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	<title type="text">--  Crete Region</title>
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	<id>http://www.envistaweb.com/leddris/crete/crete-region-93346</id>
	<updated>2014-11-28T09:56:09+00:00</updated>
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	<entry>
		<title>Crete Socio-Ecological System (SES)</title>
		<link rel="alternate" type="text/html" href="http://www.envistaweb.com/leddris/crete/crete-region-93346/286-crete-socio-ecological-system-ses-higher-spatial-levels"/>
		<published>2012-09-07T06:32:44+00:00</published>
		<updated>2012-09-07T06:32:44+00:00</updated>
		<id>http://www.envistaweb.com/leddris/crete/crete-region-93346/286-crete-socio-ecological-system-ses-higher-spatial-levels</id>
		<author>
			<name>Jane Brandt</name>
			<email>medesdesire@googlemail.com</email>
		</author>
		<summary type="html">&lt;div class=&quot;feed-description&quot;&gt;&lt;table border=&quot;0&quot;&gt;
&lt;tbody&gt;
&lt;tr&gt;
&lt;td style=&quot;width: 15%;&quot; valign=&quot;top&quot;&gt;&lt;em&gt;Authors: &lt;/em&gt;&lt;/td&gt;
&lt;td valign=&quot;top&quot;&gt;&lt;em&gt;Constantinos Kosmas, Mina Karamesouti, Thanasis Kizos, Katerina Kounalaki, Minas Metaxakis&lt;/em&gt;&lt;/td&gt;
&lt;/tr&gt;
&lt;tr&gt;
&lt;td valign=&quot;top&quot;&gt;&lt;em&gt;Editors:&lt;/em&gt;&lt;/td&gt;
&lt;td valign=&quot;top&quot;&gt;&lt;em&gt;Alexandros Kandelapas, Vassilis Koutsoukos, Jane Brandt&lt;/em&gt;&lt;/td&gt;
&lt;/tr&gt;
&lt;/tbody&gt;
&lt;/table&gt;
{xtypo_alert}Editor's note 26Nov12: Source D131-2.2{/xtypo_alert}  
&lt;table border=&quot;0&quot;&gt;
&lt;tbody&gt;
&lt;tr&gt;
&lt;td&gt;<span class="tooltips-link " title="::&lt;img src=&quot;images/com_fwgallery/files/62/fig2002.jpg&quot; /&gt;&lt;br /&gt;Location of study site of Crete"> &lt;img src=&quot;images/com_fwgallery/files/62/fig2002.jpg&quot; width=&quot;250&quot; /&gt;</span>&lt;/td&gt;
&lt;td&gt;
&lt;p&gt;&lt;strong&gt;Location&lt;/strong&gt;&lt;/p&gt;
&lt;p&gt;The region of Crete is bordered to the north by the Sea of Crete and to the south by the Libyan Sea, covering an area of 8336 km². It is divided in four prefectures/ regional units: Chania, Rethymnon, Heraklion and Lassithi, with a total of 24 municipalities. Crete is a rugged mountainous island with high variation in altitude within relatively short distance.&lt;/p&gt;
&lt;/td&gt;
&lt;/tr&gt;
&lt;/tbody&gt;
&lt;/table&gt;
&lt;p&gt;&lt;strong&gt;Climate&lt;/strong&gt;&lt;/p&gt;
&lt;p&gt;The climate of Crete is sub-humid Mediterranean with humid and relatively cold winters, dry and warm summers. However, climate characteristics show great vertical and horizontal spatial variability: distribution of rainfall during the year is highly irregular as is variation of the air temperature. The potential evapotranspiration (ETo) from 948mm to 1640 mm yr-¹.&lt;/p&gt;
&lt;p&gt;&lt;strong&gt;Soils and topography &lt;/strong&gt;&lt;/p&gt;
&lt;p&gt;Soils of Crete are generally stony with various contents of rock  fragments, a parameter that can have a great but variable effect on soil  water conservation and soil erosion, and are characterized as very well  drained. Soils are characterized by a variety parent materials such as  limestone, shale, marl, conglomerates, flysch and alluvial deposits.  Many soils are shallow or subsoil exhibit characteristics adversely  affecting biomass production such as bedrock. These characteristics  combined with the island’s predominantly steep terrain, contribute to  considerable soil erosion problems.&lt;/p&gt;
&lt;table style=&quot;width: 100%;&quot; align=&quot;center&quot; border=&quot;0&quot;&gt;
&lt;tbody&gt;
&lt;tr&gt;
&lt;td align=&quot;center&quot;&gt;{tip&amp;nbsp;&lt;img src=&quot;images/com_fwgallery/files/62/fig2009.jpg&quot; /&gt;&lt;br /&gt;Spatial distribution of soil orders in the island of Crete.&lt;em&gt; Source: (LEDDRA project)&lt;/em&gt;}&amp;nbsp;&lt;img src=&quot;images/com_fwgallery/files/62/fig2009.jpg&quot; width=&quot;300&quot; /&gt;{/tip}&lt;/td&gt;
&lt;td align=&quot;center&quot;&gt;&lt;em&gt;&lt;/em&gt;{tip&lt;img src=&quot;images/com_fwgallery/files/62/fig2007a.jpg&quot; /&gt;&lt;br /&gt;Spatial distribution of aspect classes in the island of Crete}&lt;img src=&quot;images/com_fwgallery/files/62/fig2007a.jpg&quot; width=&quot;300&quot; /&gt;{/tip}&lt;br /&gt;&lt;/td&gt;
&lt;/tr&gt;
&lt;/tbody&gt;
&lt;/table&gt;
&lt;strong&gt;Hydrology&lt;/strong&gt;
&lt;p&gt;Crete is covered by a dense hydrological network with many water   channels. Although due to its dry climate, the island has limited water   resources, it has several ponds, natural or not, which constitute also   very important wildlife reserves.&lt;/p&gt;
&lt;table style=&quot;width: 100%;&quot; align=&quot;center&quot; border=&quot;0&quot;&gt;
&lt;tbody&gt;
&lt;tr&gt;
&lt;td align=&quot;center&quot;&gt;{tip&amp;nbsp;&lt;img src=&quot;images/com_fwgallery/files/62/fig2017.jpg&quot; /&gt;&lt;br /&gt;Location of main water reservoirs of Crete. &lt;em&gt;Source: LEDDRA project&lt;/em&gt;}&amp;nbsp;&lt;img src=&quot;images/com_fwgallery/files/62/fig2017.jpg&quot; width=&quot;300&quot; /&gt;{/tip}&lt;/td&gt;
&lt;td align=&quot;center&quot;&gt;<span class="tooltips-link -img" title="&lt;img src=&quot;images/com_fwgallery/files/62/fig2018.jpg&quot; /&gt;&lt;br /&gt;Spatial distribution of main ecosystems in Crete defined according to &lt;br /&gt;Millennium Ecosystem Assessment Reporting Categories. &lt;em&gt;Source: LEDDRA project&lt;/em&gt;:: ">&amp;nbsp;&lt;img src=&quot;images/com_fwgallery/files/62/fig2018.jpg&quot; width=&quot;300&quot; /&gt;</span>&lt;/td&gt;
&lt;/tr&gt;
&lt;/tbody&gt;
&lt;/table&gt;
&lt;p&gt;&lt;strong&gt;Ecosystems and land use&lt;br /&gt;&lt;/strong&gt;&lt;/p&gt;
&lt;p&gt;The majority of ecosystems identified in the island of Crete are   cultivated (42%), dry lands (39.3%) and mountains (11.7%). Protected   areas cover about 45.4% of the island, 91.9% of which are characterized   for their unique biodiversity. Based on the CORINE2000 land   classification the major land cover types are agricultural areas (olive   groves cover 23.3% of the island) and forests and semi-natural areas   (Sclerophyllous vegetation covering 23.7%).&lt;strong&gt;&lt;em&gt; &lt;br /&gt;&lt;/em&gt;&lt;/strong&gt;&lt;/p&gt;
&lt;p&gt;&lt;strong&gt;Particular LEDD issues in Crete&lt;/strong&gt;&lt;/p&gt;
&lt;p&gt;The main LEDD problems existing in the island of Crete are:&lt;/p&gt;
&lt;ol style=&quot;list-style-type: lower-alpha;&quot;&gt;
&lt;li&gt;soil erosion&lt;/li&gt;
&lt;li&gt;soil salinization&lt;/li&gt;
&lt;li&gt;over-exploitation of natural resources related of intensive farming, extensive use of agro-chemicals, expansion of irrigation and the increase in the number of animals grazing the land&lt;/li&gt;
&lt;li&gt;water stress and &lt;/li&gt;
&lt;li&gt;land desertification related to the exhaustion of land productivity, available water reserves and irrational human actions.&lt;/li&gt;
&lt;/ol&gt;
&lt;p&gt;The main drivers of land degradation and desertification in Crete include various EU and national policies, the financial markets, climate variability, often exarcerbated by local social structures. Financial support under the CAP has accelerated intensification, specialisation and mechanisation in agriculture. In addition, the significant growth of the tourism sector has place additional strains on land resources.&lt;/p&gt;
&lt;p&gt;Land desertification in Crete has adverse environmental and social impacts including reduction in crop production and agricultural income, increase in water deficiency, proliferation of forest fires, loss of&amp;nbsp; biodiversity, land abandonment, changes in micro-climatic conditions, frequent flooding of lowland and migration of population from degraded areas.&lt;/p&gt;
&lt;div style=&quot;position: absolute; left: -10000px; top: 0px; width: 1px; height: 1px; overflow: hidden;&quot; class=&quot;mcePaste&quot; id=&quot;_mcePaste&quot;&gt;The region of Crete is bordered to the north by the Sea of Crete and to the south by the Libyan Sea, covering an area of 8336 km². It is divided in four prefectures/ regional units: Chania, Rethymnon, Heraklion and Lassithi, with a total of 24 municipalities. Crete is a rugged mountainous island with high variation in altitude within relatively short distance (Figure 1).&lt;/div&gt;&lt;/div&gt;</summary>
		<content type="html">&lt;div class=&quot;feed-description&quot;&gt;&lt;table border=&quot;0&quot;&gt;
&lt;tbody&gt;
&lt;tr&gt;
&lt;td style=&quot;width: 15%;&quot; valign=&quot;top&quot;&gt;&lt;em&gt;Authors: &lt;/em&gt;&lt;/td&gt;
&lt;td valign=&quot;top&quot;&gt;&lt;em&gt;Constantinos Kosmas, Mina Karamesouti, Thanasis Kizos, Katerina Kounalaki, Minas Metaxakis&lt;/em&gt;&lt;/td&gt;
&lt;/tr&gt;
&lt;tr&gt;
&lt;td valign=&quot;top&quot;&gt;&lt;em&gt;Editors:&lt;/em&gt;&lt;/td&gt;
&lt;td valign=&quot;top&quot;&gt;&lt;em&gt;Alexandros Kandelapas, Vassilis Koutsoukos, Jane Brandt&lt;/em&gt;&lt;/td&gt;
&lt;/tr&gt;
&lt;/tbody&gt;
&lt;/table&gt;
{xtypo_alert}Editor's note 26Nov12: Source D131-2.2{/xtypo_alert}  
&lt;table border=&quot;0&quot;&gt;
&lt;tbody&gt;
&lt;tr&gt;
&lt;td&gt;<span class="tooltips-link " title="::&lt;img src=&quot;images/com_fwgallery/files/62/fig2002.jpg&quot; /&gt;&lt;br /&gt;Location of study site of Crete"> &lt;img src=&quot;images/com_fwgallery/files/62/fig2002.jpg&quot; width=&quot;250&quot; /&gt;</span>&lt;/td&gt;
&lt;td&gt;
&lt;p&gt;&lt;strong&gt;Location&lt;/strong&gt;&lt;/p&gt;
&lt;p&gt;The region of Crete is bordered to the north by the Sea of Crete and to the south by the Libyan Sea, covering an area of 8336 km². It is divided in four prefectures/ regional units: Chania, Rethymnon, Heraklion and Lassithi, with a total of 24 municipalities. Crete is a rugged mountainous island with high variation in altitude within relatively short distance.&lt;/p&gt;
&lt;/td&gt;
&lt;/tr&gt;
&lt;/tbody&gt;
&lt;/table&gt;
&lt;p&gt;&lt;strong&gt;Climate&lt;/strong&gt;&lt;/p&gt;
&lt;p&gt;The climate of Crete is sub-humid Mediterranean with humid and relatively cold winters, dry and warm summers. However, climate characteristics show great vertical and horizontal spatial variability: distribution of rainfall during the year is highly irregular as is variation of the air temperature. The potential evapotranspiration (ETo) from 948mm to 1640 mm yr-¹.&lt;/p&gt;
&lt;p&gt;&lt;strong&gt;Soils and topography &lt;/strong&gt;&lt;/p&gt;
&lt;p&gt;Soils of Crete are generally stony with various contents of rock  fragments, a parameter that can have a great but variable effect on soil  water conservation and soil erosion, and are characterized as very well  drained. Soils are characterized by a variety parent materials such as  limestone, shale, marl, conglomerates, flysch and alluvial deposits.  Many soils are shallow or subsoil exhibit characteristics adversely  affecting biomass production such as bedrock. These characteristics  combined with the island’s predominantly steep terrain, contribute to  considerable soil erosion problems.&lt;/p&gt;
&lt;table style=&quot;width: 100%;&quot; align=&quot;center&quot; border=&quot;0&quot;&gt;
&lt;tbody&gt;
&lt;tr&gt;
&lt;td align=&quot;center&quot;&gt;{tip&amp;nbsp;&lt;img src=&quot;images/com_fwgallery/files/62/fig2009.jpg&quot; /&gt;&lt;br /&gt;Spatial distribution of soil orders in the island of Crete.&lt;em&gt; Source: (LEDDRA project)&lt;/em&gt;}&amp;nbsp;&lt;img src=&quot;images/com_fwgallery/files/62/fig2009.jpg&quot; width=&quot;300&quot; /&gt;{/tip}&lt;/td&gt;
&lt;td align=&quot;center&quot;&gt;&lt;em&gt;&lt;/em&gt;{tip&lt;img src=&quot;images/com_fwgallery/files/62/fig2007a.jpg&quot; /&gt;&lt;br /&gt;Spatial distribution of aspect classes in the island of Crete}&lt;img src=&quot;images/com_fwgallery/files/62/fig2007a.jpg&quot; width=&quot;300&quot; /&gt;{/tip}&lt;br /&gt;&lt;/td&gt;
&lt;/tr&gt;
&lt;/tbody&gt;
&lt;/table&gt;
&lt;strong&gt;Hydrology&lt;/strong&gt;
&lt;p&gt;Crete is covered by a dense hydrological network with many water   channels. Although due to its dry climate, the island has limited water   resources, it has several ponds, natural or not, which constitute also   very important wildlife reserves.&lt;/p&gt;
&lt;table style=&quot;width: 100%;&quot; align=&quot;center&quot; border=&quot;0&quot;&gt;
&lt;tbody&gt;
&lt;tr&gt;
&lt;td align=&quot;center&quot;&gt;{tip&amp;nbsp;&lt;img src=&quot;images/com_fwgallery/files/62/fig2017.jpg&quot; /&gt;&lt;br /&gt;Location of main water reservoirs of Crete. &lt;em&gt;Source: LEDDRA project&lt;/em&gt;}&amp;nbsp;&lt;img src=&quot;images/com_fwgallery/files/62/fig2017.jpg&quot; width=&quot;300&quot; /&gt;{/tip}&lt;/td&gt;
&lt;td align=&quot;center&quot;&gt;<span class="tooltips-link -img" title="&lt;img src=&quot;images/com_fwgallery/files/62/fig2018.jpg&quot; /&gt;&lt;br /&gt;Spatial distribution of main ecosystems in Crete defined according to &lt;br /&gt;Millennium Ecosystem Assessment Reporting Categories. &lt;em&gt;Source: LEDDRA project&lt;/em&gt;:: ">&amp;nbsp;&lt;img src=&quot;images/com_fwgallery/files/62/fig2018.jpg&quot; width=&quot;300&quot; /&gt;</span>&lt;/td&gt;
&lt;/tr&gt;
&lt;/tbody&gt;
&lt;/table&gt;
&lt;p&gt;&lt;strong&gt;Ecosystems and land use&lt;br /&gt;&lt;/strong&gt;&lt;/p&gt;
&lt;p&gt;The majority of ecosystems identified in the island of Crete are   cultivated (42%), dry lands (39.3%) and mountains (11.7%). Protected   areas cover about 45.4% of the island, 91.9% of which are characterized   for their unique biodiversity. Based on the CORINE2000 land   classification the major land cover types are agricultural areas (olive   groves cover 23.3% of the island) and forests and semi-natural areas   (Sclerophyllous vegetation covering 23.7%).&lt;strong&gt;&lt;em&gt; &lt;br /&gt;&lt;/em&gt;&lt;/strong&gt;&lt;/p&gt;
&lt;p&gt;&lt;strong&gt;Particular LEDD issues in Crete&lt;/strong&gt;&lt;/p&gt;
&lt;p&gt;The main LEDD problems existing in the island of Crete are:&lt;/p&gt;
&lt;ol style=&quot;list-style-type: lower-alpha;&quot;&gt;
&lt;li&gt;soil erosion&lt;/li&gt;
&lt;li&gt;soil salinization&lt;/li&gt;
&lt;li&gt;over-exploitation of natural resources related of intensive farming, extensive use of agro-chemicals, expansion of irrigation and the increase in the number of animals grazing the land&lt;/li&gt;
&lt;li&gt;water stress and &lt;/li&gt;
&lt;li&gt;land desertification related to the exhaustion of land productivity, available water reserves and irrational human actions.&lt;/li&gt;
&lt;/ol&gt;
&lt;p&gt;The main drivers of land degradation and desertification in Crete include various EU and national policies, the financial markets, climate variability, often exarcerbated by local social structures. Financial support under the CAP has accelerated intensification, specialisation and mechanisation in agriculture. In addition, the significant growth of the tourism sector has place additional strains on land resources.&lt;/p&gt;
&lt;p&gt;Land desertification in Crete has adverse environmental and social impacts including reduction in crop production and agricultural income, increase in water deficiency, proliferation of forest fires, loss of&amp;nbsp; biodiversity, land abandonment, changes in micro-climatic conditions, frequent flooding of lowland and migration of population from degraded areas.&lt;/p&gt;
&lt;div style=&quot;position: absolute; left: -10000px; top: 0px; width: 1px; height: 1px; overflow: hidden;&quot; class=&quot;mcePaste&quot; id=&quot;_mcePaste&quot;&gt;The region of Crete is bordered to the north by the Sea of Crete and to the south by the Libyan Sea, covering an area of 8336 km². It is divided in four prefectures/ regional units: Chania, Rethymnon, Heraklion and Lassithi, with a total of 24 municipalities. Crete is a rugged mountainous island with high variation in altitude within relatively short distance (Figure 1).&lt;/div&gt;&lt;/div&gt;</content>
		<category term="Crete Region" />
	</entry>
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