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    ztracené heslo?
    TUHOKlimaticka zmena / Thank you so much for ruining my day
    KEB
    KEB --- ---
    DZODZO: ale aspoň se na půdě bude dobře sušit seno :-D
    DZODZO
    DZODZO --- ---
    PAD: nevyhoda bude asi chladenie, ked to mas na konzoli nad taskami, tak je tam aspon skvirka, ktorou prefukuje trochu vzduch a chladi ti to, takto priamo pod strechou leda zeby si si tam dal nejake vetracky :)
    PAD
    PAD --- ---
    TADEAS: diky. vyhoda je estetika a asi trochu vetsi odolnost proti vetru, nevyhoda pripadny narocnejsi servis (vymenit panel bude znamenat opravovat tu hydroizolaci). ale je to takto z fotky opravdu mene hnusne.

    jine reseni te osklivosti je ty panely dat na jinou strechu - garaz, kolnu, drevnik, atp. tady: https://www.forbes.com/sites/lauriewinkless/2021/04/20/solar-city-turning-buildings-into-power-plants/?sh=7d8105b72d32 jsou fakt uz hezke formy panelu, ale cena bude asi dost vysoka ...
    TADEAS
    TADEAS --- ---
    PAD: dela to firma t-power

    Rám se dává pod panely místo kotvících háků přímo na střešní latě a vytvoří tak s panely povětrnostním podmínkám odolnou krytin. Panely budou kladeny na výšku a budou integrovány pomocí speciálních hydroizolačních modulů přímo do střešního pláště, kde nahradí stávající krytinu

    DZODZO
    DZODZO --- ---
    PAD: u tych krup bude asi zalezat aj ako na strechu dopadaju ci pod uhlom alebo kolmo na panel, proti tornadu ale nevydrzia nic

    Záběry z dronu: Tornádo se prohnalo i přes solární elektrárnu - Novinky.cz
    https://www.novinky.cz/ekonomika/clanek/zabery-dronu-tornado-se-prohnalo-i-pres-solarni-elektrarnu-40364540
    PAD
    PAD --- ---
    TADEAS: jak to v praxi vypada? ty panely pak tvori vlastne krytinu, tj. pod nimi uz je jen pojistna hydroizolace? jde mi o to, jak pak probiha vymena nebo servis.
    PAD
    PAD --- ---
    YMLADRIS: ke svym (AIXTEC) jsem ten udaj nenasel, ale ted uvazuju o techto k rodicum na chalupu a tam uvadi vydrz uderu krup do prumeru 45mm a rychlosti 30m/s (pokud se jim da verit, ze ..). Jinak bezna odolnost k stalemu zatizeni (=snih) je 2400pa, coz by nemel byt problem na drtive vetsine strech v CR (vyjimkou by byly jen velmi malo sklonene nebo ploche nekde v horach).

    Takze tyhle tenisaky velke jak dlan by tu FVE asi rozbily. Nebo by to ty panely odfouklo, nebo by to rozbila prilitnuta vetev nebo auto ... Kazdopadne ja tohle neresim, asi nejvice se bojim pripadneho spadleho stromu, ktere v sousedstvi mam.
    SHEFIK
    SHEFIK --- ---


    Asi v tom bude mit oteplovani taky prsty

    Dramatic images capture rapid slide of Antarctic glacier | Live Science
    https://www.livescience.com/satellite-images-pine-island-glacier-acceleration.html
    AIM_FREEMAN
    AIM_FREEMAN --- ---
    Ještě jedno bitechnologický hOPIUM :)

    Is Mycelium Fungus the Plastic of the Future?
    https://www.youtube.com/watch?v=cApVVuuqLFY
    AIM_FREEMAN
    AIM_FREEMAN --- ---
    A budou masový reaktory taky sekvestrovat uhlík???

    V Izraeli otevřeli továrnu pro výrobu kuřecího i vepřového z bioreaktorů
    https://www.czechcrunch.cz/2021/06/tovarna-na-maso-budoucnosti-v-izraeli-spustili-velkovyrobu-kureciho-i-veproveho-z-bioreaktoru/
    TUHO
    TUHO --- ---
    SHEFIK: mas pravdu, ted ctu vyjadreni klimatologu o situaci s tornadama v evrope (lapin, metelka, pecho) a ty tvrdi, ze tu jednak je souvislost teoreticky a jednak i v narustajici cetnosti...
    TADEAS
    TADEAS --- ---
    Unexpected: Desert Plants Are Struggling in Higher Heat - Scientific American
    https://www.scientificamerican.com/article/unexpected-desert-plants-are-struggling-in-higher-heat/

    https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2020JG005942

    Even desert plants have their limits.

    As dryland ecosystems experience stronger heat waves and droughts, scientists have wondered how climate change might affect the hardy plants that thrive in harsh deserts or dry mountains.

    With about 40% of the world covered in dry land, the question carries enormous weight for conservation policy: Will the natural toughness of those plants prepare them for even more extreme conditions? Or have they already reached the limits of what they can endure?

    Recent research suggests dry lands are at a breaking point — and it's more closely tied to temperature than previously thought.

    Dryland ecosystems "may be more susceptible to climate change than expected," a group of University of California, Irvine, researchers wrote in a recent study based around Anza-Borrego Desert State Park near the Mexican border.

    "Our analysis suggests these ecosystems may have crossed an ecological threshold," they said, describing a breakdown in the relationship between precipitation and vegetation cover beginning around 1999.

    In the Sonoran Desert and nearby landscapes, the scientists found, vegetation cover declined much more sharply than drought or wildfires alone could explain. Satellite observations between 1984 and 2017 showed "widespread" declines in perennial vegetation cover, the researchers wrote, especially in lowland deserts.

    In the lowlands, modeling revealed that temperature explained much of the desert's vegetation change, according to the study. Rising heat was also the best explanation for vegetation declines over the long term, as precipitation and wildfires have swung wildly from year to year.
    SHEFIK
    SHEFIK --- ---
    The weekend read: New support for Europe’s green energy transition – pv magazine International
    https://www.pv-magazine.com/2021/06/26/the-weekend-read-new-support-for-europes-green-transition/
    TADEAS
    TADEAS --- ---
    YMLADRIS, TADEAS:

    Hamburg Climate Futures Outlook : CLICCS : Universität Hamburg
    https://www.cliccs.uni-hamburg.de/results/hamburg-climate-futures-outlook.html
    TADEAS
    TADEAS --- ---
    YMLADRIS:

    Deep decarbonisation requires that we reduce anthropogenic emissions in the first place. In fact, we need a year-on-year reduction in emissions from now until 2050, roughly equivalent to the 7% reductions seen during the COVID-19 pandemic. Since zero-carbon technologies can take decades to scale up and optimise, and lock-in effects commit us to the technologies we choose now for years to come, we also need to act fast.

    To study the social dynamics needed for such a rapid transformation, we looked at ten social drivers of decarbonisation: United Nations climate governance, transnational initiatives, climate-related regulation, climate protests and social movements, climate litigation, corporate responses, fossil fuel divestment, consumption patterns, journalism, and knowledge production. We studied the drivers’ current trajectories, but also the enabling or constraining conditions that influence their future development.

    We found, for example, that consumption will keep growing due to a lack of regulation and strong cultural habits of consumption, “green” or otherwise. While the way in which we consume changed rapidly during the pandemic, shifting online, what and how much we consume is anchored in cultural habits and attitudes.

    We found that divestment – selling investments in fossil-fuel infrastructure – is occurring to some extent, but with unexpected negative spillover effects, such as when nation states divest at home but reinvest in fossil fuels abroad. And we found that social movements have a positive effect in some countries, but it remains uncertain how their political vision will mature after the pandemic, or in key countries like China, where protests do not usually have an influence on national politics.

    None of the drivers show enough momentum to bring about deep decarbonisation by 2050, and two drivers, consumption patterns and corporate responses, actively inhibit it. Our final assessment: even if a partial decarbonisation is currently plausible, deep decarbonisation by the year 2050 is not.

    We then combined our assessment of social plausibility with the latest set of socioeconomic future emissions scenarios and the latest physical science research on climate sensitivity – how much the climate will warm after a given amount of CO₂ emissions. This joint physical and social assessment evaluates warming lower than 1.7°C and warming higher than 4.9°C by the end of the century as currently not plausible.

    Deep decarbonisation could become more plausible, but this future would also require a good deal of tenacity. Rapid cuts in emissions may take a long time to show up in atmospheric CO₂ concentrations and warming trends – perhaps decades. Not only will we need to implement radical changes, we will also need to remain committed to seeing those changes through, beyond the time frame of one election cycle.
    DZODZO
    DZODZO --- ---
    tak uz je to jasne, polski diskuteri to rozlouskli, ziadne extremne prejavy zmeny klimy, ale bozi trest! :)

    "„To, co se Čechům stalo, je trest boží za důl Turów. Za ty miliony, co od nás denně chtějí... Museli jste donášet sousedům do Bruselu. Všemohoucí není rychlý, ale je spravedlivý. Stěžovali si před mezinárodním soudem, že polský důl jim sebral vodu, teď už by jim měla postačit,” uvedl jeden z diskutujících na stránce wp.pl, který o neštěstí na Moravě informoval."
    TADEAS
    TADEAS --- ---
    Tornáda jsou projev extrémního počasí. A to souvisí s klimatickou změnou – A2larm
    https://a2larm.cz/2021/06/tornada-jsou-projev-extremniho-pocasi-a-to-souvisi-s-klimatickou-zmenou/
    TADEAS
    TADEAS --- ---
    O klimatické spravedlnosti
    https://youtube.com/watch?v=AOA3T7EnFM4


    Co pro nás vlastně znamená "klimatická spravedlnost"?

    Minulý týden jsme k tomu uspořádali online debatu, zajímalo by mě, jaké argumenty byste k ní ještě doplnili.

    Diskutovali:
    - Romana Březovská, analytička Výzkumného centra Asociace pro mezinárodní otázky se zaměřením na problematiku změny klimatu v širších souvislostech
    - Danuše Nerudová, ekonomka a rektorka Mendelovy univerzity v Brně
    - Alexandr Ač, ekolog z Ústav výzkumu globální změny AV ČR
    TADEAS
    TADEAS --- ---


    žít klima
    TADEAS
    TADEAS --- ---
    One Planet, How Many People? A Review of Earth's Carrying Capacity
    https://na.unep.net/geas/getUNEPPageWithArticleIDScript.php?article_id=88

    https://na.unep.net/geas/archive/pdfs/geas_jun_12_carrying_capacity.pdf

    t is estimated that global population reached seven billion in late 2011 or early 2012. As global population has doubled since the 1960s, per capita GDP has grown to more than ten times what it was then. The human impact has grown to such a scale that it has become a major geophysical force. It is not surprising that concerns about the number of people the Earth can support have re-emerged recently. Attempts to define an upper limit of the number of people that the Earth could support are inevitably subject to considerable uncertainty, however, the greatest concentration estimates falls between 8 and 16 billion people — a range we are fast approaching. While there are many ways we might reduce our per capita impact on the planet, the collective impact will always be multiplied by global population, making population an issue which cannot be ignored.
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