Transborder Climate Webinars
Topic: Transborder Winter Forecasts, December 7, 2012.
1. Transborder Winter Forecast for Mexico
Martín Ibarra. CONAGUA-SMN, Mexico
Streaming recording link
Topic: Southwest Climate Change Assessment, November 9, 2012.
1. Southwest Climate Change Assessment Report: Impacts of Future Climate Change in the Southwest on Border Communities
Margaret Wilder & Gregg Garfin. School of Geography and Development & Udall Center for Studies in Public Policy, University of Arizona.
Streaming recording link
Topic: Watershed-Management and Ecosystem Services in Transboundary Environments, October 12, 2012.
1. Watershed management under climate change in cross-border environments
Laura Norman. U.S. Geological Survey. Web: https://profile.usgs.gov/lnorman
2. Ecosystem services across borders: a framework for transboundary conservation
Laura López Hoffman. School of Natural Resources and the Environment and the Udall Center for Public Policy Studies, University of Arizona.Web: http://udallcenter.arizona.edu/lauralhlab/
Species that migrate through wilderness areas deliver ecosystem services to people in faraway locations. International borders rarely coincide with natural ecological boundaries. Because neighboring countries often share ecosystems and species, they also share ecosystem services. As examples, the United States and Mexico share the regulating service of agave crop pollination by long-nosed bats; Mexican free-tailed bat helps control cotton crop pests in the southwestern United States and northern Mexico; and the North American monarch butterfly provides aesthetic value as a cultural service. The concept of ecosystem services, as articulated by the Millennium Ecosystem Assessment, could be used as an organizing principle for transboundary conservation, because it meets many of the criteria for successful transboundary policy. Ecosystem service can be used to frame conservation in terms of mutual interests between countries, consider a diversity of stakeholders, and provide a means for linking multiple services and assessing tradeoffs between uses of services.
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Topic: Cyclone Seasonal Forecasts, September 6, 2012.
1. Hurricane track forecast for the Eastern Pacific and Gulf of California
Luis M. Farfán. Centro de Investigación Científica y de Educación Superior de Ensenada, Baja California (CICESE).
2. The Gulf of Mexico and Atlantic Basin climatology of hurricanes
Barry D. Keim. Louisiana State Climatologist, and Graduate Director, Department of Geography and Anthropology, Louisiana State University
The official hurricane season for the Atlantic Basin (the Atlantic Ocean, the Caribbean Sea, and the Gulf of Mexico) is from 1 June to 30 November. The peak of the season is from mid-August to late October. However, deadly hurricanes can occur anytime in the hurricane season. We introduce SURGEDAT, a novel database that uses highly credible historical data to identify the location and height of maximum storm surge levels associated with both mild and extreme tropical storm events.
Streaming recording link
Topic: Drought In The Border Region, March 5 2012.
1. U.S. Drought Recap: 2011-2012
Mark D Svoboda. Monitoring Program Area Leader, National Drought Mitigation Center (NDMC), University of Nebraska-Lincoln, USA
The information presented in the webinar was culled from a report by the NDMC (Brian Fuchs, Climatologist) as part of our annual drought review found within our electronic quarterly newsletter DroughtScape. Impact information was compiled by Denise Gutzmer, Impacts Specialist. Drought classifications are based on the U.S. Drought Monitor.
2. Summary Of Drought In Northern Mexico
Martin Ibarra. Comisión Nacional del Agua (CONAGUA), Mexico.
The spatial distribution of rainfall in 2011 showed marked differences between regions. The wettest areas with rainfall above 1500 mm were located south of 22 ° N in portions of Nayarit, Colima, Guerrero, Veracruz, Tabasco and Chiapas. In contrast rainfall to 50% of normal or less occurred from central regions to the north, northeast and northwest, areas with rainfall less than 25% of normal were observed in Coahuila, Chihuahua, Durango and Baja California.
Streaming recording link
Topic: Organization Networks, March 30 2012.
3. Network On Hydrometeorolgical And Climatic Related Disasters (REDESClim)
Tereza Cavazos. Centro de Investigación Científica y de Educación Superior de Ensenada (CICESE), Baja California, Mexico.
REDESClim is a research network formed in 2011, and supported by the Mexican National Council of Science and Technology (CONACYT). REDESClim is an effort by the academic community to enhance the capacity of Mexico's response to hydrometeorological disasters and climate events. The network seeks to combine the collaboration of researchers, technologists, entrepreneurs, politicians and society to advance solutions to disasters associated with natural disasters in Mexico.
4. The Desert Landscape Conservation Cooperative (DESERT LCC)
Jeremey J. Mikrut. US Bureau of Reclamation-Desert Landscape Conservation Cooperative.
The Desert LCC encompasses portions of five states in the U.S. and ten states in Mexico. The Desert LCC Steering Committee consists of government and non-governmental entities in both the U.S. and Mexico. The Steering Committee identified science priorities for 2012 that fall into 11 topics areas, such as Water, Wildlife and Plant Populations, and Soils. One of the primary goals is to collaborate across agencies and organizations in order to address the science needs that are shared by partners.
Streaming recording link
Topic: Drought Risk Management and Monsoon season. April 30, 2012
5. Use of climate information for drought risk management in Mexico
Carolina Neri. Instituto de Geografía, Universidad Nacional Autónoma de México
A case study on drought planning in Mexico, which characterizes the vulnerability of water user groups, particularly in Sonora, has been useful in identifying the type of climate information needed by decision makers. This information will be included in a proposal to develop a drought early warning system for Mexico. Researchers at the Instituto de Geografía, Universidad Nacional Autónoma de México (UNAM), have initiated a project that focuses on reorienting drought policy from drought response to drought mitigation and preparedness, in collaboration with the Mexican government and stakeholders.
6. Introduction to the Monsoon season in the US Southwest
John J Brost. NOAA National Weather Service Tucson Arizona
The North American monsoon, variously known as the Southwest United States monsoon, the Mexican monsoon, or the Arizona monsoon, is experienced as a pronounced increase in rainfall from an extremely dry June to a rainy July over large areas of the southwestern United States and northwestern Mexico. These summer rains typically last until mid-September when a drier regime is reestablished over the region. Geographically, the monsoon precipitation region is centered over the Sierra Madre Occidental in the Mexican states of Sinaloa, Durango, Sonora and Chihuahua.
Streaming recording link
Topic: Monsoon Forecasts And Research, June 21 2012.
7. Monsoon forecast for Arizona with emphasis on the border region
John J Brost. NOAA National Weather Service Tucson Arizona
Deeper moisture from the south is expected to move into the state over the next couple of days. The best chances are in southeastern Arizona and that could definately enhance activity for us in the Valley in the way of outflow winds and dust and also storm development. Wednesday, looks to be most active during the morning and early afternoon hours with storm chances tapering during the evening just in time for 4th of July fireworks displays. The extra humidity and clouds will drop temperatures on Wednesday into the mid 90s.
8. The monsoon system in Mexico
Ernesto Dos Santos Caetano. Instituto de geografía, Universidad Nacional Autónoma de México (UNAM)
Mexican monsoon is associated to precipitation patterns that combines typical of the North American monsoon and large-scale mid-latitude cyclones with thunderstorms which have very different spatial/temporal distribution characteristics. The difficulty in understanding the variability of summertime convective activity in the southwestern U.S. and northwestern Mexico results from the complex interactions between atmospheric circulation features at both the synoptic and mesoscale and the extremely varied topography. The larger-scale atmospheric motions may control the distribution of water vapor and the general stability or instability in the atmosphere. Local topographic effects are critical to the geographic and even temporal distribution of convective activity.
Streaming recording link
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