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Understanding Lake Tanganyika: Insights into Climate, Circulation Dynamics, and Fishery Productivity Across Time Using Paleolimnological and Modeling Approaches
Understanding Lake Tanganyika: Insights into Climate, Circulation Dynamics, and Fishery Pr...
Understanding Lake Tanganyika: Insights into Climate, Circulation Dynamics, and Fishery Productivity Across Time Using Paleolimnological and Modeling Approaches

상세정보

자료유형  
 학위논문 서양
최종처리일시  
20260202105639
ISBN  
9798270225896
DDC  
363
저자명  
Kamulali, Tumaini M.
서명/저자  
Understanding Lake Tanganyika: Insights into Climate, Circulation Dynamics, and Fishery Productivity Across Time Using Paleolimnological and Modeling Approaches
발행사항  
[Sl] : The University of Arizona, 2025
발행사항  
Ann Arbor : ProQuest Dissertations & Theses, 2025
형태사항  
146 p
주기사항  
Source: Dissertations Abstracts International, Volume: 87-06, Section: B.
주기사항  
Advisor: Russell, Joellen.
학위논문주기  
Thesis (Ph.D.)--The University of Arizona, 2025.
초록/해제  
요약Lake Tanganyika, one of the world's most biodiverse freshwater lakes and a vital resource for local fisheries, faces significant threats from climate change that jeopardize its ecological integrity and the livelihoods of dependent communities. This dissertation investigates the lake's thermal dynamics, circulation patterns, and historical limnological conditions using the Regional Ocean Modeling System (ROMS) and sediment core analyses. Our simulations show seasonal surface temperatures between ~25.8°C and ~27.8°C, consistent with observations, along with a concerning increase of up to 0.4°C at depths below 150 meters from 2001 to 2020. Primary upwelling occurs in the southern region during the dry season, while secondary upwelling occurs in the northern region during the wet season. Notably, there is previously unrecognized downwelling on the west side of the lake during September to November. Sediment core analyses reveal a warming trend since ~1850 AD, highlighting long-term climate change impacts on the lake's ecosystem. These trends correlate with global climate patterns, raising concerns about future effects on lake stratification and fishery yields. Enhanced productivity in pelagic zones is linked to deep vertical mixing, while productivity in littoral zones is influenced by increased riverine input during wetter phases. Under high-emission climate scenarios projected through 2100, lake surface temperatures could rise by up to 3.9°C, leading to significant changes in isotherm depths and thermal stratification, which may disrupt nutrient transport and adversely affect fish populations that provide approximately 40% of animal protein for local communities. Our findings emphasize the role of hydrodynamic and atmospheric interactions on nutrient distribution and ecological dynamics. They highlight the urgent need for adaptive management strategies, including community involvement in monitoring and international collaboration, to mitigate climate change impacts on Lake Tanganyika's ecosystem. This research offers valuable insights into the interplay between climate, hydrology, and biological productivity, informing strategies to preserve the ecological balance of Lake Tanganyika and support the livelihoods of millions reliant on its resources.
일반주제명  
Climate change
일반주제명  
Paleoclimate science
일반주제명  
Physical oceanography
일반주제명  
Paleoecology
키워드  
Fisheries
키워드  
Lake modeling
키워드  
Paleolimnology
키워드  
Ecological integrity
키워드  
Regional Ocean Modeling System
기타저자  
The University of Arizona Geosciences
기본자료저록  
Dissertations Abstracts International. 87-06B.
전자적 위치 및 접속  
로그인 후 원문을 볼 수 있습니다.

MARC

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■040    ▼aMiAaPQ▼cMiAaPQ
■0820  ▼a363
■1001  ▼aKamulali,  Tumaini  M.
■24510▼aUnderstanding  Lake  Tanganyika:  Insights  into  Climate,  Circulation  Dynamics,  and  Fishery  Productivity  Across  Time  Using  Paleolimnological  and  Modeling  Approaches
■260    ▼a[Sl]▼bThe  University  of  Arizona▼c2025
■260  1▼aAnn  Arbor▼bProQuest  Dissertations  &  Theses▼c2025
■300    ▼a146  p
■500    ▼aSource:  Dissertations  Abstracts  International,  Volume:  87-06,  Section:  B.
■500    ▼aAdvisor:  Russell,  Joellen.
■5021  ▼aThesis  (Ph.D.)--The  University  of  Arizona,  2025.
■520    ▼aLake  Tanganyika,  one  of  the  world's  most  biodiverse  freshwater  lakes  and  a  vital  resource  for  local  fisheries,  faces  significant  threats  from  climate  change  that  jeopardize  its  ecological  integrity  and  the  livelihoods  of  dependent  communities.  This  dissertation  investigates  the  lake's  thermal  dynamics,  circulation  patterns,  and  historical  limnological  conditions  using  the  Regional  Ocean  Modeling  System  (ROMS)  and  sediment  core  analyses.  Our  simulations  show  seasonal  surface  temperatures  between  ~25.8°C  and  ~27.8°C,  consistent  with  observations,  along  with  a  concerning  increase  of  up  to  0.4°C  at  depths  below  150  meters  from  2001  to  2020.  Primary  upwelling  occurs  in  the  southern  region  during  the  dry  season,  while  secondary  upwelling  occurs  in  the  northern  region  during  the  wet  season.  Notably,  there  is  previously  unrecognized  downwelling  on  the  west  side  of  the  lake  during  September  to  November.  Sediment  core  analyses  reveal  a  warming  trend  since  ~1850  AD,  highlighting  long-term  climate  change  impacts  on  the  lake's  ecosystem.  These  trends  correlate  with  global  climate  patterns,  raising  concerns  about  future  effects  on  lake  stratification  and  fishery  yields.  Enhanced  productivity  in  pelagic  zones  is  linked  to  deep  vertical  mixing,  while  productivity  in  littoral  zones  is  influenced  by  increased  riverine  input  during  wetter  phases.  Under  high-emission  climate  scenarios  projected  through  2100,  lake  surface  temperatures  could  rise  by  up  to  3.9°C,  leading  to  significant  changes  in  isotherm  depths  and  thermal  stratification,  which  may  disrupt  nutrient  transport  and  adversely  affect  fish  populations  that  provide  approximately  40%  of  animal  protein  for  local  communities.  Our  findings  emphasize  the  role  of  hydrodynamic  and  atmospheric  interactions  on  nutrient  distribution  and  ecological  dynamics.  They  highlight  the  urgent  need  for  adaptive  management  strategies,  including  community  involvement  in  monitoring  and  international  collaboration,  to  mitigate  climate  change  impacts  on  Lake  Tanganyika's  ecosystem.  This  research  offers  valuable  insights  into  the  interplay between  climate,  hydrology,  and  biological  productivity,  informing  strategies  to  preserve  the  ecological  balance  of  Lake  Tanganyika  and  support  the  livelihoods  of  millions  reliant  on  its  resources.
■590    ▼aSchool  code:  0009.
■650  4▼aClimate  change
■650  4▼aPaleoclimate  science
■650  4▼aPhysical  oceanography
■650  4▼aPaleoecology
■653    ▼aFisheries
■653    ▼aLake  modeling
■653    ▼aPaleolimnology
■653    ▼aEcological  integrity
■653    ▼aRegional  Ocean  Modeling  System
■690    ▼a0404
■690    ▼a0653
■690    ▼a0415
■690    ▼a0426
■71020▼aThe  University  of  Arizona▼bGeosciences.
■7730  ▼tDissertations  Abstracts  International▼g87-06B.
■790    ▼a0009
■791    ▼aPh.D.
■792    ▼a2025
■793    ▼aEnglish
■85640▼uhttp://www.riss.kr/pdu/ddodLink.do?id=T17360928▼nKERIS▼z이  자료의  원문은  한국교육학술정보원에서  제공합니다.

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