Rwenzori Mountains National Park - Revision history

WikiEdit at 21:54, 15 October 2026

2026-10-15T21:54:43Z

← Older revision		Revision as of 17:54, 15 October 2026
Line 401:		Line 401:
	<span id="R01613"></span>Uganda. World Heritage Centre, UNESCO.		<span id="R01613"></span>Uganda. World Heritage Centre, UNESCO.

	<span id="R02310"></span>Kiribou, R., Tehoda, P., Chukwu, O., Bempah, G., Kühl, H. S., Ferreira, J., …, & Heinicke, S. (2024). Exposure of African ape sites to climate change impacts. ''PLOS Climate'', 3(2), ~~1-19~~. [https://doi.org/10.1371/journal.pclm.0000345 doi:10.1371/journal.pclm.0000345]		<span id="R02310"></span>Kiribou, R., Tehoda, P., Chukwu, O., Bempah, G., Kühl, H. S., Ferreira, J., …, & Heinicke, S. (2024). Exposure of African ape sites to climate change impacts. ''PLOS Climate'', 3(2), e0000345. [https://doi.org/10.1371/journal.pclm.0000345 doi:10.1371/journal.pclm.0000345]



	'''Page created by: '''APES Atlas Team''' Date:''' 2020-12-30		'''Page created by: '''APES Atlas Team''' Date:''' 2020-12-30

WikiEdit at 14:35, 15 October 2026

2026-10-15T14:35:49Z

← Older revision		Revision as of 10:35, 15 October 2026
Line 401:		Line 401:
	<span id="R01613"></span>Uganda. World Heritage Centre, UNESCO.		<span id="R01613"></span>Uganda. World Heritage Centre, UNESCO.

	<span id="R02310"></span>Kiribou, R., Tehoda, P., Chukwu, O., Bempah, G., Kühl, H. S., Ferreira, J., …, & Heinicke, S. (2024). Exposure of African ape sites to climate change impacts. ''PLOS Climate'', 3(2), ~~e0000345~~. [https://doi.org/10.1371/journal.pclm.0000345 doi:10.1371/journal.pclm.0000345]		<span id="R02310"></span>Kiribou, R., Tehoda, P., Chukwu, O., Bempah, G., Kühl, H. S., Ferreira, J., …, & Heinicke, S. (2024). Exposure of African ape sites to climate change impacts. ''PLOS Climate'', 3(2), 1-19. [https://doi.org/10.1371/journal.pclm.0000345 doi:10.1371/journal.pclm.0000345]



	'''Page created by: '''APES Atlas Team''' Date:''' 2020-12-30		'''Page created by: '''APES Atlas Team''' Date:''' 2020-12-30

WikiEdit at 00:10, 15 October 2026

2026-10-15T00:10:42Z

← Older revision		Revision as of 20:10, 14 October 2026
Line 120:		Line 120:
	\|5.1 Hunting & collecting terrestrial animals		\|5.1 Hunting & collecting terrestrial animals
	\|Present (unknown severity)		\|Present (unknown severity)
	\|Hunting for bushmeat ([~~https://whc.unesco.org/en/soc/971~~#~~:~:text=The%20main%20threats%20to%20the,resource%20harvesting%2C%20especially%20of%20bamboo.~~ UNESCO]).		\|Hunting for bushmeat ([[#R01613\|UNESCO]]).
	\|Ongoing (2020)		\|Ongoing (2020)
	\|-		\|-
Line 126:		Line 126:
	\|5.2 Gathering terrestrial plants		\|5.2 Gathering terrestrial plants
	\|Present (unknown severity)		\|Present (unknown severity)
	\|Harvesting plants, especially bamboo ([~~https://whc.unesco.org/en/soc/971~~#~~:~:text=The%20main%20threats%20to%20the,resource%20harvesting%2C%20especially%20of%20bamboo.~~ UNESCO]).		\|Harvesting plants, especially bamboo ([[#R01613\|UNESCO]]).
	\|Ongoing (2020)		\|Ongoing (2020)
	\|-		\|-
Line 132:		Line 132:
	\|5.3 Logging & wood harvesting		\|5.3 Logging & wood harvesting
	\|Present (unknown severity)		\|Present (unknown severity)
	\|Illegal logging ([~~https://whc.unesco.org/en/soc/971~~#~~:~:text=The%20main%20threats%20to%20the,resource%20harvesting%2C%20especially%20of%20bamboo.~~ UNESCO]).		\|Illegal logging ([[#R01613\|UNESCO]]).
	\|Ongoing (2020)		\|Ongoing (2020)
	\|}		\|}
Line 152:		Line 152:
	\|2 Counter-wildlife crime		\|2 Counter-wildlife crime
	\|2.3 Conduct regular anti-poaching patrols		\|2.3 Conduct regular anti-poaching patrols
	\|Anti-poaching patrols are conducted at the site ([~~https://whc.unesco.org/en/soc/971~~#~~:~:text=The%20main%20threats%20to%20the,resource%20harvesting%2C%20especially%20of%20bamboo.~~ UNESCO]).		\|Anti-poaching patrols are conducted at the site ([[#R01613\|UNESCO]]).
	\|		\|
	\|1991-Ongoing (2020)		\|1991-Ongoing (2020)

WikiEdit at 20:30, 12 October 2026

2026-10-12T20:30:42Z

← Older revision		Revision as of 16:30, 12 October 2026
Line 17:		Line 17:
	= Site characteristics =		= Site characteristics =

	Located in western Uganda, Rwenzori Mountains National Park comprises part of the Rwenzori mountain chain, including Africa's third highest peak, Mt Stanley's Margherita Peak at 5,109 m above sea level ([https://whc.unesco.org/en/list/684/ UNESCO]). The park is contiguous with the Virunga National Park in the Democratic Republic of the Congo (BirdLife International 2020). The region's glaciers, waterfalls and lakes make it one of the most fascinating afro-alpine areas.The park is known for its rich and unique flora; some of the world's rarest vegetation can be found here ([https://whc.unesco.org/en/list/684/ UNESCO]). Some unusual flora found here include the giant heather, and two species of forest tree, ''Hypericum bequaertii'' and ''Schefflera polysciadia'', which are only known from Rwenzori (BirdLife International 2020; [https://www.ugandawildlife.org/explore-our-parks/parks-by-name-a-z/rwenzori-mountains-national-park Uganda Wildlife Authority]). In addition, the site is home to 70 mammals and 217 bird species, including 19 Albertine Rift endemics ([https://whc.unesco.org/en/list/684/ UNESCO]; BirdLife International 2020). Twenty-five invertebrate species from the area have been described in the last 15 years (BirdLife International 2020). Mammal species of conservation concern include the Rwenzori duiker (''Cephalophus rubidus''), forest elephants (''Loxodonta cyclotis''), eastern chimpanzees (''Pan troglodytes schweinfurthii''), Ruwenzori colobus (''Colobus angolensis ruwenzorii'') and L'Hoest's monkey (''Cercopithecus l’hoesti''); subspecies of blue monkey (''Cercopithecus mitis'') and rock hyrax (''Procavia capensis'') are only known from Rwenzori Mountains National Park (BirdLife International 2020).		Located in western Uganda, Rwenzori Mountains National Park comprises part of the Rwenzori mountain chain, including Africa's third highest peak, Mt Stanley's Margherita Peak at 5,109 m above sea level ([https://whc.unesco.org/en/list/684/ UNESCO]). The park is contiguous with the Virunga National Park in the Democratic Republic of the Congo ([[#R01611\|BirdLife International 2020]]). The region's glaciers, waterfalls and lakes make it one of the most fascinating afro-alpine areas.The park is known for its rich and unique flora; some of the world's rarest vegetation can be found here ([https://whc.unesco.org/en/list/684/ UNESCO]). Some unusual flora found here include the giant heather, and two species of forest tree, ''Hypericum bequaertii'' and ''Schefflera polysciadia'', which are only known from Rwenzori ([[#R01611\|BirdLife International 2020]]; [https://www.ugandawildlife.org/explore-our-parks/parks-by-name-a-z/rwenzori-mountains-national-park Uganda Wildlife Authority]). In addition, the site is home to 70 mammals and 217 bird species, including 19 Albertine Rift endemics ([https://whc.unesco.org/en/list/684/ UNESCO]; [[#R01611\|BirdLife International 2020]]). Twenty-five invertebrate species from the area have been described in the last 15 years ([[#R01611\|BirdLife International 2020]]). Mammal species of conservation concern include the Rwenzori duiker (''Cephalophus rubidus''), forest elephants (''Loxodonta cyclotis''), eastern chimpanzees (''Pan troglodytes schweinfurthii''), Ruwenzori colobus (''Colobus angolensis ruwenzorii'') and L'Hoest's monkey (''Cercopithecus l’hoesti''); subspecies of blue monkey (''Cercopithecus mitis'') and rock hyrax (''Procavia capensis'') are only known from Rwenzori Mountains National Park ([[#R01611\|BirdLife International 2020]]).

	Henry Stanley, an explorer, placed the Rwenzori in the map in 1888; he documented "Ruwenzori" as a local name meaning “rain-maker” or “cloud-king” ([https://www.ugandawildlife.org/explore-our-parks/parks-by-name-a-z/rwenzori-mountains-national-park Uganda Wildlife Authority]). Before that, the Rwenzoris were named “Mountains of the Moon” by the Alexandrine geographer Ptolemy in AD 150 (Uganda Wildlife Authority). Much later, in 1941, the site was declared a Forest Reserve; in 1991 it was gazetted as a National Park, and in 1995 it was declared a [https://whc.unesco.org/en/list/684/ UNESCO World Heritage Site] ([https://www.ugandawildlife.org/explore-our-parks/parks-by-name-a-z/rwenzori-mountains-national-park Uganda Wildlife Authority]). The park was designated as a [https://rsis.ramsar.org/ris/1861?language=en Ramsar Site] in 2008. The Rwenzori mountains are not volcanic, as other major mountains in East Africa, but they are a block of rock up-faulted through the floor of the Western Rift Valley. The site has been long known by mountaineers. The oldest person to reach Marguerita Peak was Ms. Beryl Park, aged 78 in 2010 ([https://www.ugandawildlife.org/explore-our-parks/parks-by-name-a-z/rwenzori-mountains-national-park Uganda Wildlife Authority]).		Henry Stanley, an explorer, placed the Rwenzori in the map in 1888; he documented "Ruwenzori" as a local name meaning “rain-maker” or “cloud-king” ([https://www.ugandawildlife.org/explore-our-parks/parks-by-name-a-z/rwenzori-mountains-national-park Uganda Wildlife Authority]). Before that, the Rwenzoris were named “Mountains of the Moon” by the Alexandrine geographer Ptolemy in AD 150 (Uganda Wildlife Authority). Much later, in 1941, the site was declared a Forest Reserve; in 1991 it was gazetted as a National Park, and in 1995 it was declared a [https://whc.unesco.org/en/list/684/ UNESCO World Heritage Site] ([https://www.ugandawildlife.org/explore-our-parks/parks-by-name-a-z/rwenzori-mountains-national-park Uganda Wildlife Authority]). The park was designated as a [https://rsis.ramsar.org/ris/1861?language=en Ramsar Site] in 2008. The Rwenzori mountains are not volcanic, as other major mountains in East Africa, but they are a block of rock up-faulted through the floor of the Western Rift Valley. The site has been long known by mountaineers. The oldest person to reach Marguerita Peak was Ms. Beryl Park, aged 78 in 2010 ([https://www.ugandawildlife.org/explore-our-parks/parks-by-name-a-z/rwenzori-mountains-national-park Uganda Wildlife Authority]).
Line 72:		Line 72:
	\|Opportunistic observation		\|Opportunistic observation
	\|		\|
	\|Makombo 2017		\|[[#R01612\|Makombo 2017]]
	\|		\|
	\|		\|
Line 85:		Line 85:
	\|Line transects		\|Line transects
	\|		\|
	\|Makombo 2017		\|[[#R01612\|Makombo 2017]]
	\|		\|
	\|		\|
Line 98:		Line 98:
	\|Reconnaissance walk		\|Reconnaissance walk
	\|		\|
	\|Makombo 2017		\|[[#R01612\|Makombo 2017]]
	\|		\|
	\|		\|
Line 266:		Line 266:
	= Exposure to climate change impacts =		= Exposure to climate change impacts =

	As part of a study on the exposure of African great ape sites to climate change impacts, Kiribou et al. (2024) extracted climate data and data on projected extreme climate impact events for the site. Climatological characteristics were derived from observation-based climate data provided by the Inter-Sectoral Impact Model Intercomparison Project (ISIMIP, www.isimip.org). Parameters were calculated as the average across each 30-year period. For 1981-2010, the EWEMBI dataset from ISIMIP2a was used. For the two future periods (2021-2050 and 2071-2099) ISIMIP2b climate data based on four CMIP5 global climate models were used. For future projections, two Representative Concentration Pathways (RCP) were used. RCP 2.6 is a scenario with strong mitigation measures in which global temperatures would likely rise below 2C. RCP 6.0 is a scenario with medium emissions in which global temperatures would likely rise up to 3C by 2100. For the number of days with heavy precipitation events, the 98th percentile of all precipitation days (>1mm/d) was calculated for the 1979-2013 reference period as a threshold for a heavy precipitation event. Then, for each year, the number of days above that threshold was derived. The figures on temperature and precipitation anomaly show the deviation from the mean temperature and mean precipitation for the 1979-2013 reference period.		As part of a study on the exposure of African great ape sites to climate change impacts, [[#R02310\|Kiribou et al. (2024)]] extracted climate data and data on projected extreme climate impact events for the site. Climatological characteristics were derived from observation-based climate data provided by the Inter-Sectoral Impact Model Intercomparison Project (ISIMIP, www.isimip.org). Parameters were calculated as the average across each 30-year period. For 1981-2010, the EWEMBI dataset from ISIMIP2a was used. For the two future periods (2021-2050 and 2071-2099) ISIMIP2b climate data based on four CMIP5 global climate models were used. For future projections, two Representative Concentration Pathways (RCP) were used. RCP 2.6 is a scenario with strong mitigation measures in which global temperatures would likely rise below 2C. RCP 6.0 is a scenario with medium emissions in which global temperatures would likely rise up to 3C by 2100. For the number of days with heavy precipitation events, the 98th percentile of all precipitation days (>1mm/d) was calculated for the 1979-2013 reference period as a threshold for a heavy precipitation event. Then, for each year, the number of days above that threshold was derived. The figures on temperature and precipitation anomaly show the deviation from the mean temperature and mean precipitation for the 1979-2013 reference period.

	The estimated exposure to future extreme climate impact events (crop failure, drought, river flood, wildfire, tropical cyclone, and heatwave) is based on a published dataset by Lange et al. 2020 derived from ISIMIP2b data. The same global climate models and RCPs as described above were used. Within each 30-year period, the number of years with an extreme event and the average proportion of the site affected were calculated (Kiribou et al. 2024).		The estimated exposure to future extreme climate impact events (crop failure, drought, river flood, wildfire, tropical cyclone, and heatwave) is based on a published dataset by Lange et al. 2020 derived from ISIMIP2b data. The same global climate models and RCPs as described above were used. Within each 30-year period, the number of years with an extreme event and the average proportion of the site affected were calculated ([[#R02310\|Kiribou et al. 2024]]).

	'''Table 8. Estimated past and projected climatological characteristics in Rwenzori Mountains National Park'''		'''Table 8. Estimated past and projected climatological characteristics in Rwenzori Mountains National Park'''
Line 395:		Line 395:
	= References =		= References =

	BirdLife International. (2020). Important Bird Areas factsheet: Ruwenzori (Rwenzori) Mountains National Park. Retrieved from http://www.birdlife.org on 16/12/2020.		<span id="R01611"></span>BirdLife International. (2020). Important Bird Areas factsheet: Ruwenzori (Rwenzori) Mountains National Park. Retrieved from http://www.birdlife.org on 16/12/2020.

	Makombo, J. (2017). State of Conservation Report for Rwenzori Mountains National Park World Heritage Property –		<span id="R01612"></span>Makombo, J. (2017). State of Conservation Report for Rwenzori Mountains National Park World Heritage Property –

	Uganda. World Heritage Centre, UNESCO.		<span id="R01613"></span>Uganda. World Heritage Centre, UNESCO.

			<span id="R02310"></span>Kiribou, R., Tehoda, P., Chukwu, O., Bempah, G., Kühl, H. S., Ferreira, J., …, & Heinicke, S. (2024). Exposure of African ape sites to climate change impacts. ''PLOS Climate'', 3(2), e0000345. [https://doi.org/10.1371/journal.pclm.0000345 doi:10.1371/journal.pclm.0000345]



	'''Page created by: '''APES Atlas Team''' Date:''' 2020-12-30		'''Page created by: '''APES Atlas Team''' Date:''' 2020-12-30

WikiEdit at 12:19, 3 September 2026

2026-09-03T12:19:43Z

← Older revision		Revision as of 08:19, 3 September 2026
Line 266:		Line 266:
	= Exposure to climate change impacts =		= Exposure to climate change impacts =

	As part of a study on the exposure of African great ape sites to climate change impacts, Kiribou et al. ~~subm.~~ extracted climate data and data on projected extreme climate impact events for the site. Climatological characteristics were derived from observation-based climate data provided by the Inter-Sectoral Impact Model Intercomparison Project (ISIMIP, www.isimip.org). Parameters were calculated as the average across each 30-year period. For 1981-2010, the EWEMBI dataset from ISIMIP2a was used. For the two future periods (2021-2050 and 2071-2099) ISIMIP2b climate data based on four CMIP5 global climate models were used. For future projections, two Representative Concentration Pathways (RCP) were used. RCP 2.6 is a scenario with strong mitigation measures in which global temperatures would likely rise below 2C. RCP 6.0 is a scenario with medium emissions in which global temperatures would likely rise up to 3C by 2100. For the number of days with heavy precipitation events, the 98th percentile of all precipitation days (>1mm/d) was calculated for the 1979-2013 reference period as a threshold for a heavy precipitation event. Then, for each year, the number of days above that threshold was derived. The figures on temperature and precipitation anomaly show the deviation from the mean temperature and mean precipitation for the 1979-2013 reference period.		As part of a study on the exposure of African great ape sites to climate change impacts, Kiribou et al. (2024) extracted climate data and data on projected extreme climate impact events for the site. Climatological characteristics were derived from observation-based climate data provided by the Inter-Sectoral Impact Model Intercomparison Project (ISIMIP, www.isimip.org). Parameters were calculated as the average across each 30-year period. For 1981-2010, the EWEMBI dataset from ISIMIP2a was used. For the two future periods (2021-2050 and 2071-2099) ISIMIP2b climate data based on four CMIP5 global climate models were used. For future projections, two Representative Concentration Pathways (RCP) were used. RCP 2.6 is a scenario with strong mitigation measures in which global temperatures would likely rise below 2C. RCP 6.0 is a scenario with medium emissions in which global temperatures would likely rise up to 3C by 2100. For the number of days with heavy precipitation events, the 98th percentile of all precipitation days (>1mm/d) was calculated for the 1979-2013 reference period as a threshold for a heavy precipitation event. Then, for each year, the number of days above that threshold was derived. The figures on temperature and precipitation anomaly show the deviation from the mean temperature and mean precipitation for the 1979-2013 reference period.

	The estimated exposure to future extreme climate impact events (crop failure, drought, river flood, wildfire, tropical cyclone, and heatwave) is based on a published dataset by Lange et al. 2020 derived from ISIMIP2b data. The same global climate models and RCPs as described above were used. Within each 30-year period, the number of years with an extreme event and the average proportion of the site affected were calculated (~~see~~ Kiribou et al. ~~subm. for details~~).		The estimated exposure to future extreme climate impact events (crop failure, drought, river flood, wildfire, tropical cyclone, and heatwave) is based on a published dataset by Lange et al. 2020 derived from ISIMIP2b data. The same global climate models and RCPs as described above were used. Within each 30-year period, the number of years with an extreme event and the average proportion of the site affected were calculated (Kiribou et al. 2024).

	'''Table 8. Estimated past and projected climatological characteristics in Rwenzori Mountains National Park'''		'''Table 8. Estimated past and projected climatological characteristics in Rwenzori Mountains National Park'''

WikiEdit at 14:50, 1 September 2026

2026-09-01T14:50:14Z

← Older revision		Revision as of 10:50, 1 September 2026
Line 64:		Line 64:
	\|-		\|-
	\|''Pan troglodytes schweinfurthii''		\|''Pan troglodytes schweinfurthii''
	\|~~2010~~		\|2016
			\|
	\|		\|
	\|		\|
	\|~~0.385~~		\|231.0
	~~\|384~~.0
	\|Rwenzori Mountains National Park		\|Rwenzori Mountains National Park
	\|~~Line transects~~		\|Opportunistic observation
	\|		\|
	\|Makombo 2017		\|Makombo 2017
Line 77:		Line 77:
	\|-		\|-
	\|''Pan troglodytes schweinfurthii''		\|''Pan troglodytes schweinfurthii''
	\|~~2000~~		\|2010
	\|		\|
	\|		\|
	\|0.~~506~~		\|0.385
	\|~~500~~.0		\|384.0
	\|Rwenzori Mountains National Park		\|Rwenzori Mountains National Park
	\|~~Reconnaissance walk~~		\|Line transects
	\|		\|
	\|Makombo 2017		\|Makombo 2017
Line 90:		Line 90:
	\|-		\|-
	\|''Pan troglodytes schweinfurthii''		\|''Pan troglodytes schweinfurthii''
	\|~~2016~~		\|2000
	\|		\|
	\|		\|
	\|		\|0.506
	\|~~231~~.0		\|500.0
	\|Rwenzori Mountains National Park		\|Rwenzori Mountains National Park
	\|~~Opportunistic observation~~		\|Reconnaissance walk
	\|		\|
	\|Makombo 2017		\|Makombo 2017

WikiEdit at 09:46, 14 July 2026

2026-07-14T09:46:57Z

← Older revision		Revision as of 05:46, 14 July 2026
Line 77:		Line 77:
	\|-		\|-
	\|''Pan troglodytes schweinfurthii''		\|''Pan troglodytes schweinfurthii''
	\|~~2016~~		\|2000
	\|		\|
	\|		\|
	\|		\|0.506
	\|~~231~~.0		\|500.0
	\|Rwenzori Mountains National Park		\|Rwenzori Mountains National Park
	\|~~Opportunistic observation~~		\|Reconnaissance walk
	\|		\|
	\|Makombo 2017		\|Makombo 2017
Line 90:		Line 90:
	\|-		\|-
	\|''Pan troglodytes schweinfurthii''		\|''Pan troglodytes schweinfurthii''
	\|~~2000~~		\|2016
			\|
	\|		\|
	\|		\|
	\|~~0.506~~		\|231.0
	~~\|500~~.0
	\|Rwenzori Mountains National Park		\|Rwenzori Mountains National Park
	\|~~Reconnaissance walk~~		\|Opportunistic observation
	\|		\|
	\|Makombo 2017		\|Makombo 2017

WikiEdit at 14:48, 25 March 2026

2026-03-25T14:48:31Z

← Older revision		Revision as of 10:48, 25 March 2026
Line 13:		Line 13:
	* Key threats to chimpanzees are illegal logging, bushmeat hunting, and illegal resource harvesting.		* Key threats to chimpanzees are illegal logging, bushmeat hunting, and illegal resource harvesting.
	* Conservation activities implemented include conducting anti-poaching patrols.		* Conservation activities implemented include conducting anti-poaching patrols.

WikiEdit at 07:31, 4 February 2026

2026-02-04T07:31:18Z

← Older revision		Revision as of 03:31, 4 February 2026
Line 164:		Line 164:
	\|The site was designated as a National Park in 1991.		\|The site was designated as a National Park in 1991.
	\|		\|
	\|1991-Ongoing (~~2020~~)		\|1991-Ongoing (2026)
	\|}		\|}

WikiEdit at 07:10, 6 November 2025

2025-11-06T07:10:36Z

← Older revision		Revision as of 03:10, 6 November 2025
Line 387:		Line 387:


	<div><ul><li style="display: inline-block; vertical-align: top;"> [[File:PrecipAnomaly_Rwenzori_Mountains_NP.png\| 450px \| thumb\| none \| Precipitation anomaly ~~inRwenzori~~ Mountains National Park]] </li><li style="display: inline-block; vertical-align: top;"> [[File:TempAnomaly_Rwenzori_Mountains_NP.png \| 450px \| thumb\| none \| Temperature anomaly ~~inRwenzori~~ Mountains National Park]] </li></ul></div>		<div><ul><li style="display: inline-block; vertical-align: top;"> [[File:PrecipAnomaly_Rwenzori_Mountains_NP.png\| 450px \| thumb\| none \| Precipitation anomaly in Rwenzori Mountains National Park]] </li><li style="display: inline-block; vertical-align: top;"> [[File:TempAnomaly_Rwenzori_Mountains_NP.png \| 450px \| thumb\| none \| Temperature anomaly in Rwenzori Mountains National Park]] </li></ul></div>

	= External links =		= External links =