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A Profile of the Wami River Sub-Basin

June 2008

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(3)

TABLE OF CONTENTS

Page

Foreword ... ii

Acknowledgments ...iii

Acronyms ...iv

1. Background ... 1

51# Wkh#Gh￀qlqj#Fkdudfwhulvwlfv#ri#wkh#Zdpl#Ulyhu#Vxe0edvlq#dqg#Hvwxdu|... 1

# 514# Wkh#Ulyhu#Vxe0edvlq... 1

2.2 The Estuary ... 7

61# Kxpdq#Xvhv#ri#wkh#Zdwhuvkhg... 7

71# Wkh#Lpsdfwv#ri#Kxpdq#Dfwlylwlhv#rq#wkh#Hvwxdu|/#Ulyhu#Edvlq/# and Freshwater Flows ... 13

81# Srwhqwldo#Ixwxuh#Wkuhdwv#wr#Iuhvkzdwhu#Lq￁rzv#dqg#Hvwxdu|#Khdowk... 15

6. Major Stakeholders and their Interests... 16

:1# Wkh#Jryhuqdqfh#V|vwhp#iru#wkh#Zdpl#Ulyhu#Vxe0edvlq#dqg#Hvwxdu|... 17

;1# Uhfrpphqgdwlrqv#dqg#Rssruwxqlwlhv... 19

Contact Information... 20

Uhihuhqfhv# ... 21

List of Tables Wdeoh#4# Vxppdu|#ri#dydlodeoh#vwuhdp#￁rz#uhfrugv#lq#wkh#Zdpl#ulyhu#vxe0edvlq... 4

Wdeoh#51## Dyhudjh#gdlo|#￁rz#dw#vl{#jdjlqj#vwdwlrqv... 5

Wdeoh#61## Vhdvrqdo#frqwulexwlrq#wr#dqqxdo#￁rz#yroxphv#dw#￀yh#jdjlqj#vwdwlrqv... 6

Wdeoh#71## Wuhqg#lq#vhdvrqdo#phdq#￁rzv#dw#vhohfwhg#jdjlqj#vwdwlrqv... 6

Wdeoh#81## Srsxodwlrq#jurzwk#udwhv#lq#vhohfwhg#yloodjhv#lq#wkh#Zdpl#ulyhu#vxe0edvlq... 8

Table 6. Trends in river basin and estuary threats ... 15

Table 7. Major stakeholders and their interests... 16

List of Figures Figure 1. Location of river basins draining the Eastern Arc Mountains ... 2

Iljxuh#51## Zdpl#ulyhu#vxe0edvlq... 3

Iljxuh#6## W|slfdo#vhdvrqdo#udlqidoo#sdwwhuqv#lq#wkh#Zdpl0Uxyx#ulyhu#edvlq1... 4

Iljxuh#71## Zdpl0Uxyx#ulyhu#vxe0edvlq#jdjlqj#dqg#phwhrurorjlfdo#vwdwlrqv... 5

Iljxuh#81## Vhdvrqdo#￁rz#sdwwhuq#lq#wkh#Zdpl#... 6

Iljxuh#91## Vsdwldo#yduldwlrq#ri#wkh#vorsh#ri#d#olqhdu#wuhqg#iru#dqqxdo#￁rzv#lq#wkh#Zdpl0Uxyx1... 6

Iljxuh#:### Vsdwldo#yduldwlrq#ri#wkh#vorsh#ri#d#olqhdu#wuhqg#iru#vkruw#udlqv#lq#wkh#Zdpl0Uxyx... 6

Figure 8. Saadani National Park...11

Iljxuh#<1## Hohskdqw#fruulgruv#ghshqghqw#rq#wkh#Zdpl#ulyhu#vxe0edvlq... 12

(4)

FOREWORD

Wklv#sur￀oh#ri#wkh#Zdpl#ulyhu#vxe0edvlq#lv#suhsduhg#e|#wkh#Wdq}dqld#Frdvwdo#Pdqdjhphqw#Sduwqhuvkls#+WFPS,# dqg#lwv#odqgvfdsh0vhdvfdsh#lqlwldwlyh#xqghu#wkh#Vxvwdlqdeoh#Frdvwdo#Frppxqlwlhv#dqg#Hfrv|vwhpv#surmhfw# vxssruwhg#e|#wkh#Wdq}dqld#plvvlrq#ri#wkh#Xqlwhg#Vwdwhv#Djhqf|#iru#Lqwhuqdwlrqdo#Ghyhorsphqw#+XVDLG,1##Wkh# lqwhqwlrq#ri#wkh#sur￀oh#lv#wr#v|qwkhvl}h#h{lvwlqj#lqirupdwlrq#rq#wkh#Zdpl#zlwk#wkh#jrdo#ri#surprwlqj#odqgvfdsh0

seascape scale planning and conservation.

Wkh#sur￀oh#zdv#vwduwhg#lq#Dsulo#53391#Vlqfh#wkhq#lw#kdv#fdwdo|}hg#d#qxpehu#ri#Zdpl#ulyhu#dvvhvvphqwv#dqg# vxvwdlqdeoh#ghyhorsphqw#dfwlylwlhv1#Wkhvh#lqfoxgh#d#vwxg|#ri#wkh#lqwhuolqndjhv#ehwzhhq#Zdpl#iuhvkzdwhu#￁rzv# dqg#Vddgdql#Qdwlrqdo#Sdun#+Iheuxdu|#533:,/#dq#hfrorjlfdo#dvvhvvphqw#ri#wkh#Zdpl#hvwxdu|#+Pdufk#533:,/#dqg#d# qhz#surmhfw#vxssruwhg#e|#d#sduwqhuvkls#ehwzhhq#Wkh#Frfd0Frod#Frpsdq|#dqg#XVDLGᄋv#joredo#zdwhu#ri￀fh1#Wkh# Zdwhu#dqg#Ghyhorsphqw#Dooldqfh#+ZDGD,#surmhfw#zdv#lqlwldwhg#lq#Iheuxdu|#533:1#Lw#kdv#d#49#prqwk#wlphiudph#

and a focus on water sanitation and education, strengthening of community organizations, environmental

(5)

ACKNOWLEDGMENTS

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time, interest, insights and information.

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Odvwo|/#zh#zrxog#olnh#wr#uhfrjql}h#wkh#jhqhurvlw|#zlwk#zklfk#vr#pdq|#shrsoh#lq#wkh#Zdpl#ulyhu#vxe0edvlq# dqg#hvwxdu|#vkduhg#zlwk#xv#wkhlu#rzq#revhuydwlrqv#derxw#wkh#Zdpl#ulyhu/#lwv#frqglwlrq/#xvhv#dqg#￀vklqj#dqg#

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ACRONYMS

FUF# Frdvwdo#Uhvrxufhv#Fhqwhu

EFA Environmental Flows Assessment

FIU Florida International University

GIS Geographic Information Systems

JORZV# Joredo#Zdwhu#iru#Vxvwdlqdeoh#Surjudp

GoT Government of Tanzania

MI# Mdqxdu|0Iheuxdu|

MMDV# Mxqh0Mxo|0Dxjxvw0Vhswhpehu PDP# Pdufk0Dsulo0Pd|

PRZ# Plqlvwu|#ri#Zdwhu#

MSEL Mtibwa Sugar Estates, Ltd.

NEMC National Environmental Management Council

RQG# Rfwrehu0Qryhpehu0Ghfhpehu

SANAPA Saadani National Park Authority

SUCCESS Sustainable Coastal Communities and Ecosystems

TANAPA Tanzanian National Parks Authority

TCMP Tanzania Coastal Management Partnership

Tsh Tanzania shillings

XUL# Xqlyhuvlw|#ri#Ukrgh#Lvodqg

USAID United States Agency for International Development

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A PROFILE OF THE WAMI RIVER SUB-BASIN AND ESTUARY

1. Background

In an increasingly crowded world, competition for freshwater is becoming intense. Competition for freshwater

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and the quality of that water. Too often, the allocation of freshwater among its human users ignores the impacts that such decisions have upon the goods and services generated by healthy estuaries. Those most negatively affected by such changes are often the poor who are dependent on natural systems for livelihoods.

The Tanzania Coastal Management Partnership for Sustainable Coastal Communities and Ecosystems is

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upstream impacts on the coastal and estuarine area. This initiative recognizes that any attempt to integrate

zdwhuvkhg#dqg#hvwxdu|#sodqqlqj#dqg#pdqdjhphqw#lv#d#frpsoh{#xqghuwdnlqj#wkdw#uhtxluhv#dgguhvvlqj#d#qxpehu#

of management issues simultaneously, integrating across the needs of competing user groups, and integrating

gdwd#dqg#nqrzohgjh#rq#krz#dqg#zk|#d#odujh#dqg#frpsoh{#hfrv|vwhp#lv#fkdqjlqj1#

o Describe governance systems

r# Gh￀qh#nh|#vwdnhkroghu#jurxsv#dqg#wkhlu#lqwhuhvwv

o Identify major gaps in information as well as priorities for further analysis and management

51# Wkh#Gh￀qlqj#Fkdudfwhulvwlfv#ri#wkh#Zdpl#Ulyhu#Vxe0edvlq#dqg#Hvwxdu|

514## Wkh#Ulyhu#Vxe0edvlq

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within the basin, such as mountains, forests, woodlands, wetlands, pastures, agricultural areas and urban concentrations. The same geomorphological unit is often referred to as a drainage basin, a catchment or a watershed.

The main connection between the lower and upper reaches of a river basin and its component ecosystems is water. Those who live and work at the downstream end of a river basin depend upon the good conduct of those who use the upper reaches to ensure that adequate quantities and quality of water percolates from the upstream reaches to the downstream users.

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about 40,000 km2#dqg#furvvhv#wkh#srolwlfdo#erxqgdulhv#ri#irxu#dgplqlvwudwlyh#Uhjlrqv>#qdpho|#Grgrpd/#

Prurjrur/#Wdqjd#dqg#Frdvw#Uhjlrqv1#

Wkh#Zdpl#ulyhu#ruljlqdwhv#lq#wkh#fdwfkphqw#ri#wkh#Xndjxux/#Uxehkr/#dqg#Qjxux#prxqwdlq#udqjhv/#zklfk#duh#doo# sduw#ri#wkh#Hdvwhuq#Duf#fkdlq#ri#prxqwdlqv#lq#Nhq|d#dqg#Wdq}dqld#+vhh#Iljxuh#4,1#Wkh#Hdvwhuq#Duf#Prxqwdlqv#duh#

recognized as one of 25 globally important “hot spots” for forest biodiversity in need of immediate conservation

dfwlrq1#Wkh#Hdvwhuq#Duf#Prxqwdlqv#duh#gluhfwo|#olqnhg#wr#wkh#Lqgldq#Rfhdq1#Suhgrplqdqwo|#Hdvwhuo|#Wudgh#Zlqgv#

from the ocean are forced to rise, cool and are converted to precipitation on the mountains. The main source of water for the lowlands, which are the main population centers, is therefore the Eastern Arc Mountains.

+vrxufh=#Iruhvwu|#dqg#Ehhnhhslqj#Glylvlrq/#5338,

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Iljxuh#51#Zdpl#ulyhu#vxe0edvlq

(10)

Iljxuh#6#W|slfdo#vhdvrqdo#udlqidoo#sdwwhuqv#lq#wkh#Zdpl0Uxyx#ulyhu#edvlq1#Wkh#yhuwlfdo#pd{lpxp#lv#633# pp#dqg#wkh#lqwhuydo#lv#83#pp#zkloh#wkh#krul}rqwdo#d{lv#lv#iurp#Vhswhpehu#+ohiw,#wr#Dxjxvw#+uljkw,1#Vrxufh=#

Forestry and Beekeeping Division, 2005, p. 31.

Ghfuhdvlqj#dyhudjh#vhdvrqdo#udlqidoo#lq#wkh#Zdpl#vxe0edvlq#rffxuuhg#iurp#4<97#wr#4<<6#iru#doo#vhdvrqv#h{fhsw# wkh#vkruw#udlqv#ehwzhhq#Rfwrehu#dqg#Ghfhpehu#+Iruhvwu|#dqg#Ehhnhhslqj#Glylvlrq/#5338/#s1#64,1#Lq#hdvwhuq# Wdq}dqld#dqg#wkh#uhjlrq#ri#wkh#Zdpl#ulyhu#vxe0edvlq/#wkhuh#duh#dqhfgrwdo#uhsruwv#ri#gurxjkw#frqglwlrqv#dqg# ghfuhdvhg#gu|#vhdvrq#edvh#￁rzv#lq#wkh#Zdpl#ryhu#wkh#sdvw#￀yh#|hduv1#Udlqidoo#gdwd#wkurxjk#5336#surylghg#e|# wkh#Zdpl0Uxyx#Zdwhu#Edvlq#Ri￀fh#lqglfdwh#d#grzqzdug#wuhqg#lq#suhflslwdwlrq#+Vxphuolq#dqg#Julw}qhu/#533:,1## Gxulqj#wkh#orzhvw#￁rz#shulrg/#wkh#orzhu#Zdpl#ulyhu#lv#uhgxfhg#wr#d#vhulhv#ri#uhvlgxdo#srrov#frqqhfwhg#e|#d#

shallow stream. Since the share of agriculture that is rain fed is high in Tanzania, this trend increases food

lqvhfxulw|1#Suhglfwlrqv#iru#folpdwh#fkdqjh#lq#wkh#uhjlrq#dovr#lqglfdwh#wkdw#vxe0Vdkdudq#Diulfd#zloo#eh#dw#ulvn#iru# irrg#vhfxulw|#+Fr0rshudwlyh#Surjudp#rq#Zdwhu#dqg#Folpdwh/#5339,1#

Vwuhdp￁rz#dqdo|vlv1#D#v|vwhp#ri#56#￁rz#jdjlqj#vwdwlrqv#zdv#hvwdeolvkhg#lq#wkh#Zdpl0Uxyx#ulyhu#edvlq#lq#wkh# 4<83v#dqg#4<93v1#Irxuwhhq#ri#wkh#56#zhuh#orfdwhg#rq#wkh#Zdpl#vxe0edvlq1#Wkh#jdjlqj#vwdwlrqv#dqg#dydlodeoh#

records are shown in Table 1.

Wdeoh#41#Vxppdu|#ri#dydlodeoh#vwuhdp#￁rz#uhfrugv#lq#wkh#Zdpl#ulyhu#vxe0edvlq

Station Ulyhu Location Lat. Long. Duhd#+np2, Available records

1G1 Zdpl Dawawa 0917666 37.5333 28,488 4<860;6 1G2 Zdpl# Mandera 0915666 38.4000 36,450 4<870;7

1G5A Tami Msowero 09184:5 37.2114 4<970;6

1G6 Kisangata Mvumi 091949: 37.1833 404 4<8809< 1GA1A Lukigura Nlpdped#Ug1#Eu1 091;333 37.8000 1,060 4<970;4 1GA2 Mziha P}lkd#+Nlpdped, 091<333 37.7833 178 4<970;<

1GB1A Diwale Ngomeni 091499: 37.6167 4<970;<

1GD2 Mkondoa Kilosa 091;666 37.0000 17,560 4<850;4 1GD14 Kinyasungwe Gulwe 0917666 35.4167 11,103 4<8:0:: 1GD16 Kinyasungwe Nrqjzd2Grgrpd 0915333 36.2833 9,570 4<8;0;7 1GD29 Mkondoa Mbarahwe 0918<8; 36.7833 475 4<9<0<6 1GD30 Lumuma Kilimalulu 0919;66 36.6667 502 4<9<0:8 1GD31 Mdukwe Mdukwe 091;644 36.9333 460 4<9<05335

4<:60:;

1GD36 Mkata Mkata 091:964 37.3686

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Lq#5339/#wkh#ZUEZR#uhkdelolwdwhg#45#vwuhdp#￁rz#jdxjh#vwdwlrqv1#Wkh#orfdwlrq#ri#wkh#vwdwlrqv#lv#vkrzq#lq#

Figure 4.

Iljxuh#71#Zdpl0Uxyx#ulyhu#vxe0edvlq#jdjlqj#dqg#phwhrurorjlfdo#vwdwlrqv

Uxqrii#iurp#wkh#Grgrpd#uhjlrq#ri#wkh#Zdpl#dqg#lq#wkh#sodlqv#ri#wkh#orzhu#Zdpl#lv#orz#gxh#wr#kljk#udwhv#ri# hydsrudwlrq#lq#wkh#ulyhu#vxe0edvlq#dqg#orz#suhflslwdwlrq1#Prvw#ri#wkh#￁rz#+derxw#93#wr#:3#shufhqw,#dw#Pdqghud# vwdwlrq#+4J5,#ruljlqdwhv#iurp#d#vpdoo#sduw#ri#wkh#fdwfkphqw#rq#wkh#vorshv#ri#Qjxux/#Xndjxux#dqg#Uxehkr# prxqwdlqv#ehfdxvh#wkhvh#duhdv#kdyh#pxfk#kljkhu#udlqidoo#+Vkloxqjxvkhod/#533:,1

Dyhudjh#gdlo|#￁rzv#+DGI,#iru#vhohfwhg#jdjlqj#vwdwlrqv#hvwdeolvkhg#iurp#dydlodeoh#uhfrugv#duh#vkrzq#lq#Wdeoh#5= Wdeoh#51#Dyhudjh#gdlo|#￁rz#dw#vl{#jdjlqj#vwdwlrqv

Flow Gauge – tributary and location DGI#+p6#2v, (#}hur#￁rzv

4J4#ᄇ#Zdpl#dw#Gdndzd#eulgjh 25.8 0.0

4J5#ᄇ#Zdpl#dw#Pdqghud 60.6 0.6 1GA1A – Lukigura at Kimamba road bridge 3.98 36.3

4JD5#ᄇ#P}lkd#dw#P}lkd#+Nlpdped, 1.28 17.1

1GD2 – Mkondoa at Kilosa 10.15 0.2

1GD31 – Mdukwe at Mdukwe 4.58 0.0

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up during relatively dry years.

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Me

1G2 Wettest Month: April/May

Driest month: October

Seasonal pattern: Transition

Sep Oct Nov Dec Jan Feb Mar Apr May Jun Jul Aug

Station Useful records Trend

I n t e r m e d i a t e

Figure 6. Spatial variation of the slope of a linear wuhqg#iru#dqqxdo#￁rzv#lq#wkh#Zdpl0Uxyx#edvlq1# \hoorz#wuldqjohv#lqglfdwh#ghfuhdvlqj#wuhqgv#+vrxufh=##

Iruhvwu|#dqg#Ehhnhhslqj/#5338,

Figure 7 Spatial variation of the slope of a linear trend iru#vkruw#udlqv#+RQG,#lq#wkh#Zdpl0Uxyx#edvlq1#\hoorz# wuldqjohv#lqglfdwh#ghfuhdvlqj#wuhqgv#+vrxufh=#Iruhvwu|#

(13)

515#Wkh#Hvwxdu|1

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and well preserved mangrove forests. The salty marsh estuaries close to the river are home for pelican and

￁dplqjr#zklfk#frph#wr#ihhg#rq#￀vk#dqg#fuxvwdfhdqv#ri#wkh#vhd1#Wkh#suhydlolqj#vshflhv#ri#pdqjuryhv#lq#wkh# hvwxdu|#duh#Dylfhqqld#pdulqd#+Yhuehqdfhdh,#dqg#wkuhh#vshflhv#ri#Ukl}rskrudfhdh#+Ukl}rskrud#pxfurqdwd# ru#pnrnr/#Euxjxlhud#j|pqruukl}d#ru#pvlqgl#dqg#Fhulrsv#wdvjdo#ru#pndqgdd,1#Wkh#pdqjuryhv#vxssruw#dq# h{whqvlyh#lqwhuwlgdo#￀vkhu|#dqg#surylgh#qxuvhu|#jurxqgv#iru#d#qdwlrqdoo|#lpsruwdqw#sudzq#lqgxvwu|1#Pdqjuryhv#

also protect the coastline against destructive waves, enhance water quality, retain sediments and nutrients,

dqg#surylgh#kdelwdw#iru#￀vk/#elug#vshflhv/#klssrv/#furfrglohv/#dqg#prqnh|v1#

that occurs between September and December. These seasons correspond with transitional and wet periods

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deposits and mangrove forests near river mouths serve as important breeding ground for several species of

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November and December, and migrate back out to the ocean during the longer rains that occur from March

wr#Pd|1##Sudzq#￀vklqj#suhvhqwo|#grhv#qrw#rffxu#lq#wkh#hvwxdu|/#wkh#pdlq#uhdvrq#ehlqj#ihdu#ri#klssrv#dqg#

crocodiles rather than a desire to protect nursery areas.

Dowkrxjk#wkh#sudzq#￀vkhu|#grplqdwhv#wkh#orfdo#hfrqrplhv#ri#Vddgdql#dqg#vxuurxqglqj#vpdoohu#yloodjhv/# hvwxdulqh#￀vkhv#duh#dovr#lpsruwdqw#vrxufh#ri#irrg#dqg#lqfrph#lq#wkh#duhd/#sduwlfxoduo|#wr#wkrvh#shrsoh#olylqj# dorqj#wkh#edqnv#ri#wkh#Zdpl#ulyhu1##

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management of natural resources in areas within and adjacent to the estuary, as well as in areas in the greater

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61# Kxpdq#Xvhv#ri#wkh#Zdwhuvkhg#

Rxwvlgh#ri#wkh#pdmru#xuedq#duhdv#+Prurjrur/#Grgrpd/#dqg#Nledkd,/#djulfxowxuh#lv#wkh#sulpdu|#olyholkrrg#lq# wkh#Zdpl#ulyhu#vxe0edvlq1#Vxjdu#fdqh/#vlvdo#dqg#frwwrq#duh#surgxfhg#dv#fdvk#fursv#lq#odujh#vfdoh#djulfxowxuh1#

(14)

Vpdoo#kroghu#djulfxowxuh#lqfoxghv#pdl}h/#ulfh/#vzhhw#srwdwrhv#dqg#ehdqv1#Vxusoxv#irrg#fursv#lq#vpdoo0vfdoh# djulfxowxuh#duh#w|slfdoo|#vrog#lq#orfdo#pdunhwv1#Rwkhu#uxudo#olyholkrrg#dfwlylwlhv#lqfoxgh#olyhvwrfn#nhhslqj/# ehh#nhhslqj/#kxqwlqj#dqg#￀vklqj1#Lq#jhqhudo/#wkh#rqo|#vrxufh#ri#olyholkrrg#dydlodeoh#wr#pdq|#lq#wkh#edvlq#lv# sulpdu|/#l1h1#d#olyholkrrg#edvhg#rq#wkh#gluhfw#h{sorlwdwlrq#ri#wkh#edvlqᄋv#qdwxudo#uhvrxufhv1#Wkh#vxffhvv#ri#wkhvh#

livelihoods is directly related to land and water availability.

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harvesting of forest products for subsistence and local use has been increasing largely because of population

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At the same time, agricultural practices are often not environmentally sustainable. Kajembe and Nzunda

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due to high demand of land. Similarly, shifting cultivation is diminishing. The continuous use of soil coupled with lack of supplementation of fertility with fertilizers has resulted in declines in yields. Soil conservation

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on the steepest of the slopes.

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as observed from the 1988 and 2002 population censuses. The data demonstrate a population increase in most

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decades, and recent trends suggest it will continue to grow in the near future. Between 1988 and 2002, national

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Morogoro rural

Mvomero Mindu Tulieni Tukamisasa

Growth rate

081;

(15)

and the walls of the pits are not protected. Many are also ignorant of the pollution they cause to the river by daily life practices like washing clothes in the riverbed.

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Vrph#ri#wkh#lpsruwdqw#odqg#xvh#ihdwxuhv#lq#wkh#Zdpl#duh#ghvfulehg#lq#pruh#ghwdlo#ehorz=

Pwlezd#Vxjdu#Hvwdwh#Owg1#+PVHO,.2 The Mtibwa Sugar Factory in the village of Turiani and in the eastern

foothills of the Nguru mountain range was established in the early 1960s and was owned by the Government

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primarily grown in four estates, of which MSEL is one of them.

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countries in Africa and Southeast Asia. It has a workforce of 1,300 permanent employees and some 1,500

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MSEL occupies an area of more than 6,000 hectares of land of which 5,400 ha are currently under cane

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fed. The company also purchases sugar cane from about 900 local farmers through an out growers program. In 2002 it was estimated that sugarcane out grower farms covered over 12,000 hectares owned or cultivated

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cane processed at the factory comes from the factory and half from out growers. The sugar cane is harvested

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February.

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have been earmarked for sugar cane cultivation.

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2 Unless otherwise noted, all information comes from personal communication with Mr. Edward Adul, Irrigation Engi0

(16)

Fkdolq}h0Zdpl#zdwhu#wuhdwphqw#sodqw#dqg#vxsso|#vfkhph. The Chalinze water project was initiated in 2001 and has the purpose of providing water treatment and delivery to the Chalinze township and surrounding

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on wells, but the groundwater is not potable and during the dry season the water table is too low. The length of the main pipe line from Chalinze to the target area is 126 km and the distribution pipe line is 34 km.

The design capacity of the treatment plant is 7,200 m3 2gd|1#Dv#ri#Dsulo#5339#wkh#sodqw#zdv#surylglqj#;33#p3

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Chalinze, Pingo, Msoga, Mboga, Lugoba, Saleni, Mazizi, Msata and Kihangaiko in the south direction. In the

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Kimange and Mbwewe. The communities involved have been mobilized to form the association called Chalinze

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intake for turbidity, Ph, conductivity, and ecoli.

The Chalinze water supply project receives a subsidy from the government of Tanzania, but it is designed to

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standpipes determined by the population in the village. Each standpipe is monitored by a village member

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than other means of providing outside water. Before the project, water brought in by truck was selling for as

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cover costs of operation.

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development. Many of the poorer villages have a high dependence on charcoal making for livelihood. The government restricted charcoal permits in 2005.

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system contains both terrestrial and marine ecosystems. The terrestrial portion of the park consists of coastal plain and low hills generally below 100 meters elevation with somewhat higher ground to the southwest

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and two Collaborative Fisheries Management Areas.

(17)

Figure 8. Saadani National Park

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only perennial river in the park and thus a primary water source for the diverse wildlife of the park in the dry season.

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global biodiversity hotspots in most urgent need of immediate conservation action.

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(18)

Iljxuh#<1#Hohskdqw#fruulgruv#ghshqghqw#rq#wkh#Zdpl#ulyhu#vxe0edvlq

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basin. All informants feel that these are ancestral migration routes that may require several years for elephant

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season habitats and the migration corridors that animals travel to get to them is needed for a holistic approach to their protection.

Informal discussion with TANAPA planning staff and review of the Saadani National Park Management

(19)

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will grow as much as 100 times in the near future. Such growth is indicative of the potential opportunities for economic return to the country. As Saadani National Park grows in popularity and more people visit the area,

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during the dry season there may be additional demand for freshwater from the river caused by an increase in the number of tourists visiting SANAPA. More tourists could also mean more boat trips on the river and

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dwelling species. These considerations are important for future tourist investment and lodge construction within the Saadani National Park and surrounding areas.

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line with Tanzanian national interests, as is the generation of revenue from tourism. The location of Saadani National Park along a relatively undeveloped coastline and adjacent to terrestrial habitat still supporting large

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National Park ecosystem and one of the biggest attractions for international tourists. Economic return will depend greatly on natural resource condition in this area. Therefore, there is a clear need for conservation and

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in the river, biodiversity, and livelihood strategies.

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and the condition of the estuary. There is no continuous monitoring program of water quality parameters and condition of the river basin and estuary.

It is known, however, that the environment in the basin is being degraded and polluted. Agriculture has

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basin for agricultural irrigation, industry, and household use. In areas with intensive agricultural activities, people cultivate up to the river bank. It is known that this accelerates erosion and sedimentation. The potential

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Deforestation

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driving forces for forest cover loss are population growth, agriculture, charcoal making, and cutting of trees for poles and home construction.

Trees and other vegetation serve to hold moisture and regulate the release of water into the basin. They reduce the runoff velocity during the rainy season and increase runoff during the dry season by recharging

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stream temperature, which in turn disrupts aquatic life cycles.

Depletion of forest cover in the catchment area of the Eastern Arc Mountains has been analyzed. It is estimated that about 2000 years ago the forest cover on the Eastern Arc Mountains was 23,000 km2, which was reduced

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chain the decline in woodland cover was more than 50 percent over a span of 20 years between 1970 and 1990

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Another study of land use and land cover change in the area surrounding Saadani National Park using remote

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that the amount of agricultural land outside the park has increased by 76 percent. At the same time, there has

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the installation of new gauges at suitable sites close to understand the interactions between the forest cover,

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(20)

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for salt making.

As a result of increasing pressures on mangroves throughout the country, the Forest and Beekeeping

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the amount of illegal harvesting and littering. Although the threat of mangrove cutting has decreased in recent years, it is essential for Saadani National Park staff to continue their enforcement efforts to ensure that the demand for charcoal in various areas of Tanzania does not result in the removal of mangroves within and

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that number has dropped to less than 10 kilograms per day and working in deeper waters is now necessary to

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Several reasons have been given for the noted decrease in shrimp catch. Primary among these are the increase

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mangroves removes important breeding habitat for shrimp and allows water temperatures to increase, which prompts migration out into the ocean. Since the creation of Saadani National Park, mangrove cutting and the

Gambar

Figure 1. Location of river basins draining the Eastern Arc Mountains +vrxufh=#Iruhvwu|#dqg#Ehhnhhslqj#Glylvlrq/#5338,
Figure 4. Iljxuh#71#Zdpl0Uxyx#ulyhu#vxe0edvlq#jdjlqj#dqg#phwhrurorjlfdo#vwdwlrqv
Figure 7  Spatial variation of the slope of a linear trend iru#vkruw#udlqv#+RQG,#lq#wkh#Zdpl0Uxyx#edvlq1#\hoorz#wuldqjohv#lqglfdwh#ghfuhdvlqj#wuhqgv#+vrxufh=#Iruhvwu|#dqg#Ehhnhhslqj/#5338,
Figure 8. Saadani National Park
+3

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