BALTEX Phase II 2003 â 2012. Science Framework and ...
BALTEX Phase II 2003 â 2012. Science Framework and ...
BALTEX Phase II 2003 â 2012. Science Framework and ...
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<strong>BALTEX</strong> <strong>Phase</strong> <strong>II</strong> <strong>Science</strong> <strong>Framework</strong> <strong>and</strong> Implementation Strategy 51<br />
On the other h<strong>and</strong>, research needs knowledge from stakeholders <strong>and</strong> decision makers, e.g. detailed<br />
information on several environmental variables, which serve as input to models are needed.<br />
Furthermore plausible <strong>and</strong> possible perspectives for future changes of l<strong>and</strong> use, river regulations,<br />
regional emissions of aerosols <strong>and</strong> other regional or local agents influencing the regional <strong>and</strong> local<br />
climate are needed for a realistic construction of projections <strong>and</strong> scenarios. Stakeholders shall also be<br />
encouraged to provide scenarios of other anthropogenic factors (e.g., release of harmful substances),<br />
which will be acting on the Baltic Sea environment (e.g., ecosystem functioning) in conjunction or in<br />
addition to climate forcing <strong>and</strong> change. This latter aspect is important especially given extensions of<br />
<strong>BALTEX</strong> data <strong>and</strong> modelling studies beyond the physical climate system.<br />
In the following section, examples of <strong>BALTEX</strong> research with a high potential for applications – <strong>and</strong><br />
therefore stakeholder involvement – will be given.<br />
5.3. Examples of <strong>BALTEX</strong> Research with a high Application Potential<br />
5.3.1. Adaptation of Security Infrastructure<br />
The full evaluation of long-term observations of rainfall, river discharge or levels, snow pack duration<br />
<strong>and</strong> snow water equivalent, lake- <strong>and</strong> sea-ice duration <strong>and</strong> thickness offers not only an assessment of<br />
observed changes in variability <strong>and</strong> thus extremes, but – in conjunction with climate change<br />
projections - also allows a careful interpretation of projection of changes for the coming few decades<br />
as basis of the adaptation of security infrastructure like dykes <strong>and</strong> dams <strong>and</strong> its planning. <strong>BALTEX</strong><br />
scientists will establish contact <strong>and</strong> cooperation with panning authorities, preferably in a dedicated<br />
working group on “Infrastructure Adaptation” to changed climate variability with emphasis on water<br />
cycle parameters <strong>and</strong> the coming decades. Participation of particularly scientists developing coupled<br />
model systems is envisaged, after the coupled models have been validated with observed variability<br />
changes <strong>and</strong> have become useful tools for the projection of future extremes in the water cycle.<br />
5.3.2. Sea Level Variability <strong>and</strong> Change Estimates for Coastal Zone Management<br />
The joint evaluation of all observations at sea level gauges in <strong>and</strong> around the Baltic Sea basin will give<br />
not only mean sea level fall or rise but also wind-driven variability. This knowledge constitutes one of<br />
the main cornerstones for coastal zone management. <strong>BALTEX</strong> will establish cooperation with other<br />
programmes such as LOICZ (see Chapter 10.6), <strong>and</strong> with relevant management authorities in order to<br />
maintain a multidisciplinary discussion platform for the development of strategies for coastal zone<br />
management based on regionalized sea level variability <strong>and</strong> change. In addition to topics like coastal<br />
defence this should involve also consequences of changes in the physical system for ecosystems.<br />
5.3.3. Prediction of Floods, Snow Cover <strong>and</strong> Hydropower Potential<br />
The models used for the projection of regional climate change can also be used for improved<br />
forecasting of floods, snowfall, snowmelt etc., if driven by global forecasting models, e.g. from the<br />
European Centre for Medium-Range Weather Forecasts (ECMWF). This allows many new<br />
applications for meteorological <strong>and</strong> hydrological services that participate in <strong>BALTEX</strong> <strong>Phase</strong> <strong>II</strong>.<br />
Because the starting fields for the forecasts need information about near surface ocean structure as<br />
well as soil <strong>and</strong> groundwater storage growing with the forecast time scale, this aspect of the<br />
application of <strong>BALTEX</strong> <strong>Phase</strong> <strong>II</strong> results needs also input from the developing upper ocean observing<br />
system in the North Atlantic. User will be addressed <strong>and</strong> cooperation will be established, whenever<br />
improvements have become evident with a potential for rapid application. However, their full potential<br />
can only be exploited if seasonal predictions of climate anomalies show more skill for the Baltic Sea<br />
basin. Should such skill emerge during <strong>BALTEX</strong> <strong>Phase</strong> <strong>II</strong>, contacts to insurance companies,<br />
distributors of oil, hydropower companies operating large reservoirs <strong>and</strong> authorities responsible for<br />
water supply, to name just a few, should be established jointly with meteorological <strong>and</strong> hydrological<br />
services.<br />
5.3.4. Reduction of the Eutrophication of the Baltic Sea<br />
Discharge of nutrients into the Baltic Sea by rivers <strong>and</strong> deposition of nitrogen fertilisers from the<br />
atmosphere have led to eutrophication of large parts of the Baltic Sea. The coupled regional models