique temperature regimes due to the tropical latitude and alpine altitude. How climate change will impact these temperature regimes is not clear as there are so few temperature records in these environments. This study attempts to characterize the near‐surface air and ground temperature regime for the Teleki Valley (3,200–4,200 m. a.s.l) on the western slope of Mount Kenya using a set of six temperature loggers placed at 200 m elevation intervals. Temperature was recorded at 30 min intervals from September 2021 to October 2022. The mean diurnal temperature range varied from 6°C to 14°C, with maximum daily swings in excess of 25°C. There was a distinct seasonality in temperature, with a hot season during the months of January‐March, where it was roughly 3°C warmer than the coolest months. Diurnal temperature swings were also highest in March. This seasonality is driven by radiation and moisture: higher radiation during the vernal equinox combined with clear skies during the dry season made for higher temperatures. Elevation was the dominant spatial gradient determining temperature regimes, but rock and vegetation cover played a large role in modifying near‐surface air and ground temperature. The highest elevation logger (4,200 m. a.s.l), measuring ground temperature, showed muted seasonal and diurnal swings, creating for warmer temperatures than lower elevation loggers. This demonstrates the importance of thermal refugia at these high elevations. This also makes predictions of plant and animal responses to climate change difficult, as uniform upward shifts would not necessarily maintain thermal niches.https://doi.org/10.1029/2023EA003410temperature regimetropical alpinefrost daysthermal nichelapse rate
spellingShingle Timothy A. Downing
Daniel O. Olago
Tobias Nyumba
Seasonal and Diurnal Variability in Near‐Surface Air and Ground Temperature Regimes of the Alpine Zone of Mount Kenya
Earth and Space Science
temperature regime
tropical alpine
frost days
thermal niche
lapse rate
title Seasonal and Diurnal Variability in Near‐Surface Air and Ground Temperature Regimes of the Alpine Zone of Mount Kenya
title_full Seasonal and Diurnal Variability in Near‐Surface Air and Ground Temperature Regimes of the Alpine Zone of Mount Kenya
title_fullStr Seasonal and Diurnal Variability in Near‐Surface Air and Ground Temperature Regimes of the Alpine Zone of Mount Kenya
title_full_unstemmed Seasonal and Diurnal Variability in Near‐Surface Air and Ground Temperature Regimes of the Alpine Zone of Mount Kenya
title_short Seasonal and Diurnal Variability in Near‐Surface Air and Ground Temperature Regimes of the Alpine Zone of Mount Kenya
title_sort seasonal and diurnal variability in near surface air and ground temperature regimes of the alpine zone of mount kenya
topic temperature regime
tropical alpine
frost days
thermal niche
lapse rate
url https://doi.org/10.1029/2023EA003410
work_keys_str_mv AT timothyadowning seasonalanddiurnalvariabilityinnearsurfaceairandgroundtemperatureregimesofthealpinezoneofmountkenya
AT danieloolago seasonalanddiurnalvariabilityinnearsurfaceairandgroundtemperatureregimesofthealpinezoneofmountkenya
AT tobiasnyumba seasonalanddiurnalvariabilityinnearsurfaceairandgroundtemperatureregimesofthealpinezoneofmountkenya