Earth Sciences

Relative Contribution of the Most Important Environmental Variables to the Model

Appendix S1. Codes for 22 environmental variables layers used to model species distribution.Appendix S2. Herpetofauna species distribution in southeast Mexican states, number of localities, threat and endemic categories and relative contribution of the

Dead Zones: Where Even Fish Can T Live

Dead Zones: Where even fish can t live.What are dead zones?.Dead zones are hypoxic areas of the world s oceans. This means that they have less oxygen in the water than is needed to sustain sea-life. They tend to be located near to the shore, usually

Modeling and Numerical Simulation of Non-Isothermal Water and Organic Solute Transport

Modeling and Numerical Simulation of Non-Isothermal Water and Organic Solute Transport

Modeling and Numerical Simulation of Non-isothermal Water and Organic Solute Transport in Soil Vadose Zone.Josep M Gasto1, Jordi Grifoll1 and Yoram Cohen2.Presented at AIChE 2002 Annual Meeting, November 3 - 8, Indianapolis, Indiana

Bilingual Unit 3. Professional Subject: Tourist Destinations

Teacher: David Romero Moreno Subject: Tourist Destinations. Training course: Travel agency and event management.BILINGUAL UNIT 3. PROFESSIONAL SUBJECT: TOURIST DESTINATIONS.THE TOURIST GEOGRAPHY WORLDWIDE.1. The World Tourism Organization (UNWTO / OMT).1.1. Definition and functions

Synopsis: ENSO-Neutral Conditions May Transition to La Niña Co s2

EL NIÑO/SOUTHERN OSCILLATION (ENSO) DIAGNOSTIC DISCUSSION.CLIMATE PREDICTION CENTER/NCEP/NWS.and the International Research Institute for Climate and Society.ENSO Alert System Status: Not Active.Synopsis: ENSO-neutral is expected to continue into the Northern Hemisphere summer 2014

On-Line Resource 2

On-Line Resource 2

On-Line Resource 2.Title: Projected 21st century trends in hydroclimatology of the Tahoe basin.Journal: Climatic Change.Authors: Robert Coats1, Mariza Costa-Cabral, John Riverson, John Reuter, Goloka Sahoo, Geoffrey Schladow and Brent Wolfe

J. Kros, M.M. Bakker, P. Reidsma, A. Kanellopoulos, S. Jamal Alam, W. De Vries

Supplementary material to Impacts of agricultural changes in response to climate and socio economic change on nitrogen deposition in nature reserves.J. Kros, M.M. Bakker, P. Reidsma, A. Kanellopoulos, S. Jamal Alam, W. de Vries

Relationship of NDVI to Field-Collected Vegetation Data

Relationship of NDVI to field-collected vegetation data.A vegetation inventory on Ft. Benning was conducted on selected stands in 2007, and updated and completed in 2011. Although the forest inventory was not useful for the current study because it was

Video Shot List One

Video Shot List One.2010 U.S. Indonesian Ocean Exploration Partnership.File Name: 10index agu h.264 qt960.mov.Image Credits: NOAA Okeanos Explorer Program, INDEX-SATAL 2010.0:00 0:10 Start, Expedition Title. Background footage of the Institution for

Extreme Weather Conditions and the Impact on Society

Meteorological challenges 3.Extreme weather conditions and the impact on society.November 21st -22nd 2013., KRAŠ auditorium, Zagreb, Croatia.Is global warming a scientific certainty or political liability?.2. GEOLOGIC RECORDS OF CLIMATE CHANGES 4.2.1. Mesozoic and Cenozoic Eras 5

Identification of Ship's Movement

Identification of Ship's Movement

CBS/ISS/ET-DR&C/Doc.2.3(1), p.2.Submitted by the Secretariat.CBS/ISS/ET-DR&C/Doc., p.4.1. Bracknell, Offenbach and Toulouse are working in association with ECMWF and EUMETSAT on the development of a virtual Global Information System Center (VGISC). The

Weekly Report Drought Monitor / Snowpack Update s6

Weekly Snowpack and Drought Monitor Update Report.Weekly Report - Snowpack / Drought Monitor Update Date: 11 December, 2008.SNOTEL SNOWPACK AND PRECIPITATION SUMMARY.Snow: Snow-water equivalent percent to date continues to show low values across the West

Curriculum Vitae s477

CURRICULUM VITAE.Jared V. Goldstone.Research Specialist.Woods Hole Oceanographic Institution.B.S. Yale University, Chemistry, 1993.S.M. Massachusetts Institute of Technology, Inorganic Chemistry, 1996.Ph.D. MIT-WHOI Joint Program in Oceanography, Chemical Oceanography, 2002

Lab: Dewpoint Temperature

Measuring Dewpoint Temperature Lab.Ever wonder why water can be seen dripping down a cold bottle of water or pop, or why the grass is wet in the morning during the fall, or why after a thunderstorm the temperature of the air is cooler? This lab will help you find these answers!

Ice Mass & Sea Level Change Unit 5: Tide Gauge Exercise

Unit 5: Tide Gauge Exercise.Ice Mass & Sea Level Change Unit 5: Tide Gauge Exercise.Becca Walker and Leigh Stearns.In Units 3 and 4, you explored how changes in the Greenland Ice Sheet contribute to sea level rise. We use the term eustatic when referring

Atmospheric Water Vapor Transport and Precipitation

Revisiting forest impact on.atmospheric water vapor transport and precipitation.Anastassia M. Makarieva1*, Victor G. Gorshkov1 and Bai-Lian Li2.1Theoretical Physics Division, Petersburg Nuclear Physics Institute, 188300, Gatchina, St.Petersburg, Russia

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