{"id":25,"date":"2025-01-17T10:56:13","date_gmt":"2025-01-17T10:56:13","guid":{"rendered":"https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/?page_id=25"},"modified":"2026-01-15T14:14:09","modified_gmt":"2026-01-15T14:14:09","slug":"validation-of-the-method","status":"publish","type":"page","link":"https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/index.php\/validation-of-the-method\/","title":{"rendered":"Outcomes"},"content":{"rendered":"\n<p class=\"has-text-align-left\">The WAPOSAL project produced results of crucial importance for the extraction of wave resources along many coasts. The developed WAPOSAL method provides the wave power density with uncertainties ranging from 1.5% to 9% (Final Report, Section 8).\u00a0An example is shown in Figure 6 for the Mediterranean. The highest uncertainty is found in the Adriatic Sea and nearby coasts. <\/p>\n\n\n\n<p>The WAPOSAL database is available at:<\/p>\n\n\n\n<p><a href=\"https:\/\/esa-earthcode.github.io\/tutorials\/waposal\">https:\/\/esa-earthcode.github.io\/tutorials\/waposal<\/a><\/p>\n\n\n\n<p>Figure 2 illustrates the along-track distribution of wave power density in the North of Spain using Sentinel-3 A\/B.&nbsp;<\/p>\n\n\n\n<p class=\"has-text-align-left\"><\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"467\" src=\"https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/05\/Diciembres7anos-2-1024x467.jpg\" alt=\"\" class=\"wp-image-285\" srcset=\"https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/05\/Diciembres7anos-2-1024x467.jpg 1024w, https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/05\/Diciembres7anos-2-300x137.jpg 300w, https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/05\/Diciembres7anos-2-768x350.jpg 768w, https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/05\/Diciembres7anos-2-1536x701.jpg 1536w, https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/05\/Diciembres7anos-2-2048x934.jpg 2048w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/figure>\n\n\n\n<p class=\"has-text-align-center\">Figure 2. Average Wave Power Density along-track Sentinel-3 A\/B (2016-2023) for the Spain Atlantic coast (all December).<\/p>\n\n\n\n<p>The influence of ocean currents on the wave energy flux is one of the subjects that deserves attention. Figure 3 shows a comparison along-track (CryoSat-2 mission) between the ocean current (IBI product) and the wave power density (top panels). The simultaneous wind and wave fields (bottom panels) are taken from the ERA5 reanalysis. The comparison shows a high correlation (Correlation Coefficient = 0.96) between the current and the wave power density and that the current can influence the wave power density.<\/p>\n\n\n\n<figure class=\"wp-block-image aligncenter size-large is-resized\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"547\" src=\"https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/04\/RES_CS_OFFL_SIR1SAR_FR_20210318T232630_20210318T232822_D001_WavePower-1024x547.jpg\" alt=\"\" class=\"wp-image-228\" style=\"width:545px;height:auto\" srcset=\"https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/04\/RES_CS_OFFL_SIR1SAR_FR_20210318T232630_20210318T232822_D001_WavePower-1024x547.jpg 1024w, https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/04\/RES_CS_OFFL_SIR1SAR_FR_20210318T232630_20210318T232822_D001_WavePower-300x160.jpg 300w, https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/04\/RES_CS_OFFL_SIR1SAR_FR_20210318T232630_20210318T232822_D001_WavePower-768x410.jpg 768w, https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/04\/RES_CS_OFFL_SIR1SAR_FR_20210318T232630_20210318T232822_D001_WavePower-1536x820.jpg 1536w, https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/04\/RES_CS_OFFL_SIR1SAR_FR_20210318T232630_20210318T232822_D001_WavePower-2048x1093.jpg 2048w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/figure>\n\n\n\n<p>Figure 3. Comparison of the wave power density and ocean current along the CrysoSat-2 track in the Gulf of Lyon, Mediterranean. Date: 18 March 2021.<\/p>\n\n\n\n<p><strong>Validation<\/strong> <strong>of the Gommenginger method<\/strong><\/p>\n\n\n\n<p class=\"has-text-align-left\">To obtain the wave period necessary for estimating the wave power density, we apply and improve the empirical method of Gommenginger et al. (2003), assessed at 124 locations utilizing &#8220;real&#8221; wave buoys (82) and ERA5 &#8220;virtual&#8221; wave buoys (42) for eleven regions shown in Figure 1. The Mediterranean Sea is displayed below as an example in Figure 4.<\/p>\n\n\n\n<p class=\"has-text-align-center\"><\/p>\n\n\n\n<figure class=\"wp-block-image aligncenter size-large is-resized\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"412\" src=\"https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/01\/Mediterranep_VF_100-7-1024x412.jpg\" alt=\"\" class=\"wp-image-130\" style=\"width:529px;height:auto\" srcset=\"https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/01\/Mediterranep_VF_100-7-1024x412.jpg 1024w, https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/01\/Mediterranep_VF_100-7-300x121.jpg 300w, https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/01\/Mediterranep_VF_100-7-768x309.jpg 768w, https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/01\/Mediterranep_VF_100-7.jpg 1100w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/figure>\n\n\n\n<p class=\"has-text-align-center\">Figure&nbsp;4.&nbsp;The&nbsp;<em>Mediterranean Sea and the location of wave buoys.&nbsp;<\/em><\/p>\n\n\n\n<figure class=\"wp-block-image aligncenter size-full is-resized\"><img loading=\"lazy\" decoding=\"async\" width=\"954\" height=\"502\" src=\"https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/04\/image.png\" alt=\"\" class=\"wp-image-240\" style=\"width:452px;height:auto\" srcset=\"https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/04\/image.png 954w, https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/04\/image-300x158.png 300w, https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/04\/image-768x404.png 768w\" sizes=\"auto, (max-width: 954px) 100vw, 954px\" \/><\/figure>\n\n\n\n<p class=\"has-text-align-left\">Figure 5.&nbsp;<em>Scatter plots for significant wave height (m) (left) and wave period Tz (seconds) (right) for the wave buoy 6100106<\/em>&nbsp;in the Western Mediterranean&nbsp;and&nbsp;<em>Ancona<\/em>, Italy.<\/p>\n\n\n\n<p>Figure 6. <em>Uncertainty of Wave Power Density in the Mediterranean Sea (2007-2022).<\/em><em style=\"caret-color: rgb(0, 0, 0); color: rgb(0, 0, 0); text-align: start; white-space: normal;\"><\/em><\/p>\n\n\n\n<figure class=\"wp-block-gallery has-nested-images columns-default is-cropped wp-block-gallery-1 is-layout-flex wp-block-gallery-is-layout-flex\">\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"792\" height=\"444\" data-id=\"302\" src=\"https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/08\/Screenshot-2025-08-19-at-11.29.32.png\" alt=\"\" class=\"wp-image-302\" srcset=\"https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/08\/Screenshot-2025-08-19-at-11.29.32.png 792w, https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/08\/Screenshot-2025-08-19-at-11.29.32-300x168.png 300w, https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/08\/Screenshot-2025-08-19-at-11.29.32-768x431.png 768w\" sizes=\"auto, (max-width: 792px) 100vw, 792px\" \/><\/figure>\n<\/figure>\n\n\n\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"795\" height=\"445\" src=\"https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/08\/Screenshot-2025-08-19-at-11.32.49.png\" alt=\"\" class=\"wp-image-305\" srcset=\"https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/08\/Screenshot-2025-08-19-at-11.32.49.png 795w, https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/08\/Screenshot-2025-08-19-at-11.32.49-300x168.png 300w, https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/08\/Screenshot-2025-08-19-at-11.32.49-768x430.png 768w\" sizes=\"auto, (max-width: 795px) 100vw, 795px\" \/><\/figure>\n\n\n\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"799\" height=\"453\" src=\"https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/08\/Screenshot-2025-08-19-at-11.39.33.png\" alt=\"\" class=\"wp-image-306\" srcset=\"https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/08\/Screenshot-2025-08-19-at-11.39.33.png 799w, https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/08\/Screenshot-2025-08-19-at-11.39.33-300x170.png 300w, https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2025\/08\/Screenshot-2025-08-19-at-11.39.33-768x435.png 768w\" sizes=\"auto, (max-width: 799px) 100vw, 799px\" \/><\/figure>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"578\" src=\"https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2026\/01\/Local_Variability-1024x578.png\" alt=\"\" class=\"wp-image-316\" srcset=\"https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2026\/01\/Local_Variability-1024x578.png 1024w, https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2026\/01\/Local_Variability-300x169.png 300w, https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2026\/01\/Local_Variability-768x433.png 768w, https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/wp-content\/uploads\/2026\/01\/Local_Variability.png 1053w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/figure>\n","protected":false},"excerpt":{"rendered":"<p>The WAPOSAL project produced results of crucial importance for the extraction of wave resources along many coasts. The developed WAPOSAL method provides the wave power density with uncertainties ranging from 1.5% to 9% (Final Report, Section 8).\u00a0An example is shown in Figure 6 for the Mediterranean. The highest uncertainty is found in the Adriatic Sea [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":1,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-25","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/index.php\/wp-json\/wp\/v2\/pages\/25","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/index.php\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/index.php\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/index.php\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/index.php\/wp-json\/wp\/v2\/comments?post=25"}],"version-history":[{"count":65,"href":"https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/index.php\/wp-json\/wp\/v2\/pages\/25\/revisions"}],"predecessor-version":[{"id":324,"href":"https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/index.php\/wp-json\/wp\/v2\/pages\/25\/revisions\/324"}],"wp:attachment":[{"href":"https:\/\/waposal.tecnico.ulisboa.pt\/~waposal.daemon\/index.php\/wp-json\/wp\/v2\/media?parent=25"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}