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<html><head><style>div[role] {border:solid 1px;margin:1px;}</style><base href="https://en.wikipedia.org/wiki/"></head><body><div role="ami_dictionary" title="dict_test_new"><div name="nimby" term="nimby" role="ami_entry"><p>search term: nimby <a href="https://en.wikipedia.org/w/index.php?search=nimby">Wikipedia Page</a></p><p class="wpage_first_para"><b>NIMBY</b> (<span class="rt-commentedText nowrap"><span class="IPA nopopups noexcerpt" lang="en-fonipa"><a href="/wiki/Help:IPA/English" title="Help:IPA/English">/<span style="border-bottom:1px dotted"><span title="/ˈ/: primary stress follows">ˈ</span><span title="'n' in 'nigh'">n</span><span title="/ɪ/: 'i' in 'kit'">ɪ</span><span title="'m' in 'my'">m</span><span title="'b' in 'buy'">b</span><span title="/i/: 'y' in 'happy'">i</span></span>/</a></span></span>, or <b>nimby</b>),<sup id="cite_ref-1" class="reference"><a href="#cite_note-1"><span class="cite-bracket">[</span>1<span class="cite-bracket">]</span></a></sup> an <a href="/wiki/Acronym" title="Acronym">acronym</a> for the phrase "<b>not in my back yard</b>",<sup id="cite_ref-2" class="reference"><a href="#cite_note-2"><span class="cite-bracket">[</span>2<span class="cite-bracket">]</span></a></sup><sup id="cite_ref-3" class="reference"><a href="#cite_note-3"><span class="cite-bracket">[</span>3<span class="cite-bracket">]</span></a></sup> is a characterization of opposition by residents to proposed <a href="/wiki/Real_estate_development" title="Real estate development">real estate development</a> and <a href="/wiki/Infrastructure" title="Infrastructure">infrastructure</a> developments in their local area, as well as support for strict land use regulations. It carries the connotation that such residents are only opposing the development because it is close to them and that they would tolerate or support it if it were built farther away. The residents are often called <b>nimbys</b>, and their viewpoint is called <b>nimbyism</b>. The opposite movement is known as <a href="/wiki/YIMBY" title="YIMBY">YIMBY</a> for "yes in my back yard".<sup id="cite_ref-4" class="reference"><a href="#cite_note-4"><span class="cite-bracket">[</span>4<span class="cite-bracket">]</span></a></sup>
</p><div title="figure"><figure class="mw-default-size" typeof="mw:File/Thumb"><a href="/wiki/File:Nimby_unfinished_tower_(cropped).jpg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/2/24/Nimby_unfinished_tower_%28cropped%29.jpg/220px-Nimby_unfinished_tower_%28cropped%29.jpg" decoding="async" width="220" height="165" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/2/24/Nimby_unfinished_tower_%28cropped%29.jpg/330px-Nimby_unfinished_tower_%28cropped%29.jpg 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/2/24/Nimby_unfinished_tower_%28cropped%29.jpg/440px-Nimby_unfinished_tower_%28cropped%29.jpg 2x" data-file-width="4034" data-file-height="3026"></a><figcaption>Unfinished tower in <a href="/wiki/Tenleytown,_Washington,_D.C." class="mw-redirect" title="Tenleytown, Washington, D.C.">Tenleytown</a>, Washington, D.C. that was later removed as a result of complaints from the neighborhood</figcaption></figure>
</div><p></p></div><div name="deglaciation" term="deglaciation" role="ami_entry"><p>search term: deglaciation <a href="https://en.wikipedia.org/w/index.php?search=deglaciation">Wikipedia Page</a></p><p class="wpage_first_para"><b>Deglaciation</b> is the transition from full glacial conditions during <a href="/wiki/Ice_age" title="Ice age">ice ages</a>, to warm <a href="/wiki/Interglacial" title="Interglacial">interglacials</a>, characterized by <a href="/wiki/Global_warming" class="mw-redirect" title="Global warming">global warming</a> and <a href="/wiki/Sea_level_rise" title="Sea level rise">sea level rise</a> due to change in continental ice volume.<sup id="cite_ref-1" class="reference"><a href="#cite_note-1"><span class="cite-bracket">[</span>1<span class="cite-bracket">]</span></a></sup> Thus, it refers to the retreat of a <a href="/wiki/Glacier" title="Glacier">glacier</a>, an <a href="/wiki/Ice_sheet" title="Ice sheet">ice sheet</a> or frozen surface layer, and the resulting exposure of the <a href="/wiki/Earth" title="Earth">Earth</a>'s surface. The decline of the <a href="/wiki/Cryosphere" title="Cryosphere">cryosphere</a> due to <a href="/wiki/Ablation" title="Ablation">ablation</a> can occur on any scale from global to localized to a particular glacier.<sup id="cite_ref-2" class="reference"><a href="#cite_note-2"><span class="cite-bracket">[</span>2<span class="cite-bracket">]</span></a></sup> After the <a href="/wiki/Last_Glacial_Maximum" title="Last Glacial Maximum">Last Glacial Maximum</a> (ca. 21,000 years ago), the last deglaciation begun, which lasted until the early <a href="/wiki/Holocene" title="Holocene">Holocene</a>.<sup id="cite_ref-3" class="reference"><a href="#cite_note-3"><span class="cite-bracket">[</span>3<span class="cite-bracket">]</span></a></sup><sup id="cite_ref-ClarkEtal_4-0" class="reference"><a href="#cite_note-ClarkEtal-4"><span class="cite-bracket">[</span>4<span class="cite-bracket">]</span></a></sup> Around much of Earth, deglaciation <a href="/wiki/Retreat_of_glaciers_since_1850" title="Retreat of glaciers since 1850">during the last 100 years</a> has been accelerating as a result of <a href="/wiki/Climate_change" title="Climate change">climate change</a>, partly brought on by <a href="/wiki/Global_warming" class="mw-redirect" title="Global warming">anthropogenic changes to greenhouse gases</a>.<sup id="cite_ref-5" class="reference"><a href="#cite_note-5"><span class="cite-bracket">[</span>5<span class="cite-bracket">]</span></a></sup>
</p><div title="figure"><figure class="mw-default-size" typeof="mw:File/Thumb"><a href="/wiki/File:20191021_Temperature_from_20,000_to_10,000_years_ago_-_recovery_from_ice_age.png" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/1/15/20191021_Temperature_from_20%2C000_to_10%2C000_years_ago_-_recovery_from_ice_age.png/220px-20191021_Temperature_from_20%2C000_to_10%2C000_years_ago_-_recovery_from_ice_age.png" decoding="async" width="220" height="167" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/1/15/20191021_Temperature_from_20%2C000_to_10%2C000_years_ago_-_recovery_from_ice_age.png/330px-20191021_Temperature_from_20%2C000_to_10%2C000_years_ago_-_recovery_from_ice_age.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/1/15/20191021_Temperature_from_20%2C000_to_10%2C000_years_ago_-_recovery_from_ice_age.png/440px-20191021_Temperature_from_20%2C000_to_10%2C000_years_ago_-_recovery_from_ice_age.png 2x" data-file-width="2572" data-file-height="1948"></a><figcaption>Temperature from 20,000 to 10,000 years ago, derived from EPICA Dome C Ice Core (Antarctica)</figcaption></figure>
</div><p></p></div><div name="wildfires" term="wildfires" role="ami_entry"><p>search term: wildfires <a href="https://en.wikipedia.org/w/index.php?search=wildfires">Wikipedia Page</a></p><p class="wpage_first_para">A <b>wildfire</b>, <b>forest fire</b>, or a <b>bushfire</b> is an unplanned, uncontrolled and unpredictable <a href="/wiki/Fire" title="Fire">fire</a> in an area of <a href="/wiki/Combustibility_and_flammability" title="Combustibility and flammability">combustible</a> <a href="/wiki/Vegetation" title="Vegetation">vegetation</a>.<sup id="cite_ref-Cambridge2_1-0" class="reference"><a href="#cite_note-Cambridge2-1"><span class="cite-bracket">[</span>1<span class="cite-bracket">]</span></a></sup><sup id="cite_ref-CIFFC_Glossary2_2-0" class="reference"><a href="#cite_note-CIFFC_Glossary2-2"><span class="cite-bracket">[</span>2<span class="cite-bracket">]</span></a></sup> Depending on the type of vegetation present, a wildfire may be more specifically identified as a bushfire (<a href="/wiki/Bushfires_in_Australia" title="Bushfires in Australia">in Australia</a>), desert fire, grass fire, hill fire, peat fire, prairie fire, vegetation fire, or <a href="/wiki/Veld" title="Veld">veld</a> fire.<sup id="cite_ref-Cbbcco.uk2_3-0" class="reference"><a href="#cite_note-Cbbcco.uk2-3"><span class="cite-bracket">[</span>3<span class="cite-bracket">]</span></a></sup> Some natural forest ecosystems <a href="/wiki/Fire_ecology" title="Fire ecology">depend on wildfire.</a><sup id="cite_ref-Fire_Tree_Mortality2222_4-0" class="reference"><a href="#cite_note-Fire_Tree_Mortality2222-4"><span class="cite-bracket">[</span>4<span class="cite-bracket">]</span></a></sup> Wildfires are different from <a href="/wiki/Controlled_burn" title="Controlled burn">controlled or prescribed burning</a>, which are carried out to provide a benefit for people. Modern <a href="/wiki/Forest_management" title="Forest management">forest management</a> often engages in prescribed burns to mitigate fire risk and promote natural forest cycles. However, controlled burns can turn into wildfires by mistake.
</p><div title="figure"><figure class="mw-default-size" typeof="mw:File/Thumb"><a href="/wiki/File:Burnout_ops_on_Mangum_Fire_McCall_Smokejumpers.jpg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/0/05/Burnout_ops_on_Mangum_Fire_McCall_Smokejumpers.jpg/300px-Burnout_ops_on_Mangum_Fire_McCall_Smokejumpers.jpg" decoding="async" width="300" height="200" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/0/05/Burnout_ops_on_Mangum_Fire_McCall_Smokejumpers.jpg/450px-Burnout_ops_on_Mangum_Fire_McCall_Smokejumpers.jpg 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/0/05/Burnout_ops_on_Mangum_Fire_McCall_Smokejumpers.jpg/600px-Burnout_ops_on_Mangum_Fire_McCall_Smokejumpers.jpg 2x" data-file-width="612" data-file-height="408"></a><figcaption>Wildfire burning in the <a href="/wiki/Kaibab_National_Forest" title="Kaibab National Forest">Kaibab National Forest</a>, <a href="/wiki/Arizona" title="Arizona">Arizona</a>, United States, in 2020. The <a href="/wiki/Mangum_Fire" title="Mangum Fire">Mangum Fire</a> burned more than 70,000 acres (280 km<sup>2</sup>) of <a href="/wiki/Forest" title="Forest">forest</a>.</figcaption></figure>
</div><p></p></div><div name="Greenland ice sheet" term="Greenland ice sheet" role="ami_entry"><p>search term: Greenland ice sheet <a href="https://en.wikipedia.org/w/index.php?search=Greenland%20ice%20sheet">Wikipedia Page</a></p><p class="wpage_first_para">The <b>Greenland ice sheet</b> is an <a href="/wiki/Ice_sheet" title="Ice sheet">ice sheet</a> which forms the second largest body of ice in the world. It is an average of 1.67 km (1.0 mi) thick, and over 3 km (1.9 mi) thick at its maximum.<sup id="cite_ref-BBC2017_2-2" class="reference"><a href="#cite_note-BBC2017-2"><span class="cite-bracket">[</span>2<span class="cite-bracket">]</span></a></sup> It is almost 2,900 kilometres (1,800 mi) long in a north–south direction, with a maximum width of 1,100 kilometres (680 mi) at a latitude of <a href="/wiki/77th_parallel_north" title="77th parallel north">77°N</a>, near its northern edge.<sup id="cite_ref-BRGIS_1-3" class="reference"><a href="#cite_note-BRGIS-1"><span class="cite-bracket">[</span>1<span class="cite-bracket">]</span></a></sup> The ice sheet covers 1,710,000 square kilometres (660,000 sq mi), around 80% of the surface of <a href="/wiki/Greenland" title="Greenland">Greenland</a>, or about 12% of the area of the <a href="/wiki/Antarctic_ice_sheet" title="Antarctic ice sheet">Antarctic ice sheet</a>.<sup id="cite_ref-BBC2017_2-3" class="reference"><a href="#cite_note-BBC2017-2"><span class="cite-bracket">[</span>2<span class="cite-bracket">]</span></a></sup> The term 'Greenland ice sheet' is often shortened to GIS or GrIS in <a href="/wiki/Scientific_literature" title="Scientific literature">scientific literature</a>.<sup id="cite_ref-Tan2018_3-0" class="reference"><a href="#cite_note-Tan2018-3"><span class="cite-bracket">[</span>3<span class="cite-bracket">]</span></a></sup><sup id="cite_ref-Noël2021_4-0" class="reference"><a href="#cite_note-No%C3%ABl2021-4"><span class="cite-bracket">[</span>4<span class="cite-bracket">]</span></a></sup><sup id="cite_ref-Höning2023_5-0" class="reference"><a href="#cite_note-H%C3%B6ning2023-5"><span class="cite-bracket">[</span>5<span class="cite-bracket">]</span></a></sup><sup id="cite_ref-Bochow2023_6-0" class="reference"><a href="#cite_note-Bochow2023-6"><span class="cite-bracket">[</span>6<span class="cite-bracket">]</span></a></sup>
</p><div title="figure"><a href="/wiki/File:Greenland_ice_sheet_AMSL_thickness_map-en.png" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/9/98/Greenland_ice_sheet_AMSL_thickness_map-en.png/288px-Greenland_ice_sheet_AMSL_thickness_map-en.png" decoding="async" width="288" height="491" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/9/98/Greenland_ice_sheet_AMSL_thickness_map-en.png/432px-Greenland_ice_sheet_AMSL_thickness_map-en.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/9/98/Greenland_ice_sheet_AMSL_thickness_map-en.png/576px-Greenland_ice_sheet_AMSL_thickness_map-en.png 2x" data-file-width="1056" data-file-height="1801"></a></div><p></p></div><div name="water cycle" term="water cycle" role="ami_entry"><p>search term: water cycle <a href="https://en.wikipedia.org/w/index.php?search=water%20cycle">Wikipedia Page</a></p><p class="wpage_first_para">The <b>water cycle</b> (or <b>hydrologic cycle</b> or <b>hydrological cycle</b>), is a <a href="/wiki/Biogeochemical_cycle" title="Biogeochemical cycle">biogeochemical cycle</a> that involves the continuous movement of <a href="/wiki/Water" title="Water">water</a> on, above and below the surface of the <a href="/wiki/Earth" title="Earth">Earth</a>. The mass of water on Earth remains fairly constant over time. However, the partitioning of the water into the major reservoirs of <a href="/wiki/Ice" title="Ice">ice</a>, <a href="/wiki/Fresh_water" title="Fresh water">fresh water</a>, <a href="/wiki/Saline_water" title="Saline water">salt water</a> and <a href="/wiki/Atmosphere" title="Atmosphere">atmospheric water</a> is variable and depends on <a href="/wiki/Climate" title="Climate">climatic variables</a>. The water moves from one reservoir to another, such as from river to <a href="/wiki/Ocean" title="Ocean">ocean</a>, or from the ocean to the atmosphere. The processes that drive these movements are <a href="/wiki/Evaporation" title="Evaporation">evaporation</a>, <a href="/wiki/Transpiration" title="Transpiration">transpiration</a>, <a href="/wiki/Condensation" title="Condensation">condensation</a>, <a href="/wiki/Precipitation_(meteorology)" class="mw-redirect" title="Precipitation (meteorology)">precipitation</a>, <a href="/wiki/Sublimation_(phase_transition)" title="Sublimation (phase transition)">sublimation</a>, <a href="/wiki/Infiltration_(hydrology)" title="Infiltration (hydrology)">infiltration</a>, <a href="/wiki/Surface_runoff" title="Surface runoff">surface runoff</a>, and subsurface flow. In doing so, the water goes through different forms: liquid, solid (<a href="/wiki/Ice" title="Ice">ice</a>) and <a href="/wiki/Water_vapor" title="Water vapor">vapor</a>. The ocean plays a key role in the water cycle as it is the source of 86% of global evaporation.<sup id="cite_ref-:4_2-0" class="reference"><a href="#cite_note-:4-2"><span class="cite-bracket">[</span>2<span class="cite-bracket">]</span></a></sup>
</p><div title="figure"><figure class="mw-default-size" typeof="mw:File/Thumb"><a href="/wiki/File:USGS_WaterCycle_English_ONLINE_20221013.png" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/6/60/USGS_WaterCycle_English_ONLINE_20221013.png/300px-USGS_WaterCycle_English_ONLINE_20221013.png" decoding="async" width="300" height="205" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/6/60/USGS_WaterCycle_English_ONLINE_20221013.png/450px-USGS_WaterCycle_English_ONLINE_20221013.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/6/60/USGS_WaterCycle_English_ONLINE_20221013.png/600px-USGS_WaterCycle_English_ONLINE_20221013.png 2x" data-file-width="11400" data-file-height="7800"></a><figcaption>A detailed diagram depicting the global water cycle. The direction of movement of water between reservoirs tends towards upwards movement through <a href="/wiki/Evapotranspiration" title="Evapotranspiration">evapotranspiration</a> and downward movement through <a href="/wiki/Gravity" title="Gravity">gravity</a>. The diagram also shows how human water use impacts where water is stored and how it moves.<sup id="cite_ref-1" class="reference"><a href="#cite_note-1"><span class="cite-bracket">[</span>1<span class="cite-bracket">]</span></a></sup></figcaption></figure>
</div><p></p></div><div name="Atlantic meridional overturning circulation" term="Atlantic meridional overturning circulation" role="ami_entry"><p>search term: Atlantic meridional overturning circulation <a href="https://en.wikipedia.org/w/index.php?search=Atlantic%20meridional%20overturning%20circulation">Wikipedia Page</a></p><p class="wpage_first_para">The <b>Atlantic meridional overturning circulation</b> (<b>AMOC</b>) is the main <a href="/wiki/Ocean_current" title="Ocean current">ocean current</a> system in the <a href="/wiki/Atlantic_Ocean" title="Atlantic Ocean">Atlantic Ocean</a>.<sup id="cite_ref-IPCC_AR6_AnnexVII_1-0" class="reference"><a href="#cite_note-IPCC_AR6_AnnexVII-1"><span class="cite-bracket">[</span>1<span class="cite-bracket">]</span></a></sup><sup class="reference nowrap"><span title="Page / location: 2238">: 2238 </span></sup> It is a component of Earth's <a href="/wiki/Ocean_circulation" class="mw-redirect" title="Ocean circulation">ocean circulation</a> system and plays an important role in the <a href="/wiki/Climate_system" title="Climate system">climate system</a>. The AMOC includes Atlantic currents at the surface and at great depths that are driven by changes in weather, temperature and <a href="/wiki/Salinity" title="Salinity">salinity</a>. Those currents comprise half of the global <a href="/wiki/Thermohaline_circulation" title="Thermohaline circulation">thermohaline circulation</a> that includes the flow of major ocean currents, the other half being the <a href="/wiki/Southern_Ocean_overturning_circulation" title="Southern Ocean overturning circulation">Southern Ocean overturning circulation</a>.<sup id="cite_ref-NOAA2023_2-0" class="reference"><a href="#cite_note-NOAA2023-2"><span class="cite-bracket">[</span>2<span class="cite-bracket">]</span></a></sup>
</p><div title="figure"><figure class="mw-default-size" typeof="mw:File/Thumb"><a href="/wiki/File:OCP07_Fig-6.jpg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/d/d4/OCP07_Fig-6.jpg/220px-OCP07_Fig-6.jpg" decoding="async" width="220" height="173" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/d/d4/OCP07_Fig-6.jpg/330px-OCP07_Fig-6.jpg 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/d/d4/OCP07_Fig-6.jpg/440px-OCP07_Fig-6.jpg 2x" data-file-width="600" data-file-height="473"></a><figcaption>Topographic map of the Nordic Seas and subpolar basins with surface currents (solid curves) and deep currents (dashed curves) that form a portion of the Atlantic meridional overturning circulation. Colors of curves indicate approximate temperatures.</figcaption></figure>
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