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How Do Homebuyers Value Different Types of Green Space?
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IRI Technical Report 11-04: Final Report: Summer Institute on Climate Information for Public Health
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High-yield oil palm expansion spares land at the expense of forests in the Peruvian Amazon
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North Tropical Atlantic influence on western Amazon fire season variability
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Climate and Society No. 3: A Better Climate for Disaster Risk Management
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Evaluation of Satellite Rainfall Estimates and Gridded Gauge Products over the Upper Blue Nile Region [In Nile River Basin, Melesse, A. M., Ed.]
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Revisiting the East African malaria debate
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IRI Technical Report 11-03: HARITA IRI Report to Oxfam America: Final Report for General IRI Capacity Building and Technical Support for HARITA Micro-Insurance Scale up (Re: ETH 018 /10)
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Decadal Climate Predictability and Prediction: Where Are We?
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IRI Progress Report to NOAA 2011 – NA10OAR4310210 – July 2010 – March 2011
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IRI Technical Report 11-01: Climate and Health in Africa: 10 Years On Workshop. Addis Ababa, Ethiopia
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The Maritime Continent Monsoon (In press. In The Global Monsoon System: Research and Forecast, Chang, C.-P., et al, Ed.)
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Risk Assessment, Risk Management and Communication: Methods for climate variability and change (In “Treatise on Water Science,” Wilderer, P., Ed.)
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Increased climatic stress on high-Andean ecosystems in the Cordillera Central of Colombia [In Climate Change and Biodiversity in the Tropical Andes, Herzoz, et al, Ed.]
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Predictability of Seasonal Sahel Rainfall Using GCMs and Lead-Time Improvements Through the Use of a Coupled Model
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Consequences of climate change for ecosystems and ecosystem services in the Tropical Andes [In Climate Change and Biodiversity in the Tropical Andes, Herzog, et al, Ed.]
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Trend changes of African airmass intrusions in the marine boundary layer over the subtropical Eastern North Atlantic region in winter
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Synthesis of the Climate of the Tropical Andes [In Climate Change and Biodiversity in the Tropical Andes, Herzog, et al, Ed.]
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Interannual Variation of the South Asian Monsoon: Links with ENSO and EQUINOO (In The Global Monsoon System: Research and Forecast, Chang, C.-P., et al, Ed.)
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