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[object Object],GLACIER RECESSION & HUMAN VULNERABILITY IN THE CORDILLERA BLANCA, PERU B.G. Mark (1) , J. Bury (2), J.M. McKenzie (3), T. Condom (4), M. Baraer (3), Adam French (2), K.I. Huh (1), Sarah Fortner (1) and Ricardo Jesus Gomez (5) (1) Geography & BPRC, Ohio State University, (2) Environmental Studies, UCSC, (3) Earth and Planetary Sciences, McGill University, (4) Institut de Recherche pour le DĂ©veloppement, France; (5) Unidad de Glaciologia y Recursos Hidricos, Peru http://www.water4people.org/
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],http://bprc.osu.edu/glacierchange ,[object Object],[object Object],[object Object],[object Object],[object Object]
Tropical Andean Glaciers 71% in Peru 22% in Bolivia 4% in Ecuador 3% in Colombia ~1% Venezuela Source-J. Bury UC-Santa Cruz NASA Worldwind
Cordillera Blanca Peru Huandoy (6395 m) ,[object Object],[object Object],[object Object],[object Object],Source-J. Bury UC-Santa Cruz NASA Worldwind http:// newark.osu.edu/facultystaff/personal/dleavell/Pages/default.aspx
 
Regional climate model PDF of annual temperature in the Andes for 1961-90 (blue) and 2071-2100 (green-B2, red-A2) Mean temperature change (2071-2100 minus 1961-90) as simulated with PRECIS (Urrutia & Vuille, 2009) B2 scenario A2 scenario
[object Object],[object Object],[object Object],Source-J. Bury UC-Santa Cruz NASA Worldwind Rio Santa
Interdisciplinary Research  Objectives & Methods ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Glacier tributaries Case-study watersheds Discharge Station Colcas Los Cedros Paron Llanganuco Chancos Querococha Pachacoto La Recreta
Tributaries to Rio Santa:  Normalized annual discharge anomalies  ( 1953-1997) ,[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object]
[object Object],[object Object],La Balsa
HBCM: distributed, multi-component mixing model at the watershed scale Baraer et al. 2009, Adv Geosci
Simplified watershed characteristics M. Baraer (1) Llanganuco (2) Quilcay (3) Querococha
Spatial variability of meltwater & groundwater (1) Llanganuco (2) Quilcay (3) Querococha M. Baraer
M. Baraer
Stream flow time series analysis:  test anticipated dynamic influence of glacier melt ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
New discharge logger prototype 1.5m 0.7m 0.1m 0.08m (int)
 
Water balance model discharge
Discharge simulation by glacier retreat rate ( Îł)  scenarios ,[object Object],[object Object]
Phase of glacier melt influence on discharge ,[object Object],[object Object]
Discharge phase comparison with historic & new observations
Regional synthesis ,[object Object],[object Object]
Fortner Present water quality issues in the Upper Rio Santa, Peru Mine Tailings Rio Santa
Fortner
Fortner
Fortner
Fortner What does this mean for glacial ecosystems? ,[object Object],[object Object]
Rio Quilcay Glacier fed headwaters Melt routed through shallow wetlands Metamorphic sedimentary rocks, sulfide deposits Large pastureland and eventual municipal water supply  How is water quality impacted along flow paths from headwaters?
Discharge = ~1.2 m 3 /s, ~3/5 from NE, ~2/5 from NW
Unusual tributary in northeast Below convergence Lake feeding northwest branch
Alpine vegetation (w/o lake drainage) Wetlands Less  Vegetation Lakes pH rapidly decreases downstream, then increases
Sulfide mineral oxidation tributary:  Elevated concentrations of DOC, all metals (except Cu, Pb)
Fortner 1 Cameron et al., 1995;  2 Schuster, 2005 Tributary exceeds WHO drinking water standards
Silicate Weathering in Glacial Meltwater from the Cordillera Blanca Relative to specific runoff, high cation flux indicates high chemical weathering rates
Summary of insights Quantity: ,[object Object],[object Object],[object Object],[object Object]
Fortner ,[object Object],[object Object],[object Object],[object Object],[object Object]
Related publications ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],http:// www.geography.osu.edu/faculty/bmark /

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Glacier Change and Human Vulnerability

Hinweis der Redaktion

  1. White line elevation of highest mountains in the grid used to make the model. Triangles are the elevations of the highest mountains at those latitudes. The white area was not modelled.
  2. In Peru, glacier melt is important not only for hydropower, but for agricultural and domestic use. Therefore, it it is important to understand stream geochemitsry and how it relates to human heath. Will water quality get worse with the loss of glacial melt?
  3. In Peru, glacier melt is important not only for hydropower, but for agricultural and domestic use. Therefore, it it is important to understand stream geochemitsry and how it relates to human heath. Will water quality get worse with the loss of glacial melt?
  4. In Peru, glacier melt is important not only for hydropower, but for agricultural and domestic use. Therefore, it it is important to understand stream geochemitsry and how it relates to human heath. Will water quality get worse with the loss of glacial melt?
  5. In Peru, glacier melt is important not only for hydropower, but for agricultural and domestic use. Therefore, it it is important to understand stream geochemitsry and how it relates to human heath. Will water quality get worse with the loss of glacial melt?
  6. Thank you for inviting me here. It is my pleasure to speak to you about Mountain Glacier Melt Geochemistry and share some insights from reesearch in the Antarctic Dry Valleys and the Cordillera Blanca, Peru
  7. Make note that headwaters are neutral
  8. references