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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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