Cape Buffalo, Bison and Water

By Bianca T. Esposito, NWNL Research Intern
(Edited by Alison M.  Jones, NWNL Director)

NWNL research intern Bianca T. Esposito is a senior at Syracuse University studying Biology and minoring in Economics. Her research this summer is on the intertwined relationships of biodiversity and our water resources. This is Bianca’s second blog on Biodiversity for NWNL. Read her first blog on wild Salmon here.

This blog compares how water impacts the health of sub-Sahara’s Cape buffalo populations to how North America’s bison impact the health of our water resources.  This investigation covers three of our NWNL case study watersheds: Africa’s Mara and Nile River Basins, and North America’s Mississippi River Basin.

The Cape buffalo (Syncerus caffer caffer) is found in Kenya’s Mara River Basin savanna and Uganda’s Nile River Basin plains. The bison (Bison bison) used to dominate the Mississippi River Basin’s Great Plains and are still there in scattered small populations. Both species are large, herbivorous mammals that primarily graze on tall-grass ecosystems. However, their habitats and connections to water differ significantly.

Africa’s Cape buffalo migrate seasonally in large herds on cyclical routes dependent on fluctuations in water availability. They move out of areas with limited resources and into areas where moisture and nutrients are available. Cape buffalo also migrate away from their habitat when water levels increase, since flooding restricts their foraging abilities. In these cases, Cape buffalo move to a drier habitat where, in turn, they may experience drought. Either way, when resources become low, their vulnerability becomes high.

Jones_090927_K_9062.jpgA lone Cape Buffalo bull in Kenya’s Mara Conservancy (© Alison M. Jones)

Africa’s famed Serengeti-Mara Ecosystem is located throughout northern Tanzania and extends into Kenya. Much of this region is situated within the Mara River Basin. In the Serengeti National Park, the migration pattern of the Cape buffalo, similar to that of the wildebeest-zebra migration, is dependent on the fluctuation of rainfall each year. Generally, this journey begins in April when Cape buffalo depart their southern plains habitat to head north. This movement is triggered by the onset of heavy rain that floods the plains, reducing the Cape buffalo’s ability to graze. By May the herd is in the northwest Serengeti, where the dry season lasts through July and proximity to the equator allows rainfall to be more evenly distributed, allowing greater opportunities for foraging. Then, in August, the late dry season hits, causing the herd to move further north. On their venture north, they cross the Mara River into Kenya’s Maasai Mara National Reserve. The Cape buffalo remain here enjoying green pastures until November, albeit subject to drought if there’s no rainfall. In December, usually the first rainfall comes which they sense as the onset of the rainy season. They then trek back into Tanzania’s southern plains for the wet season. From January to April, they graze there on plentiful, nutritious grasses.  

Syncerus-caffer-Masaai-Mara-Kenya.JPGHerd of Cape buffalo in Kenya’s Mara Conservancy (Creative Commons)

When Cape buffalo inhabit dry lands their reproductive success (also referred to as “recruitment ability”) decreases; but their body condition improves due to what seems to be a fat-storing mechanism that anticipates limited future resources. One benefit of Cape buffalo having to cope with drought is that when food supplies are reduced, they forage through peat layers in dried-up underground channels, releasing nutrients otherwise trapped below ground.

A current major concern for this species is that anthropogenic factors (human activity) causing climate change are expected to increase both water levels and drought, which could push the Cape buffalo outside of their protected areas. In 2017, the Serengeti experienced a drought that lasted over a year causing declines in populations of many species, including Cape buffalo. Drought also causes herds of cattle, goats and sheep outside to enter protected lands to graze, creating a competition for resources between wildlife, livestock and humans in both the Maasai Mara National Reserve and Serengeti National Park. If the Mara River – the only major river in the area – dries up, there would be few resources for ungulates. As well, when droughts end, there is always potential for flash-floods which deter herds from crossing rivers to find greener pastures.

Jones_120107_K_0640.jpgA lone Cape Buffalo bull in Kenya (© Alison M. Jones)

When water is scarce in the Serengeti, a decline of Cape buffalo leads to increased lion mortality. When Cape buffalo lack sufficient food due to drought, they become weak and must travel increased distances to quench their thirst. This leaves the herd fatigued, causing some members to fall behind and thus become more vulnerable to predation. Also, after a drought and the rains begin, Babesia-carrying ticks infect Cape buffalo. Infected buffalo become weak or die, allowing easy predation by lions. Unfortunately, their carcasses transfer babesiosis disease to lions. Alone, this disease is not fatal to the lion. However, babesiosis coupled with canine distemper virus (CDV) is lethal.

Babesiosis from Cape buffalo has caused two major declines in Serengeti lion populations. In 1994, a third of the lion population was lost due to this combination, killing over 1,000 lions.

Lions_taking_down_cape_buffalo.jpgLions taking down a Cape buffalo (Creative Commons)

On a smaller scale, in 2001 the Ngorongoro Crater lion population also lost about 100 lions due to this synchronization of disease. Craig Packer, a University of Minnesota biologist, stated, “Should drought occur in the future at the same time as lions are exposed to masses of Babesia-carrying ticks—and there is a synchronous CDV epidemic–lions will once again suffer very high mortality.” He also warns that extreme weather due to climate change puts species at greater risk to diseases not considered a major threat before.  Fortunately, mud-wallowing that Cape buffalo use to cool down their bodies is also an effective shield against infiltrating bugs and ticks once the mud dries.

Overall, Cape buffalo rely heavily on rainfall patterns; but climate change is disrupting traditional migratory patterns by raising water levels or causing drought. Both extremes present negative impacts to the Mara River Basin and the biodiversity that inhabits it.  

North America’s bison – a bovine counterpart to African Cape buffalo – historically occupied The Great Plains west of the Mississippi River. Early settlers recorded 10 to 60 million bison openly roaming the fields. Like Cape buffalo, bison also migrate in search of food. Their migration paths used to cover vast territory, thus paving the way for many current roads and railroads. A major threat to  bison – as with most species – has been habitat loss due to human infringement, as well as well-documented, extensive hunting by new settlers heading west. By 1889, only approximately 1,000 bison remained in North America.

Jones_121024_TX_6814.jpgFarmed bison in Texas (© Alison M. Jones)

Due to recent conservation efforts, bison populations are rising; however, not to past numbers. Currently, they are found only in National Parks, refuges and farms. As of 2017, approximately 31,000 pure wild bison remain in 68 conservation herds. “Pure wild bison” are those not bred with cattle for domestication. However, only approximately 18,000 of the remaining population “function” as wild bison. This count excludes very small bison herds used for research, education and public viewing – or bison held in captivity waiting to be culled by protected areas such as Yellowstone National Park due to required limits.

Bison inhabiting the Mississippi River Basin, which drains throughout the Great Plains, have many positive impacts on its waterways and tributaries. Yellowstone Park, where the Yellowstone River drains into the Missouri-Mississippi River system, is the only place in North America where bison continue to freely roam as they used to. In Yellowstone, bison occupy the central and northern area of the park where they migrate by elevation, seasonally choosing food according to abundance, rather than quality. In the winter, they select lower elevations near thermal hot springs or rivers where there is less snow accumulation.

Bison positively affect water supplies when they wallow and paw at the ground. This results in intense soil compaction that creates soil depressions in grasslands. After many years, this soil depression tends to erode since bison don’t like to wallow on previously-created depressions. However, during the rainy season, wetland plants and vegetation grow in these wallows created by bison dust-bathing and trampling. For a short time many species enjoy these ephemeral pool habitats before they disappear in droughts or floods. Meanwhile bison wallows increase species diversity that would otherwise not be present in grasslands.

A_bison_wallow_is_a_shallow_depression_in_the_soil.jpgBison rolling around in a dry wallow (Creative Commons)

Bison have other positive impacts on water. As they trample through streams, they widen available habitat and alter water quality. Even after a bison dies, it can still contribute to the health of its ecosystem. Their carcasses are a nutritious food source for wolves, coyotes and crows. Studies suggest that bison carcasses take roughly seven years to fully decompose, during which time their remains release nutrients such as phosphorus and carbon into rivers. These nutrients sustain microbes, insects, fish and large scavengers of the area. A bison carcass can also provide sustenance for local fish since maggots, green algae and bacteria grow over their bones during decomposition. Bison carcasses also deposit nutrients into the soil which fertilizes plant regrowth.

Bison can negatively affect water resources, by decreasing native plant diversity due to overgrazing. However, they graze on only grass, which allows forbs (non-woody flowering plants) to flourish, adding biodiversity in grasslands. As well, when bison urinate, they deposit nitrogen into the soil, a key nutrient for grass growth and survival. Their urine also becomes a selectable marker allowing them to return to formerly-grazed pastures during the season. This constant reselection of grassland, allows combustion in ignored, non-grazed pastures, since fire tends to occur in tall grass with nitrogen loss. After fires, the bison are attracted to newly-burned watersheds because of C4-dominated grass which grows in dry environments. Bison select C4-dominated grassy areas because they have low plant diversity, unlike less-frequently burned sites where forbs are abundant. Thus, bison’s pasture preferences allow for more biodiversity, creating healthier watersheds.  

Jones_121024_TX_7314.jpgMural near of Native Americans on bison near Masterson, Texas (© Alison M. Jones)

Each of these two similar bovine species have significant, but different, relationships to water availability and quality within their river basins.  The African Cape buffalo migration is guided by water fluctuations. This could impact their future since anthropogenically-caused climate change could incur longer and more frequent droughts and increased flood-water levels to an extent that would drive Cape buffalo out of their protected habitats. In contrast, North American bison herds improve the health of waterways in the Mississippi River Basin in several ways. Nutrients from their decomposing carcasses add to the health of tributary streams and rivers; and their mud wallows support greater diversity of wetland and grassland flora.

Whether we look at watersheds in Africa or North America, it is clear that it is as important to study how biodiversity is affected by water availability, as how watershed water quality and quantity affects its biodiversity. Any changes to these ecosystems due to climate change could drastically affect the biodiversity and health of these watersheds.

Bibliography:

Briske, David. Springer Series on Environmental Management, accessed June 19, 2018, via link.
van Wyk, Pieter. MalaMala Game Reserve Blog, accessed on June 19, 2018, via link.
Bennitt, Emily. Journal of Mammalogy, accessed on June 19, 2018, via link.
Wilcox, Bradford. Springer Series on Environmental Management, accessed June 19, 2018, via link.
Chardonnet, Philippe. Gnusletter, accessed on June 19, 2018, via link.
Defenders of Wildlife, accessed on June 20, 2018, via link.
Coppedge, Bryan R.
The American Midland Naturalist, accessed on June 20, 2018, via link.
Polley, H. Wayne.
The Southwestern Naturalist, accessed on June 20, 2018, via link.
Crow, Diana.
Smithsonian, accessed on June 20, 2018, via link.
Knapp, Alan K.
American Institute of Biological Sciences, accessed on June 20, 2018, via link.
North Arizona University, accessed on June 25, 2018, via link.Dybas, Cheryl Lyn.
BioScience, accessed on June 25, 2018, via link.
Water Resources and Energy Management (WREM) International Inc., accessed on June 25, 2018, via link.
Defenders of Wildlife, accessed on June 26, 2018, via link.
Yellowstone National Park, accessed on June 26, 2018, via link.
Huffman, Brent. Ultimate Ungulate, accessed on June 26, 2018, via link.
Department of Primary Industries, accessed on July 9, 2018, via link.
Popescu, Adam. New Scientist, accessed on July 9, 2018, via link.
Hoagland, Mahlon B. Exploring the Way Life Works: The Science of Biology, accessed on July 9, 2018E, via link.
White, PJ. Yellowstone Association, accessed on July 9, 2018, via link.

Buzz Numbers

By NWNL Director, Alison Jones

As NWNL plans its website redo (to launch this fall), we envision “Buzz Numbers” on the home page.  What?  Well, “Buzz Numbers,” are our Project Manager Sarah’s take-off on “buzz words.”  Just another great tool to quickly project complex concepts.  So, while in that mode, here’s a NWNL BLOG with 0 references to specific watersheds and just 1 URL link. The Buzz Numbers below refer to values of, or impacts on, all rivers and streams in the Americas or East Africa, the 2 regions where NWNL case-study watersheds are located.

Jones_160319_CA_1544.jpgDrought in California, 2016

BUZZ NUMBERS for The Americas

  • 13%: The Americas’ share of world’s human population
  • >50%: Share of Americans with a water security problem
  • 50%: Decrease in renewable freshwater available per person since 1960s
  • 200-300%: Increase in human ecological footprint since 1960s
  • >95%: Tall grass prairies lost to human activity since pre-European settlement
  • >50%: US wetlands lost (90% in agricultural regions) since European settlement
  • 15–60%: American drylands habitat lost between 2000 and 2009
  • 5 million hectares [3.7 million acres]: Great Plains grassland lost from 2014 to 2015
  • $24.3 trillion: terrestrial nature’s annual economic contribution (=GDP)
    Jones_080530_WY_1866.jpgGrey Wolf in Yellowstone National Park, 2008

Projections for 2050 in the Americas

  • 20%: expected population increase (to 1.2 billion) by 2050
  • +/-100%: expected growth in GDP by 2050, driving biodiversity loss if ‘business as usual’ continues
  • 40%: loss of biodiversity expected by 2050 if climate change continues
———-
Jones_040828_ET_0050.jpgVillagers in Lalibela, Ethiopia with erosion in foreground, 2004

BUZZ NUMBER Trends / Data for Africa

  • +/- 500,000: km2 [123 million acres] degraded by deforestation, unsustainable agriculture, overgrazing, uncontrolled mining activities, invasive alien species and climate change – causing soil erosion, salinization, pollution, and loss of vegetation or soil fertility
  • +/- 62%: rural population using wild nature for survival (the most of any continent)
  • +/- 2 million km2 [494 million acres]: land designated as protected
  • 25%: Sub-Saharans suffering hunger and malnutrition (2011–2013) in the world’s most food-deficient region
Jones_130118_K_1688.jpgCommercial fisherman preparing to sell in Nairobi, 2013

Economic Values of Nature’s Contributions East Africans

  • $1.2 billion: annual inland fishery value added
  • $16,000: annual food production per km2 [247 acres
  • $12,000: annual forest carbon sequestration per km2 (247 acres])
  • $11,000: annual erosion control per km2 [247 acres]

All our Buzz Number stats come from the Appendix of an ISPBES Intergovernmental Science-Policy Platform on Biodiversity and Ecosystem Services March 2018 Report, sponsored by UN

Jones_120125_K_5464.jpgWoman collecting water from spring in Mau Forest, Kenya, 2012

 

All photos © Alison M. Jones.

What We’re Reading #1

Introducing a new semi-regular blog series: What We’re Reading!  For two months this winter, our NWNL Director Alison Jones was in Kenya. Among the many interviews and trips to the Omo and Mara River Basins, Alison was also busy reading during this expedition. The goal of this new blog series is to share the books NWNL reads and give you ideas of books to read about our watersheds!

Ruaha National Park: An Intimate View

ruahanationalpark.jpgWritten by Alison’s new acquaintance Sue Stolberger, this is the first field guide to trees, flowers and small creatures found in Ruaha National Park, and surrounding Central Tanzania. While not part of one of NWNL’s watersheds, flora and fauna within Ruaha National Park are very similar to that of Tanzania’s Serengeti National Park that is within the Mara River Basin.

 

 

 

 

 

Rivergods: Exploring the World’s Great Wild Riversrivergods.jpg

In this wonderfully photographed book, Richard Bangs & Christian Kallen raft down rivers across the globe. The first chapter covers the Omo River in Ethiopia, one of NWNL’s case-study watersheds, which the book calls the “River of Life.”

 

 

 

 

Ethiopia: The Living Churches of an Ancient Kingdom

livingchurches.jpg

Nigel Pavitt, an informal advisor to NWNL on the Nile and Omo River Basins and Carol Beckwith a friend of NWNL Director Alison Jones are two of the photographers for this stunning large-format book tracing art, culture, ecclesiastical history and legend in Ethiopia’s Blue Nile River Basin.

 

 

 

 

 

 

Web Design: Make Your Website a Success

webdesign.jpg

Finally, NWNL would like to make a special announcement:  we are re-designing our website!  In preparation for that,  Alison  read a helpful book by Sean McManus on easy steps to designing websites. Simultaneously, a team of experts were working with our Project Manager in our NYC office, so the process is already underway.  By the end of summer we will unveil our new website!

Day Zero – A Water Warning

By Stephanie Sheng for No Water No Life (NWNL)
Edited by NWNL Director, Alison Jones

Stephanie Sheng is a passionate strategist for environmental and cultural conservation. Having worked in private and commercial sectors, she now uses her branding and communications expertise to drive behavior change that will help protect our natural resources. Inspired by conservation photographers, The Part We Play is her current project.  Her goal is to find how best to engage people and encourage them to take action. 

Misc-Pollution.jpg

I was horrified when I first heard the news from South Africa of Cape Town’s water crisis and impending ‘Day Zero’ – the day their taps would run dry. Originally forecasted for April 16, then pushed out to May, the apocalyptic-sounding day has now successfully been pushed out to next year. Had Day Zero remained slated for April or May, Cape Town would have been the first major city to run out of water. Although postponed, the threat still remains, and thus restrictions on water usage to 13.2 gallons (50 liters) per day for residents and visitors. Water rationing and a newly-heightened awareness around water use is now the new, legally-enforced normal in Cape Town.

Two things struck me as I read about this situation. First, the seemingly unthinkable felt very close. My visit to Cape Town a few years ago reminded me of San Francisco, my home before New York. Suddenly I was reading that this seemingly-similar city was on the brink of having no water coming out of their taps. As that hit me, I considered what modern, urban life would be like when water is scarce.

ClimateChange-ColumbiaBC.jpgCape Town’s restriction of 13.2 gal (50 L) per day is miniscule in comparison to the 39.6 gal (150 L) per day used by the average UK consumer[1] and the 79.3 to 99 gal (300 to 375 L) per day used by the average US consumer.[2] Unsurprisingly, Cape Town had to undergo drastic changes. It is now illegal to wash a car or fill a swimming pool. Hotel televisions blare messages to guests to take short 90-second showers. Washroom taps are shut off in restaurants and bars. Signs around bathroom stalls say, “If it’s yellow, let it mellow.” Hand sanitizer is now the normal method of hand cleaning.WASH-Tanzania.jpgShocked by the harsh realities of what water shortage could look like here at home, I was inspired to walk through my day comparing my water habits to the new realities being faced by those in the Cape Town facing a severe crisis. I wanted to discover opportunities where I could cut back, even though I consider myself on the more conscious end of the usage spectrum.

Here is a breakdown of my average water usage per day while living and working in NY, based on faucets spewing 2.6 gal (10 L) per minute[3], and a toilet flush using 2.3 gal (9L).[4]

  • Faucet use for brushing teeth and washing face for 4 min/day: 6 gal (40L)
  • Faucet use for dish washing and rinsing food for 7 min/day:5 gal (70L)
  • Toilet flushes, 4/day: 5 gal (36 L)
  • Drinking water: 4 gal (1.5 L)
  • Showering for 9 min/day — 8 gal (90 L)

My water usage totaled roughly 62.8 gal (237.5 L) per day. That is lower than the average American’s usage, but still more than four times the new water rations for Capetonians!

Misc-NYC.jpg

Living in an urban city that isn’t facing an impending water shortage, it may be more difficult to control certain uses than others (e.g. not flushing the toilet at work). However, there are some simple, yet significant ways to lower our daily water use:

  • Turn off the faucet while you brush your teeth and wash your face.
  • Use the dishwasher instead of washing dishes by hand. Only run it when full.
  • Only run the laundry with full loads.
  • When showering, shut off the water while you soap up and shave. Put a time in your shower to remind you not to linger.
  • Recycle water when possible. If you need to wait for hot water from the faucet, capture the cold water and use it for pets, plants, hand washing clothes, and such.

VWC-Beef.jpg

Water use discussed thus far includes obvious personal contributors to our water footprint. But the biggest contributor is actually our diet. Agriculture accounts for roughly 80% of the world’s freshwater consumption[5]. Different foods vary greatly in the amount of water consumed in their growth and production. Meat, especially from livestock with long life cycles, contains a high “virtural water” content per serving. For example, 792.5 gal (3,000 L) of water are required for a ⅓ lb. beef burger[6] – representing four times as much water as required for the same amount of chicken. That virtual water content ratio is even greater when red meat is compared to vegetables.

We don’t have to become vegetarians, but we can cut down on meat and choose meats other than beef and lamb. That change alone would save hundreds of thousands of gallons (or liters) consumed in a year, which is much greater than the 18,069.4 gal (68,400 L) I’d save by reducing my current water usage to that of a Capetonian. Consideration of virtual water content offers some food for thought!

Sources

[1] BBC News
[2] United States Geological Survey
[3] US Green Building Council: Water Reduction Use
[4] US Green Building Council: Water Reduction Use
[5] Food Matters Environment Reports
[6] National Geographic
All images/”hydrographics” are © Alison Jones, No Water No Life®.
For more “hydrographics” visit our
website.

World Wetlands Day 2018

World Wetlands Day – February 2, 2018
blog by Sarah Kearns, NWNL Project Manager

BOT-OK-107.jpgOkavango Delta, Botswana, Africa

What are “wetlands”?

Synonyms: Marsh, fen, bog, pothole, mire, swamp, bottomlands, pond, wet meadows, muskeg, slough, floodplains, river overflow, mudflats, saltmarsh, sea grass beds, estuaries, and mangroves.

Jones_070605_BC_1624.jpgDevelopment on edge of Columbia Wetlands, British Columbia

Worldwide, wetlands regulate floods, filter water, recharge aquifers, provide habitat, store carbon, and inspire photographers & artists.

Jones_111024_LA_8655.jpgCyprus trees in Atchafalaya River Basin Wetlands, Louisiana

Wetlands control rain, snowmelt, and floodwater releases: mitigation that is more effective and less costly than man-made dams. Nearly 2 billion people live with high flood risk – This will increase as wetlands are lost or degraded.

Jones_091004_TZ_2124.jpgFishing boats among invasive water hyacinth in Lake Victoria, Tanzania

Wetlands absorb nitrogen and phosphorous which provides cleaner water downstream for drink water supplies, aquifers and reservoirs.

Jones_091002_TZ_1209.jpgWoman collecting water in Maseru Swamp, Tanzania

Wetlands absorb heat by day and release is at night, moderating local climates.

Jones_111021_LA_2490.jpgRed-earred turtles in Bluebonnet Swamp, Baton Rouge, Louisiana

We all need the clean air, water, and protection from flooding that wetland forests provide. But up to 80% of wetland forests in the US South have disappeared. What are our standing wetland forests worth? Let’s be sure we invest in our wetland forests. (From dogwoodalliance.org)  Worldwide, we must protect our wetlands.

Jones_150817_AZ_5849.jpgSouthern tip of Lake Havasu and incoming Williams River and its wetlands, Arizona

To learn more about World Wetlands day visit http://www.worldwetlandsday.org.

All photos © Alison M. Jones.

 

Amboseli Wetlands

by Pongpol Adireksarn for No Water No Life
Edited by Alison Jones, NWNL Director

Amboseli Wetlands 1.jpg

Kilimanjaro is Africa’s highest and most well-known mountain. The Maasai call it “Ol Dolnyo Oibor” (The White Mountain) because of its snow-capped top, a symbolic landmark for centuries. Besides being picturesque, Kilimanjaro has lived up to its reputation as “The Life-giving Mountain.” It has provided water for millions of wildlife, people and their livestock in a semi-desert area with less than 340 mm [13.3 in] of rainfall annually. Amboseli National Park, a popular Kenyan safari destination, lies below the lower northern shoulders of this “Rooftop of Africa.”

In 1991 an effort began to conserve the biodiversity of Amboseli; support development of local human populations; and improve the park’s infrastructure. UNESCO and the Government of Kenya designated Amboseli National Park and its surrounding area as a “Man and the Biosphere Reserve.”

[Editor’s Note: The Man and the Biosphere Programme is an intergovernmental, scientific program launched in 1971 by UNESCO. Using science, education and economics, this program establishes benefits to human communities while safeguarding surrounding ecosystems and wildlife. Its World Network of Biosphere Reserves currently counts 669 sites in 120 countries]

Amboseli Elephant 1.jpg

On a 2005 visit to Amboseli, I saw the toll climate change is taking on Kilimanjaro: the alarming sight of less snow on the mountaintop. My most recent visit in October 2017 was disheartening. From a distance I saw only a small area of snow remaining on top of Kilimanjaro. I recalled the assessment that Kilimanjaro has lost 80 % of its snow cover since 1912; and that by 2033 the snows of Kilimanjaro would no longer exist.

Amboseli Great White Pelican.jpg

I drove deeper into the park, remembering that 12 years ago I saw a mirage of water everywhere I looked. However the mirage I saw on this drive started to disappear. Instead, what I saw before me were wide wetlands filled with water on both sides of the road. As I continued on, there were bulldozers and heavy equipment dredging these wetlands and laying large concrete pipes on both sides of the road. My local guide explained that the park is expanding the wetlands by filling existing swamps with more of the water that flows down from Kilimanjaro via underground channels.

Amboseli Elephant 3.jpg

This development fulfills the objectives set for Amboseli National Park by the Man and the Biosphere Programme. In a land of world-famous elephant matriarchs, this program is creating biodiversity havens to benefit wildlife in the immediate area of the park, while also supporting Maasai and their livestock living near the park.

Amboseli Hippo 1.jpg

The next morning, passing through an arid area with Kilimanjaro in the background, I saw a large herd of elephants walking towards the wetlands to drink and bathe. An hour later as I went closer to a wetlands, I saw several elephants and ungulates enjoying their time in the swamp. More wildlife arrived at the wetlands as the day continued. A family of hippopotamus occasionally left the swamp to graze, Hundreds of great white pelicans, winter migrants from Eastern Europe, were enjoying pleasant weather on an island in the swamp under sunny skies.

Amboseli Elephant 4.jpg

My local guide took me to Observation Hill, overlooking the vast Amboseli wetlands. As we walked up the hill, I noticed two large signs put up by International Fund for Animal Welfare (IFAW) and Kenya Wildlife Service (KWS). One sign coined two apt phrases, “Kilimanjaro, The Life-Giving Mountain,” and “Without Kilimanjaro, Many Lives would Cease!” The other sign read, “Where Life Springs Up In A Desert.” Addressing national – and indeed global – issues, it noted, “While many wetlands in Kenya dwindle and lose biodiversity because of destructive and unchecked human activities, this protected oasis will remain a source of life. Only if man does not adversely affect it.”

 

Pongpol Adireksarn was born in Bangkok, Thailand, and received a Bachelor Degree in International Relations from Lehigh University, USA, and a Master Degree in the same field from American University, USA. Elected four times as a Member of Parliament from Saraburi Province, he was appointed Minister of Foreign Affairs, Minister of Tourism and Sports, Minister of Agriculture and Cooperatives, Minister of Education, and Deputy Prime Minister. Pongpol wrote several novels in Thai and English using his real name and the pen name “Paul Adirex”.  In the past nine years, Pongpol has been producer and host of a television documentary program on world heritage sites which has led him to many national parks and wildlife reserves all over the world, prompting him to become seriously interested in wildlife threatened species.
All photos © Pongpol Adireksarn.

Seeking Nile River Origins via its Tributaries

By Joannah Otis for No Water No Life

This is the third blog on the Nile River in Egypt by NWNL Researcher Joannah Otis, sophomore at Georgetown University. This essay addresses the sources of the Nile  – lakes, tributaries, and a great swamp. [NWNL has completed documentary expeditions to the White and Blue Nile Rivers, but due to current challenges for photojournalists in Egypt and Sudan, NWNL is using literary and online resources to investigate the main stem of the Nile.]

For centuries, the debate over the source of the Nile River incited explorations and evoked endless questions. The Ancient Egyptians believed that the Nile originated from an underground sea or spring, but never ventured upriver to confirm their theory.  Instead they put their faith in Hapi, god of the Nile River.1 [See NWNL Blog “Finding Hapi-ness on the Nile,” .]

1000px-River_Nile_map.svgMap of the Nile River and its sources. (Attribution: Hel-Hama)

Interest in the elusive source arose again c. 440 BCE when Herodotus wrote in The Histories of the “fountains of the Nile.”  He asserted that melting snow from upstream mountains flooded the headwaters to create the seasonal inundation.2  It was not until 1768 when James Bruce began searching for and ultimately found the source of the Blue Nile at Lake Tana in the Ethiopian Highlands that some light was shed on the issue.  

In 1874, Henry Morton Stanley confirmed an earlier theory by John Hanning Speke that Lake Victoria was the source of the White Nile. These explorers and many others were often sponsored by the Royal Geographical Society in England and driven by their own hopes for fame.3 Today’s satellite technology and advanced resources have enabled us to positively identify Lake Tana as the source of the Blue Nile and Lake Victoria as the source of the White Nile. These two main rivers meet in Khartoum, Egypt to form the great Nile River.

ET Bar 0125D.JPGTissiat Falls, from L. Tana, source  of the Blue Nile.  (© Alison M. Jones)

The Blue Nile is the source of about 85% of the Nile’s water.4 Beginning in the Ethiopian Highlands where a plateau of basalt lava receives rain from seasonal monsoons from May to October, the Blue Nile stretches over 900 miles into Sudan. This origin point lies 2,500 meters above sea level.  Beginning its northbound route, this river flows through Lake Tana, as well as the Blue Nile Gorge.5 Lake Tana is a shallow body of water measuring 1,400 square miles, surrounded by the Amhara tribe’s ancestral lands.6 The Blue Nile Gorge, lying on the edge of Africa’s Great Rift Valley, guides the Blue Nile for 370 miles into the middle of the Ethiopian Highlands.7

While the White Nile contributes only 15% of the Nile River’s water, it is still an important ecological and hydrological presence.8 Originating in Lake Victoria and fed by the Ruvubu, Nyabarongo, Mara and other rivers, the White Nile flows through Lake Kyoga, Lake Albert, and the Sudd.9 The White Nile flows through much of the Albertine Rift Region.  It spans from the northernmost point of Uganda’s Lake Albert to the southern tip of Lake Tanganyika.10  This rift is home to a plethora of diverse wildlife, including 5,793 plant species, which brings profitable tourism to Uganda. Between Juba, Ethiopia and Khartoum, the river in Sudan drops just 75 meters. To the east and west of the river, the floodplains become savannah and then desert as lush growth that adorns the Nile’s banks disappears.11

White_Nile_Bridge,_Omdurman_to_Khartoum,_SudanThe White Nile Bridge in Sudan. (Attribution: David Stanley)

Just south of Khartoum, lies the vast Sudd, covering most of  South Sudan. Meaning ‘obstacle’ in Arabic. the Sudd is one of the world’s largest wetlands and the Nile Basin’s largest freshwater wetland.  The Sudd is a 12,355 square-mile practically impenetrable swamp of complex channels and lagoons –  an explorer’s challenge.  Fed by heavy rainfall from April to October,12 it provides floodwater storage and water habitat for 350 plant species, 470 migratory bird species, and 100 fish species.  Antelope migrations from the surrounding arid Sahel retreat annually to the Sudd in astonishing numbers.  Around 1.2 million white-eared kob, Nile Lechwe, and tiang, as well as wild dogs, crocodiles and hippos in the Sudd are best viewed by air.   The Sudd is also the home to pastoralist Nuer, Dinka and Shilluk tribes, Nilotic peoples who practice subsistence semi-nomadic cattle breeding and some grain farming.

Jones_040826_ET_0160Lake Tana, Ethiopia’s source of the Blue Nile. (© Alison M. Jones)

Ecosystems within the swamp include open waters with submerged vegetation, floodplain shrubland, surface-floating fringe vegetation, seasonally flooded grassland and woodland.13 Since most of the water that enters the Sudd evaporates due to high temperatures in Sudan, the White Nile leaves this swamp with half the power with which it enters.14  Since the 1930’s, there’ve been proposals to build a canal, today referred to as the Jonglei Canal Project, east out of the Sudd directly to the main stem of the Nile River.  It is said such a canal could increase Egypt’s water supply by five to seven percent. While Sudan and Egypt would benefit, South Sudan would see its fisheries die, grazing lands dry out and groundwater lowered.

Uganda:Lake Victoria, Uganda’s source of the White Nile. (© Alison M. Jones)

After years of searching, the sources of the Blue and White Nile River are no longer mysteries. The number of plant and animal species who depend on them are staggering, but they also serve as important lifelines for the humans living on their banks. From water for irrigation to water for domestic use, the Nile River tributaries are vital to North African survival of all species, including humans. It would be a human and environmental tragedy if these Nile tributaries or the great Sudd were drained and disappeared, as has Africa’s Lake Chad. Thus, these waterways deserve the respect and care owed to such treasured and vital resources.

Sources

1 Holmes, Martha; Maxwell, Gavin; Scoones, Tim. Nile. BBC Books. 2004.
2Bangs, Richard; Scaturro, Pasquale. Mystery of the Nile. G.P. Putnam’s Sons. New York, New York. 2005.
3 Turnbull, March. “The Great Race for the Rivers of Africa.” Africa Geographic. May 2004.
4 “Nile River Facts.” Africa Facts. Web.
5“History of the Nile.” Penn State College of Earth and Mineral Sciences. Web.
6Bangs, Richard; Scaturro, Pasquale. Mystery of the Nile. G.P. Putnam’s Sons. New York, New York. 2005.
7Holmes, Martha; Maxwell, Gavin; Scoones, Tim. Nile. BBC Books. 2004.
8“Nile River Facts.” Africa Facts. Web. September 27, 2017.
9Caputo, Robert. “Journey up the Nile.” National Geographic. May 1985.
10“The Environmental Resources of the Nile Basin.” p 57-98. Web.
11Pavan, Aldo. The Nile From the Mountains to the Mediterranean. Thames and Hudson Ltd. 2006.
12 Holmes, Martha; Maxwell, Gavin; Scoones, Tim. Nile. BBC Books. 2004.
13“The Environmental Resources of the Nile Basin.” p 57-98. Web.
14Holmes, Martha; Maxwell, Gavin; Scoones, Tim. Nile. BBC Books. 2004.