{"id":1147,"date":"2022-04-11T14:36:30","date_gmt":"2022-04-11T12:36:30","guid":{"rendered":"https:\/\/mosj.no\/indikator\/climate\/atmosphere\/uv-i-ny-alesund\/"},"modified":"2026-01-21T15:18:14","modified_gmt":"2026-01-21T14:18:14","slug":"uv-in-ny-alesund","status":"publish","type":"bc_indicator","link":"https:\/\/mosj.no\/en\/indikator\/climate\/atmosphere\/uv-in-ny-alesund\/","title":{"rendered":"UV in Ny-\u00c5lesund"},"content":{"rendered":"\n<p class=\"has-sizing-small\">Last updated 21 January 2026<\/p>\n\n\n\n<p class=\"has-sizing-medium\">Excessive doses of ultraviolet (UV) radiation can damage the development and growth of plants and microorganisms, and cause, for example, sunburn and skin cancer in humans. Monitoring of UV radiation in Ny-\u00c5lesund started in 1996.<\/p>\n\n\n\n<div style=\"height:20px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"2560\" height=\"960\" src=\"https:\/\/mosj.no\/wp-content\/uploads\/2023\/01\/np078177-scaled.jpg\" alt=\"\" class=\"wp-image-62494\" srcset=\"https:\/\/mosj.no\/wp-content\/uploads\/2023\/01\/np078177-scaled.jpg 2560w, https:\/\/mosj.no\/wp-content\/uploads\/2023\/01\/np078177-300x113.jpg 300w, https:\/\/mosj.no\/wp-content\/uploads\/2023\/01\/np078177-1024x384.jpg 1024w, https:\/\/mosj.no\/wp-content\/uploads\/2023\/01\/np078177-768x288.jpg 768w, https:\/\/mosj.no\/wp-content\/uploads\/2023\/01\/np078177-1536x576.jpg 1536w, https:\/\/mosj.no\/wp-content\/uploads\/2023\/01\/np078177-2048x768.jpg 2048w, https:\/\/mosj.no\/wp-content\/uploads\/2023\/01\/np078177-684x257.jpg 684w\" sizes=\"auto, (max-width: 2560px) 100vw, 2560px\" \/><figcaption class=\"wp-element-caption\">The Zeppelin Observatory in Ny-\u00c5lesund. Photo: Ove Hermansen \/ NILU<\/figcaption><\/figure>\n<\/div>\n\n\n<div class=\"wp-block-group alignwide has-white-background-color has-background\"><div class=\"wp-block-group__inner-container is-layout-constrained wp-block-group-is-layout-constrained\">\n<h2 class=\"wp-block-heading has-text-align-center has-sizing-medium\">What is being monitored?<\/h2>\n\n\n\n<hr class=\"wp-block-separator has-text-color has-mosj-yellow-color has-alpha-channel-opacity has-mosj-yellow-background-color has-background\"\/>\n\n\n\n<h3 class=\"wp-block-heading has-text-align-center has-sizing-medium\">UV doses (ultraviolet radiation levels)<\/h3>\n\n\n\n<div style=\"height:50px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<div class=\"wdt-wrapper-chart-loader\" data-id=\"228\"\n     style=\"height: 400px;\">\n    <div class=\"wdt-main-item\">\n                <div class=\"wdt-chart-animated-background\" style=\"height: 100px\">\n            <div class=\"wdt-background-masker wdt-btn-divide-left wdt-chart-one\"><\/div>\n            <div class=\"wdt-background-masker wdt-btn-divide-left-2\"><\/div>\n            <div class=\"wdt-background-masker wdt-btn-divide-left-3\"><\/div>\n            <div class=\"wdt-background-masker wdt-btn-divide-left-4 wdt-chart-three\"><\/div>\n            <div class=\"wdt-background-masker wdt-btn-divide-left-5\"><\/div>\n            <div class=\"wdt-background-masker wdt-btn-divide-left-6\"><\/div>\n            <div class=\"wdt-background-masker wdt-btn-divide-left-7 \"><\/div>\n            <div class=\"wdt-background-masker wdt-btn-divide-left-8\"><\/div>\n        <\/div>\n        <div class=\"wdt-chart-animated-background\" style=\"height: 100px\">\n            <div class=\"wdt-background-masker wdt-btn-divide-left\"><\/div>\n            <div class=\"wdt-background-masker wdt-btn-divide-left-2 wdt-chart-two\"><\/div>\n            <div class=\"wdt-background-masker wdt-btn-divide-left-3\"><\/div>\n            <div class=\"wdt-background-masker wdt-btn-divide-left-4\"><\/div>\n            <div class=\"wdt-background-masker wdt-btn-divide-left-5 wdt-chart-four\"><\/div>\n            <div class=\"wdt-background-masker wdt-btn-divide-left-6\"><\/div>\n            <div class=\"wdt-background-masker wdt-btn-divide-left-7\"><\/div>\n            <div class=\"wdt-background-masker wdt-btn-divide-left-8\"><\/div>\n        <\/div>\n        <div class=\"wdt-chart-animated-background\" style=\"height: 100px\">\n            <div class=\"wdt-background-masker wdt-btn-divide-left\"><\/div>\n            <div class=\"wdt-background-masker wdt-btn-divide-left-2\"><\/div>\n            <div class=\"wdt-background-masker wdt-btn-divide-left-3\"><\/div>\n            <div class=\"wdt-background-masker wdt-btn-divide-left-4\"><\/div>\n            <div class=\"wdt-background-masker wdt-btn-divide-left-5\"><\/div>\n            <div class=\"wdt-background-masker wdt-btn-divide-left-6 wdt-chart-five\"><\/div>\n            <div class=\"wdt-background-masker wdt-btn-divide-left-7\"><\/div>\n            <div class=\"wdt-background-masker wdt-btn-divide-left-8\"><\/div>\n        <\/div>\n        <div class=\"wdt-chart-animated-background\" style=\"height: 100px\">\n            <div class=\"wdt-background-masker wdt-btn-divide-left\"><\/div>\n            <div class=\"wdt-background-masker wdt-btn-divide-left-2\"><\/div>\n            <div class=\"wdt-background-masker wdt-btn-divide-left-3\"><\/div>\n            <div class=\"wdt-background-masker wdt-btn-divide-left-4\"><\/div>\n            <div class=\"wdt-background-masker wdt-btn-divide-left-5\"><\/div>\n            <div class=\"wdt-background-masker wdt-btn-divide-left-6\"><\/div>\n            <div class=\"wdt-background-masker wdt-btn-divide-left-7\"><\/div>\n            <div class=\"wdt-background-masker wdt-btn-divide-left-8\"><\/div>\n        <\/div>\n        <div class=\"wdt-static-background\">\n            <div class=\"wdt-background-masker\"><\/div>\n        <\/div>\n    <\/div>\n<\/div>\n<style>\n    \n<\/style>    <script type=\"text\/javascript\">\n        if (typeof (wpDataCharts) == 'undefined') wpDataCharts = {};\n        wpDataCharts[228] = {\n            render_data: {\"wdtNumberFormat\":\"1\",\"options\":{\"title\":{\"text\":\"UV doses in Ny-\\u00c5lesund\",\"floating\":false,\"align\":\"center\"},\"series\":[{\"type\":\"\",\"name\":\"April dose\",\"color\":\"#040404\",\"label\":\"April dose\",\"orig_header\":\"aprildose\",\"data\":[22670,25411,22177,20921,24030,19435,19093,19327,17834,null,16741.5,20249,20425,23675,21006.5,17265,18615,19193,18659,18438,20176,19524,18984,16443,26321,20242,20222,17447,18495],\"yAxis\":0},{\"type\":\"\",\"name\":\"July dose\",\"color\":\"#35F43D\",\"label\":\"July 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(J\\\/m\\u00b2)\"},\"opposite\":true}],\"chart\":{\"backgroundColor\":\"\",\"borderWidth\":0,\"borderColor\":\"\",\"borderRadius\":0,\"zoomType\":\"x\",\"panning\":false,\"panKey\":\"shift\",\"plotBackgroundColor\":\"\",\"plotBackgroundImage\":\"\",\"plotBorderColor\":\"\",\"plotBorderWidth\":0,\"inverted\":false},\"subtitle\":{\"text\":\"\",\"align\":\"center\"},\"tooltip\":{\"enabled\":true,\"backgroundColor\":\"rgba(255,255,255,0.85)\",\"borderWidth\":\"1\",\"borderColor\":\"\",\"borderRadius\":\"3\",\"shared\":true,\"valuePrefix\":\"\",\"valueSuffix\":\"\"},\"legend\":{\"enabled\":true,\"backgroundColor\":\"\",\"title\":{\"text\":\"\"},\"layout\":\"horizontal\",\"align\":\"center\",\"verticalAlign\":\"bottom\",\"borderWidth\":\"0\",\"borderColor\":\"\",\"borderRadius\":\"0\"},\"exporting\":{\"enabled\":true,\"chartOptions\":{\"plotOptions\":{\"series\":{\"dataLabels\":{\"enabled\":false}}}},\"filename\":\"\",\"width\":\"\",\"buttons\":{\"contextButton\":{\"align\":\"right\",\"verticalAlign\":\"top\",\"symbolStroke\":\"#666\",\"text\":\"\"}}},\"credits\":{\"enabled\":true,\"href\":\"\",\"text\":\"Data: NILU\"}},\"type\":\"highcharts_line_chart\",\"height\":400},\n            engine: \"highcharts\",\n            type: \"highcharts_line_chart\",\n            title: \"UV doses in Ny-\u00c5lesund\",\n            container: \"wpDataChart_228\",\n            follow_filtering: 0,\n            wpdatatable_id: 229,\n            group_chart: 0        }\n    <\/script>\n\n    <div id=\"wpDataChart_228\" class=\"highcharts_line_chart\" style=\"width: 100%\"><\/div>\n\n\n\n\n<p class=\"has-sizing-mini\">The figure shows UV doses in Ny-\u00c5lesund from 1996. Data from 2005 are missing due to instrument calibration. The maximum daily UV dose, which occurs around May 1st, shows large variations from year to year. This is due to changes in cloud cover, the ozone layer, and\/or fresh snow on the ground. The highest UV dose in April was observed in 1997, the same year that record-low ozone values were recorded.<br>(<em>Cite these data: NILU (2026). UV doses in Ny-\u00c5lesund. Environmental monitoring of Svalbard and Jan Mayen (MOSJ). URL: https:\/\/mosj.no\/en\/climate\/atmosphere\/uv-ny-alesund.html<\/em>)<\/p>\n\n\n\n<div style=\"height:50px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<div class=\"wp-block-pb-accordion-item c-accordion__item js-accordion-item no-js\" data-initially-open=\"false\" data-click-to-close=\"true\" data-auto-close=\"false\" data-scroll=\"false\" data-scroll-offset=\"0\"><h2 id=\"at-11471\" class=\"c-accordion__title js-accordion-controller\" role=\"button\">Details on these data<\/h2><div id=\"ac-11471\" class=\"c-accordion__content\">\n<figure class=\"wp-block-table is-style-stripes\"><table><tbody><tr><td><strong>Last updated<\/strong><\/td><td>21 January 2026<\/td><\/tr><tr><td><strong>Update interval<\/strong><\/td><td>Yearly<\/td><\/tr><tr><td><strong>Next update<\/strong><\/td><td>October 2026<\/td><\/tr><tr><td><strong>Executive organization<\/strong><\/td><td><a href=\"https:\/\/www.nilu.com\/\" target=\"_blank\" rel=\"noreferrer noopener\">NILU<\/a><\/td><\/tr><tr><td><strong>Contact persons<\/strong><\/td><td><a href=\"https:\/\/www.nilu.com\/employee\/tove-svendby\/\" target=\"_blank\" rel=\"noreferrer noopener\">Tove Svendby<\/a><\/td><\/tr><\/tbody><\/table><\/figure>\n\n\n\n<h3 class=\"wp-block-heading\">Method<\/h3>\n\n\n\n<p class=\"has-sizing-medium\">GUV-511 is a filter instrument from Biospherical Instruments Inc., USA, which measures global surface irradiance in&nbsp;5 channels. There are&nbsp;4 channels&nbsp;in the UV area, with central wavelengths of&nbsp;305 nm, 313 nm,&nbsp;320 nm,&nbsp;340 nm&nbsp;and&nbsp;380 nm. The band width is&nbsp;ca 10 nm.<\/p>\n\n\n\n<p class=\"has-sizing-medium\">The instrument is temperature stabilised at 40\u00b0C and has a temporal resolution of 1 minute.<\/p>\n\n\n\n<p class=\"has-sizing-medium\">Using algorithms from Dahlback (1996), it is possible to calculate&nbsp;CIE&nbsp;doses, spectral UV from 290 to&nbsp;400 nm, total column ozone, UV ground albedo and cloud optical thickness.<\/p>\n\n\n\n<p class=\"has-sizing-medium\">The measuring method requires UV radiation and the measurements are more unreliable if the cloud cover is thick and the sun low. The measurements are most unreliable in the winter months (15 September&nbsp;to&nbsp;15 March) due to low solar intensity.<\/p>\n\n\n\n<h3 class=\"wp-block-heading\">Quality<\/h3>\n\n\n\n<p class=\"has-sizing-medium\">The GUV instrument is calibrated once a year against a mobile reference instrument. The Norwegian Radiation and Nuclear Safety Authority is responsible for calibrating the reference instrument.<\/p>\n<\/div><\/div>\n<\/div><\/div>\n\n\n\n<div style=\"height:50px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<h2 class=\"wp-block-heading\">Status and trend<\/h2>\n\n\n\n<p class=\"has-sizing-medium\">The ozone layer protects plants, animals and humans from harmful UV radiation from the sun.<\/p>\n\n\n\n<p class=\"has-sizing-medium\">In the 1980s and 1990s, gradual thinning of the ozone layer was observed in most parts of the world. The main reason was high emissions of ozone-depleting substances. In 1987 the Montreal Protocol, requiring the industrialised nations to reduce the emissions, was signed. The major focus on the ozone situation in the 1990s led to the initiation of several programmes to monitor ozone and UV radiation in many countries around the world.<\/p>\n\n\n\n<p class=\"has-sizing-medium\">Since the signing of the Montreal Protocol, emissions have been reduced by more than 95%. This seems to be having positive effects on the ozone layer. It is nevertheless vital to monitor the trend in UV radiation in the coming decades.<\/p>\n\n\n\n<p class=\"has-sizing-medium\">UV measurements in Ny-\u00c5lesund began in 1995, in a period when the ozone layer was at its thinnest. It should therefore be expected that UV radiation showed a tendency to decline in the years after 1997, in pace with the thickening of the ozone layer. However, it is difficult to draw such a conclusion from our measurements. This is chiefly because the cloud cover varies greatly from year to year and will affect the UV radiation just as much as a possible increase in ozone.<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Causal factors<\/h2>\n\n\n\n<p class=\"has-sizing-medium\">Ozone holes are caused by emissions of industrial chemicals, especially chlorofluorocarbons (CFCs).<\/p>\n\n\n\n<p class=\"has-sizing-medium\">The CFC gases, which are very stable on the Earth\u2019s surface, react effectively with the ozone in the stratosphere. Under the special geophysical conditions in the polar stratosphere, the gases trigger chemical processes which lead to the rapid breakdown of ozone.<\/p>\n\n\n\n<p class=\"has-sizing-medium\">In the early-1980s, a substantial reduction in the ozone layer over Antarctica was observed from September to November and the situation gradually deteriorated until the mid-1990s.<\/p>\n\n\n\n<p class=\"has-sizing-medium\">Normally, the highest ozone concentrations are found in the stratosphere at 10-25 kilometres up (in polar regions), but measurements from Antarctica showed that ozone concentrations at 12 to 20 kilometres were virtually zero in the Antarctic spring. The geographical extent of ozone depletion could also be measured far beyond the Antarctic continent.<\/p>\n\n\n\n<p class=\"has-sizing-medium\">This situation still arises from September to November each year and is termed the &#8220;Antarctic Ozone Hole&#8221;. As a consequence of the Antarctic Ozone Hole, UV radiation has increased to levels normally measured in middle latitudes.<\/p>\n\n\n\n<p class=\"has-sizing-medium\">This has raised questions surrounding the development of the UV level in the northern polar regions, but annual huge ozone holes are unlikely to arise in northern areas. This is mainly because the stratosphere in the north is warmer than in the south and the polar wind systems differ. The topography and meteorology in the Arctic are quite different from conditions in the Antarctic.<\/p>\n\n\n\n<p class=\"has-sizing-medium\">However, climate change is expected to lead to warming of the troposphere and cooling of the stratosphere. A colder stratosphere will give more frequent occurrences of polar stratospheric clouds (PSCs), which can give strong ozone depletion, called &#8220;mini-holes&#8221;, also in Arctic regions. Such ozone hole was observed in spring 2011 and 2020, for example.<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Consequences<\/h2>\n\n\n\n<p class=\"has-sizing-medium\">UV radiation is most important for health and the environment. As there is a close relationship between the thickness of the ozone layer and the UV radiation at ground level, a thinner ozone layer may have major environmental consequences.<\/p>\n\n\n\n<p class=\"has-sizing-medium\">Modelling implies that human-induced climate changes will reduce the temperature in the stratosphere and increase the formation of Polar Stratospheric (ice) Clouds (PSC, or nacreous clouds) in Arctic regions. This can lead to ozone depletion and a corresponding increase in UV radiation.<\/p>\n\n\n\n<p class=\"has-sizing-medium\">The thawing of polar ice may also put marine organisms at greater risk of exposure to UV. However, as there is a very complex link between stratospheric ozone and long-lived climate gases, the net effect on the ozone layer is uncertain.<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">About the monitoring<\/h2>\n\n\n\n<p class=\"has-sizing-medium\">Continuous measurements of stratospheric ozone and several halogenated greenhouse gases are conducted by NILU, as part of the Norwegian Environment Agency\u2019s program for Greenhouse gases, ozone layers, UV radiation and atmospheric pollution.<\/p>\n\n\n\n<p class=\"has-sizing-medium\">When interpreting the monitoring results, it is important to be aware that the strength of UV radiation at the surface depends on several factors.<\/p>\n\n\n\n<p class=\"has-sizing-medium\">The most important reason for variations in UV radiation is the cloud cover, but the ozone layer can also have a significant impact, both from day to day and year to year.<\/p>\n\n\n\n<p class=\"has-sizing-medium\">A 1% thinner ozone layer gives just over a 1% rise in the UV level. Influence from other important factors:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>Cloud cover<br><em>A thick cloud cover will reduce UV radiation by up to 90%.<\/em><\/li>\n\n\n\n<li>Reflection from the ground<br><em>Newly fallen snow can reflect over 90% of the UV rays and substantially raise UV doses near the ground.<\/em><\/li>\n\n\n\n<li>Height of the sun<br><em>The low height of the sun, even in summer, is the main reason why levels of UV radiation at high latitudes, like in Ny-\u00c5lesund, are in general relatively low.<\/em><\/li>\n\n\n\n<li>Aerosols<br><em>Even low concentrations of aerosols in the atmosphere can contribute to a reduction in the UV level.<\/em><\/li>\n<\/ul>\n\n\n\n<div class=\"wp-block-group has-light-grey-background-color has-background\"><div class=\"wp-block-group__inner-container is-layout-constrained wp-block-group-is-layout-constrained\">\n<h3 class=\"wp-block-heading\">Places and areas<\/h3>\n\n\n\n<ul class=\"wp-block-list\">\n<li><a href=\"https:\/\/www.npolar.no\/en\/zeppelin\/\" target=\"_blank\" rel=\"noreferrer noopener\">Ny-\u00c5lesund (Zeppelin observatory)<\/a><\/li>\n<\/ul>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-group\"><div class=\"wp-block-group__inner-container is-layout-flow wp-block-group-is-layout-flow\">\n<div class=\"wp-block-group\"><div class=\"wp-block-group__inner-container is-layout-flow wp-block-group-is-layout-flow\">\n<div class=\"wp-block-group has-light-grey-background-color has-background\"><div class=\"wp-block-group__inner-container is-layout-constrained wp-block-group-is-layout-constrained\">\n<h3 class=\"wp-block-heading\">Relations to other monitoring<\/h3>\n\n\n\n<h4 class=\"wp-block-heading has-sizing-medium\">Monitoring programme<\/h4>\n\n\n\n<ul class=\"wp-block-list has-sizing-medium\">\n<li><a href=\"https:\/\/www.miljodirektoratet.no\/ansvarsomrader\/overvaking-arealplanlegging\/miljoovervaking\/overvakingsprogrammer\/forurensning-og-klimagasser\/klimagasser-ozonlag-uv-straling-og-atmosfarisk-forurensning\/\" target=\"_blank\" rel=\"noreferrer noopener\">Norwegian Environment Agency\u2019s program for Greenhouse gases, ozone layers, UV radiation and atmospheric pollution<\/a> (<em>in Norwegian<\/em>).<\/li>\n<\/ul>\n\n\n\n<h4 class=\"wp-block-heading has-sizing-medium\">International environmental agreements<\/h4>\n\n\n\n<ul class=\"wp-block-list has-sizing-medium\">\n<li><a href=\"https:\/\/www.unep.org\/ozonaction\/who-we-are\/about-montreal-protocol\" target=\"_blank\" rel=\"noreferrer noopener\">The Montreal Protocol<\/a><\/li>\n<\/ul>\n\n\n\n<h4 class=\"wp-block-heading has-sizing-medium\">Voluntary international cooperation<\/h4>\n\n\n\n<ul class=\"wp-block-list has-sizing-medium\">\n<li>None<\/li>\n<\/ul>\n\n\n\n<h4 class=\"wp-block-heading has-sizing-medium\">Related monitoring<\/h4>\n\n\n\n<ul class=\"wp-block-list has-sizing-medium\">\n<li>None<\/li>\n<\/ul>\n<\/div><\/div>\n<\/div><\/div>\n\n\n\n<h2 class=\"wp-block-heading\">Further reading<\/h2>\n\n\n\n<div class=\"wp-block-group has-light-grey-background-color has-background\"><div class=\"wp-block-group__inner-container is-layout-constrained wp-block-group-is-layout-constrained\">\n<h3 class=\"wp-block-heading has-sizing-medium\">Links<\/h3>\n\n\n\n<ul class=\"wp-block-list has-sizing-medium\">\n<li><a href=\"http:\/\/uv.nilu.no\/\">UV alert for towns in Norway and holiday destinations abroad (<\/a><em><a href=\"http:\/\/uv.nilu.no\/\" target=\"_blank\" rel=\"noreferrer noopener\">in Norwegian<\/a><\/em><a href=\"http:\/\/uv.nilu.no\/\">)<\/a><\/li>\n\n\n\n<li><a href=\"https:\/\/uvnett.dsa.no\/default_en.aspx\" target=\"_blank\" rel=\"noreferrer noopener\">Today&#8217;s UV index: See today&#8217;s maximum daily UV index at the monitoring stations in the Norwegian UV network<\/a><\/li>\n<\/ul>\n\n\n\n<h3 class=\"wp-block-heading has-sizing-medium\">Publications<\/h3>\n\n\n\n<ol class=\"wp-block-list\">\n<li>Petkov, B., Hansen, G.H., Svendby,T.M., Sobolewski, P., &amp; Laska, K. (2019). <a href=\"https:\/\/www.sios-svalbard.org\/sites\/sios-svalbard.org\/files\/common\/SESS_2018_08_UV_ozone.pdf\" target=\"_blank\" rel=\"noreferrer noopener\">Observations of the solar UV irradiance and ozone column at Svalbard.<\/a> In: Orr et al. (eds): SESS report 2018, Svalbard Integrated Arctic Earth Observing System, Longyearbyen, pp. 170-183. <a href=\"https:\/\/doi.org\/10.5281\/zenodo.4778491\" target=\"_blank\" rel=\"noreferrer noopener\">https:\/\/doi.org\/10.5281\/zenodo.4778491<\/a>.<\/li>\n\n\n\n<li>Svendby, T., Fj\u00e6raa, A. M., Nilsen, A.-C., Schulze, D., &amp; Johnsen, B. (2023). <a href=\"https:\/\/www.miljodirektoratet.no\/publikasjoner\/2023\/september-2023\/monitoring-of-the-atmospheric-ozone-layer-and-natural-ultraviolet-radiation\/\" target=\"_blank\" rel=\"noreferrer noopener\">Monitoring of the atmospheric ozone layer and natural ultraviolet radiation. Annual Report 2022<\/a>. <em>NILU report 16\/2023;Norwegian Environment Agency M-2575|2023<\/em>. Kjeller: NILU.<\/li>\n\n\n\n<li>Svendby, T. M., Johnsen, B., Kylling, A., Dahlback, A., Bernhard, G. H., Hansen, G. H., &#8230; &amp; Vitale, V. (2021). <a href=\"https:\/\/acp.copernicus.org\/articles\/21\/7881\/2021\/\" target=\"_blank\" rel=\"noreferrer noopener\">GUV long-term measurements of total ozone column and effective cloud transmittance at three Norwegian sites.<\/a>&nbsp;<em>Atmospheric Chemistry and Physics<\/em>,&nbsp;<em>21<\/em>(10), 7881-7899. <a href=\"https:\/\/doi.org\/10.5194\/acp-21-7881-2021\" target=\"_blank\" rel=\"noreferrer noopener\">https:\/\/doi.org\/10.5194\/acp-21-7881-2021<\/a>.<\/li>\n<\/ol>\n<\/div><\/div>\n<\/div><\/div>\n","protected":false},"featured_media":62494,"parent":1139,"menu_order":0,"template":"","class_list":["post-1147","bc_indicator","type-bc_indicator","status-publish","has-post-thumbnail"],"acf":[],"_links":{"self":[{"href":"https:\/\/mosj.no\/en\/wp-json\/wp\/v2\/bc_indicator\/1147","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/mosj.no\/en\/wp-json\/wp\/v2\/bc_indicator"}],"about":[{"href":"https:\/\/mosj.no\/en\/wp-json\/wp\/v2\/types\/bc_indicator"}],"version-history":[{"count":1,"href":"https:\/\/mosj.no\/en\/wp-json\/wp\/v2\/bc_indicator\/1147\/revisions"}],"predecessor-version":[{"id":64032,"href":"https:\/\/mosj.no\/en\/wp-json\/wp\/v2\/bc_indicator\/1147\/revisions\/64032"}],"up":[{"embeddable":true,"href":"https:\/\/mosj.no\/en\/wp-json\/wp\/v2\/bc_indicator\/1139"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/mosj.no\/en\/wp-json\/wp\/v2\/media\/62494"}],"wp:attachment":[{"href":"https:\/\/mosj.no\/en\/wp-json\/wp\/v2\/media?parent=1147"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}