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    Item type:EMFIG - EKBY Collection,
    A Simplistic Approach for Assessing Hydroclimatic Vulnerability of Lakes and Reservoirs with Regulated Superficial Outflow
    (2019-07-24)
    K. Demertzi
    ;
    D. Papadimos
    ;
    V. Aschonitis
    ;
    D. Papamichail
    This study proposes a simplistic model for assessing the hydroclimatic vulnerability of lakes/reservoirs (LRs) that preserve their steady-state conditions based on regulated superficial discharge (Qd) out of the LR drainage basin. The model is a modification of the Bracht-Flyr et al. method that was initially proposed for natural lakes in closed basins with no superficial discharge outside the basin (Qd = 0) and under water-limited environmental conditions {mean annual ratio of potential/reference evapotranspiration (ETo) versus rainfall (P) greater than 1}. In the proposed modified approach, an additional Qd function is included. The modified model is applied using as a case study the Oreastiada Lake, which is located inside the Kastoria basin in Greece. Six years of observed data of P, ETo, Qd, and lake topography were used to calibrate the modified model based on the current conditions. The calibrated model was also used to assess the future lake conditions based on the future climatic projections (mean conditions of 2061-2080) derived by 19 general circulation models (GCMs) for three cases of climate change (three cases of Representative Concentration Pathways: RCP2.6, RCP4.5 and RCP8.5). The modified method can be used as a diagnostic tool in water-limited environments for analyzing the superficial discharge changes of LRs under di erent climatic conditions and to support the design of new management strategies for mitigating the impact of climate change on (a) flooding conditions, (b) hydroelectric production, (c) irrigation/industrial/domestic use and (d) minimum ecological flows to downstream rivers. Hydrology 6(3), 61. https://doi.org/10.3390/hydrology6030061
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    Assessing lake vulnerability to climate change using the coupled MIKE SHE/MIKE 11 model: Case study of Lake Zazari in Greece. Paper presented at 11th World Congress on Water Resources and Environment (EWRA 2019) “Managing Water Resources for a Sustainable Future”. Madrid, Spain, 25-29 June 2019
    (2019-07-04)
    D. Papadimos
    If the worst predictions of general circulation models (GCMs) about climate change become true, then lakes will hardly manage to maintain their current conditions (Zhang et al. 2016) especially in regions, which have been identified as climate change hot spots such as the countries of Mediterranean Basin (Loizidou et al. 2016) from which Greece is of special interest since it has 54 lakes/reservoirs of 0.5 km2 minimum size. The hydrological models are important tools for assessing the water balance components of lakes and for supporting the design of water management strategies. Depending on the modelling purposes and the specific attributes of a lake, different types of models and different levels of model complexities can be selected, starting from complex models such as MIKE SHE (Abbott et al. 1986), WATLAC (Zhang 2011) or using simpler methods (Yang et al. 2018). The MIKE model is among the most integrated models and has been used in the past for similar cases (Singh et al. 2010), while in combination with the future climate projections of general circulation models (GCMs), can be used to investigate lake conditions under future climate scenarios. The aim of this study is to present an application for analyzing the vulnerability of a lake to climate change using the MIKE SHE/11 model using as a case study the Lake Zazari in Greece.
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    Item type:EMFIG - EKBY Collection,
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    Item type:EMFIG - EKBY Collection,
    Χάρτης Βαθυμετρίας λίμνης Χειμαδίτιδας
    (Ελληνικό Κέντρο Βιοτόπων-Υγροτόπων (ΕΚΒΥ), 2018-10-18)
    Α. Αποστολάκης
    ;
    Χ. Δουλγέρης
    Ο παρών χάρτης εκπονήθηκε στο πλαίσιο του Εθνικού Δικτύου Παρακολούθησης της ποιότητας και της ποσότητας των υδάτων των λιμνών (ΚΥΑ Αριθμ. οικ. 140384/2011) που υλοποιείται από το Ελληνικό Κέντρο Βιοτόπων - Υγροτόπων, υπό τον συντονισμό και επίβλεψη της Ειδικής Γραμματείας Υδάτων. Χρηματοδότηση: Ταμείο συνοχής και εθνικοί πόροι - Επιχειρησιακό Πρόγραμμα Υποδομές Μεταφορών, Περιβάλλον και Αειφόρος Ανάπτυξη 2014 - 2020. Προτεινόμενη βιβλιογραφική αναφορά: Αποστολάκης Α. και Χ. Δουλγέρης. 2017. Χάρτης Βαθυμετρίας λίμνης Χειμαδίτιδας. Ελληνικό Κέντρο Βιοτόπων-Υγροτόπων (ΕΚΒΥ). Κλίμακα 1:15.000.
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    Item type:EMFIG - EKBY Collection,
    Report on the development of the national assessment method for the ecological status of natural lakes in Greece, using the Biological Quality Element “Macrophytes” (Hellenic Lake Macrophytes-HeLM assessment method)
    (Greek Biotope/Wetland Centre (EKBY), 2018-08-01)
    V. Tsiaoussi
    This report discusses the development of the national ecological assessment method for Greek natural lakes, based on the Biological Quality Element (BQE) “macrophytes”. Due to lack of a common natural lake type within the Mediterranean Lake Geographical intercalibration Group, there has not been a Med GIG Intercalibration Exercise for macrophytes in natural lakes. As a result, there are neither proposed assessment methods with common boundaries within the Med GIG, nor proposed metrics for the assessment of lakes based on macrophytes. It is noted that at the Mediterranean Lake Phytoplankton GIG Intercalibration Report, Member States defined two common water body types (L-M5/7 and L-M8) for reservoirs but none for natural lakes. The operation of the Greek water monitoring network started in 2012, following the publication of a Joint Ministerial Decision in 2011. The development of the current assessment method, as described in this report, is based on the data from this national water monitoring network. In particular, 50 lake water bodies (including 26 reservoirs) have been included in the monitoring network, out of which 16 have been monitored for macrophytes during the 3-year period of 2013-2015. Eight of them are warm monomictic, deep natural lakes with mean depth >9m (GR-DNL), when the other eight are polymictic, shallow natural lakes with mean depth 3-9m (GR-SNL). In these 16 lakes, a total of 272 monitoring sites were established for sampling macrophytes, which resulted in an equal number of macrophytic sampling transects, the data of which have been added in the national dataset. Thirty six of these sites were revisited during the 3-year period, and a total of 308 measurements of maximum macrophytic colonization depth were made. On this national dataset, the most suitable lake macrophyte based assessment components proposed by WISER deliverables D3.2-1 (Kolada et al., 2009), D3.2-2 (Dudley et al., 2011) and D3.2-3 (Kolada et al., 2011) were tested, in various combinations, so as to reach a final form that can be used as a national assessment method for Greece. As already mentioned, this is the first effort to establish a national method, which may need additions and improvements in the future, as well as intercalibration exercises among Member States in the Mediterranean GIG.
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    Item type:EMFIG - EKBY Collection,
    Report on the application of phytoplankton index NMASRP for reservoirs in Greece
    (Greek Biotope/Wetland Centre (EKBY), 2018-08-01)
    V. Tsiaoussi
    Assessment methods had been intercalibrated for lake types LM 5/7 (deep siliceous reservoirs) and LM 8 (deep calcareous reservoirs) (de Hoyos et al. 2014). In the first round of IC that Greece participated, boundaries for individual phytoplankton metrics (chlorophyll-a, total biovolume, percentage of cyanobacteria, IGA and MedPTI) were agreed (using option 1 of IC) and formally included in the 200 8 EC Intercalibration Decision. During the second round of IC, national assessment methods based on the above metrics (NMASRP for Cyprus and Portugal, MASRP for Spain and NITMET for Italy) were intercalibrated for LM 5/7 and LM 8 types. Greece had not started the operation of the monitoring network at that time, and thus had not submitted its national assessment method for the second round of IC. The operation of the Greek monitoring network started in 2012, following the publication of a Joint Ministerial Decision in 2011. Fifty lake water bodies have been included in the monitoring network, out of which 15 are LM 5/7 and 5 are LM 8 reservoirs. The national phytoplankton assessment method applied for Greek LM 5/7 and LM 8 reservoirs is the New Mediterranean Assessment System for Reservoirs Phytoplankton (NMASRP), that has been intercalibrated in the Med GIG, as applied by Cyprus and Portugal (i.e. the metric percentage of cyanobacteria is replaced by the metric biovolume of cyanobacteria, in order to account for algal blooms) (de Hoyos et al. 2014). Spain uses MASRP (i.e., with the metric percentage of cyanobacteria). NMASRP addresses eutrophication pressure in Mediterranean reservoirs. This report does not discuss the development of new or revised ecological assessment method for phytoplankton according to finalized IC results, but the application of the existing NMASRP phytoplankton assessment method as intercalibrated in the Med GIG (including existing MEP values and EQRs), into the national dataset. NMASRP values are calculated as annual mean. This dataset contains data collected during the 2012-2015 sampling campaign, and in particular 53 NMASRP values for LM 5/7 and 18 NMASRP values for LM 8 reservoirs arising from 139 and 56 samplings, respectively.
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    Item type:EMFIG - EKBY Collection,
    Report on the development of the national method for the assessment of the ecological status of natural lakes in Greece, using the biological quality element “phytoplankton”
    (Greek Biotope/Wetland Centre (EKBY), 2018-08-01)
    V. Tsiaoussi
    This report discusses the development of a national method for the assessment of ecological status of natural lakes in Greece, based on the Biological Quality Element (BQE) “phytoplankton”; it is a revised version of the 2016 report, following comments by JRC and Intercalibration Review Panel experts. The main changes include an amendment to modNygaard index (exclusion of Centrales, see 2.1), the exclusion of a lake’s data from the reference dataset in order to avoid ircularity in the assessment, and construction of pressure response curves with phytoplankton and TP data from lake years 2014 and 2015. At the Mediterranean Lake Geographical Intercalibration Group, Member States defined two common water body types for reservoirs (L-M5/7 and L-M8). In spite of common efforts, within the Mediterranean GIG, there was no possibility to intercalibrate natural Mediterranean lakes because of the absence of common types with enough lakes. As a result, no assessment methods for phytoplankton of natural lakes have been intercalibrated within the Med GIG. The operation of the Greek water monitoring network started in 2012, following the publication of a Joint Ministerial Decision in 2011 and comprises 23 natural lakes. The development of the current assessment method, as described in this report, is based on the data from this national water monitoring network. Natural lakes in Greece are grouped into 3 types: 1) warm monomictic, deep natural lakes with mean depth >9 m (type GR-DNL, 7 lakes), 2) polymictic, shallow natural lakes with mean depth 3-9 m (type GR-SNL, 8 lakes), 3) very shallow lakes < 3 m (type GR-VSNL, 8 lakes).
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    Item type:EMFIG - EKBY Collection,
    Untitled
    (Φορέας Διαχείρισης Λιμνών Κορώνειας - Βόλβης, 2017-10-05)
    Μ. Δούρδα
    ;
    Μ. Κατσακιώρη
    ;
    Κ. Μπόλη
    Το εκπαιδευτικό υλικό αναδεικνύει, μέσα από σύγχρονες παιδαγωγικές μεθόδους και προσεγγίσεις, τη σημασία της προστατευόμενης περιοχής. Αποτελείται από σύντομο κείμενο παρουσίασης του Εθνικού Πάρκου, από παιδαγωγικές δραστηριότητες συνοδευόμενες από σχετικές οδηγίες για την υλοποίησή τους, καθώς και από ένα φύλλο αξιολόγησης του υλικού. Τα αντικείμενα μελέτης αρθρώνονται με τρόπο ώστε να συνθέτουν συνολικά τις διαφορετικές όψεις και διαστάσεις του Πάρκου (π.χ.γεωγραφία, βλάστηση, χλωρίδα, πανίδα, πολιτισμός, ανθρώπινες δραστηριότητες). Τα παιδιά εργάζονται, ατομικά ή ομαδικά, σύμφωνα με συγκεκριμένες γραπτές οδηγίες που περιέχονται στις δραστηριότητες και σύμφωνα με τις υποδείξεις και οδηγίες του εκπαιδευτή. Καθώς το υλικό απευθύνεται σε παιδιά ηλικίας 6-12 ετών (μεγάλο εύρος σε επίπεδο γνωστικό, ικανοτήτων και δεξιοτήτων), επιχειρήθηκε το εκπαιδευτικό υλικό να περιλαμβάνει δραστηριότητες που να καλύπτουν τις απαιτήσεις των παιδιών τόσο της μικρότερης, όσο και της μεγαλύτερης ηλικίας.
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    Item type:EMFIG - EKBY Collection,
    Κείμενα εκθεμάτων του Κέντρου Πληροφόρησης Εθνικού Πάρκου Κορώνειας-Βόλβης και Μακεδονικών Τεμπών
    (Φορέας Διαχείρισης Λιμνών Κορώνειας-Βόλβης, 2017-09-19)
    Γ. Πουλής
    ;
    Κ. Μπόλη
    ;
    Μ. Κατσακιώρη