here - CEOP-HE
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4. <strong>CEOP</strong>-<strong>HE</strong>: Contributions and Synergies with International Activities<br />
<strong>CEOP</strong>-<strong>HE</strong>’s aims to provide an interdisciplinary and global vision of water cycle and climate<br />
dynamics and related processes in high elevation areas. To reach its goals, <strong>CEOP</strong>-<strong>HE</strong> will benefit<br />
from its affiliation with Ev-K2-CNR’s SHARE Project and also with <strong>CEOP</strong>/GEWEX activities.<br />
4.1 Interactions with other <strong>CEOP</strong> Elements<br />
Specific interactions and collaborations between <strong>HE</strong> and other <strong>CEOP</strong> Elements<br />
(http://monsoon.t.u-tokyo.ac.jp/ceop2/) were identified during discussions within a breakout<br />
session on <strong>HE</strong> held within the 2 nd <strong>CEOP</strong> Annual Meeting, and reconfirmed during the 3 rd <strong>CEOP</strong><br />
Annual Meeting, which took place on August 19-21, 2009, in Melbourne, Australia.<br />
In particular, collaboration will regard especially three main elements that directly influence or<br />
characterize high elevated areas, i.e. Regional Studies (RSs), Cross-Cutting Studies (CCRs) and<br />
Regional Hydroclimate Projects (RHPs).<br />
<strong>HE</strong> is included in the Regional Studies, of <strong>CEOP</strong> and the interactions with other <strong>CEOP</strong> elements<br />
could be based on adopting common strategies to cover energy and water budgets studies at global<br />
scale. In particular, some components of RS are complementary, like Cold Regions that studies the<br />
same processes as <strong>HE</strong> (e.g. the permafrost melting) but at different altitude. In addition, Semi-Arid<br />
and Monsoon Studies have strong affinities with high elevation areas. For these reasons, such<br />
interactions are expected to produce results of great interest.<br />
The second area of fruitful interaction was identified with CCRs, in particular, with three<br />
components. The first is the Water and Energy Budget Studies (WEBS) group, the second is<br />
Aerosols group, and the thirdis the Isotope Cross Cut Study (ICCS) group, Such cross-cutting<br />
studies could contribute considerably to knowledge on the water budget in high elevated areas,<br />
considering the fundamental role played by all these factors (water and energy budgets, aerosols<br />
and isotopes) in the individuation of mechanisms of monsoon circulation.<br />
The MAHASRI (Monsoon Asian Hydro-Atmosp<strong>here</strong> Scientific Research and Prediction Initiative),<br />
CPPA (Climate Prediction Program for the Americas) and NEESPI (Northern Eurasia Earth<br />
Science Partnership Initiative) are the main RHP activities which could interact with <strong>HE</strong>. Such<br />
interaction could have a key role in identifying representative case study areas. The research<br />
facilities available within the RHPs, the operative activities carried out at a meaningful level in<br />
terms of space and time, and the long experience of researchers, will be of crucial to support the <strong>HE</strong><br />
activity, especially in view of the opportunity of linking the different high altitude observations<br />
within a more complete context.<br />
<strong>CEOP</strong> case studies which are representative of high elevated areas, such as Western American<br />
Mountains, will also be taken into account. Joint activities will also be undertaken with the Model<br />
Studies group.<br />
4.1.1 Specific benefits obtained from interactions<br />
The interaction with other Regional Climate Foci is essential in the planned activities of the <strong>HE</strong><br />
Working Group. In particular, it will regard the following specific aspects:<br />
Cold Region Studies<br />
<strong>HE</strong> will require information on glacier retreat/extension over the studied high elevated regions and<br />
on the respective possible theory, if already proposed. Also required is a list of existing glaciers,<br />
snow cover and permafrost, as possible reference sites in high elevated areas, as well as of heavy<br />
snow events at <strong>HE</strong> during <strong>CEOP</strong>-Phase I (2003-2004) and <strong>CEOP</strong>-Phase II (2006-2010). Finally,<br />
snow cover and permafrost climatology details will be required for the expected high elevated<br />
<strong>CEOP</strong>-<strong>HE</strong><br />
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