Перевод песни Astronaut in the ocean (Masked Wolf)
Astronaut in the ocean
Астронавт в океане
What you know about rollin’ down in the deep?
When your brain goes numb
You can call that mental freeze
When these people talk too much
Put that shit in slow motion, yeah
I feel like an astronaut in the ocean, ayy
What you know about rollin’ down in the deep?
When your brain goes numb
You can call that mental freeze
When these people talk too much
Put that shit in slow motion, yeah
I feel like an astronaut in the ocean, ayy
She say that I’m cool
I’m like, «Yeah, that’s true»
I believe in G-O-D
Don’t believe in T-H-O-T
She keep playing me dumb
I’ma play her for fun
Y’all don’t really know my mental
Let me give you the picture like stencil
Fallin’ out in a drought
No flow, rain wasn’t pourin’ down
See, that pain was all around
See, my mode was kinda lounged
Didn’t know which, which way to turn
Flow was cool
But I still felt burnt
Energy up
You can feel my surge
I’ma kill everything like this purge
Let’s just get this straight for a second, I’ma work
Even if I don’t get paid for progression, I’ma get it
Everything that I do is electric
I’ma keep it in a motion
Keep it movin’ like kinetic
Put this shit in a frame, better know I don’t blame
Everything that I say, man, I seen you deflate
Let me elevate, this ain’t a prank
Have you walkin’ on a plank, la-la-la-la-la
Both hands together, God, let me pray
I’ve been goin’ right, right around, call that relay
Pass the baton, back and I’m on
Swimmin’ in the pool — Kendrick Lamar, uh
Want a piece of this, a piece of mine, my peace a sign
Can you please read between the lines?
My rhyme’s inclined to break your spine
They say that I’m so fine
You could never match my grind
Please do not, not waste my time
What you know about rollin’ down in the deep?
When your brain goes numb
You can call that mental freeze
When these people talk too much
Put that shit in slow motion, yeah
I feel like an astronaut in the ocean, ayy
What you know about rollin’ down in the deep?
When your brain goes numb
You can call that mental freeze
When these people talk too much
Put that shit in slow motion, yeah
I feel like an astronaut in the ocean
Что ты знаешь о том, каково это — идти ко дну?
Когда твой мозг немеет
Можешь называть это заморозкой разума
Когда эти люди говорят слишком много
Запускаю их бред в слоу-моушне, да
Чувствую себя, будто астронавт в океане, эй
Что ты знаешь о том, каково это — идти ко дну?
Когда твой мозг немеет
Можешь называть это заморозкой разума
Когда эти люди говорят слишком много
Запускаю их бред в слоу-моушне, да
Чувствую себя, будто астронавт в океане, эй
Она говорит, что я крут
Я такой: «Ага, верно»
Я верю в Б-О-Г-А
Не верю Ш-Л-Ю-Х-А-М
Она продолжает держать меня за идиота
Я играю ею ради забавы
Никто из вас не знает, что у меня в голове
Давайте я нарисую вам картинку, как по трафарету
Погружаюсь в засуху
Ни капли 1 , дождь не льётся с небес
Гляди, эта боль была повсюду
Гляди, я вроде как был в режиме ничегонеделанья
Не знал куда, куда повернуть
Поток меня освежил 2
Но я всё ещё чувствовал себя выгоревшим
Теперь у меня есть энергия
Вы можете почувствовать, как она хлещет
Я уничтожу всё вокруг, будто это Судная ночь 3
Давайте на секунду поговорим начистоту; я в работе
Даже если мне не заплатят за прогресс, я его совершу
Всё, что я делаю, заряжено электричеством
Я продолжу движение
Буду двигаться на кинетической энергии
Можешь записывать за мной, знай, я никого не виню
Каждый день я говорю: «Мужик, я видел, как ты сдулся»
Позволь мне подняться, это не розыгрыш
Ходил когда-нибудь по тонкой доске? Ла-ла-ла-ла-ла
Обе руки вместе, Боже, позволь помолиться
Я ходил вокруг, вокруг да около, называй это эстафетой
Передавай эстафетную палочку, я вернулся, и я заряжен
Плаваю в бассейне — Кендрик Ламар 4
Хочешь свою часть, часть меня, мой знак мира?
Будь добр, читай между строк
Мои рифмы склонны переломить твой хребет
Они говорят, что я очень хорош
Вам не сравниться со мной в трудолюбии
Пожалуйста, можете сейчас не тратить моё время?
Что ты знаешь о том, каково это — идти ко дну?
Когда твой мозг немеет
Можешь называть это заморозкой разума
Когда эти люди говорят слишком много
Запускаю их бред в слоу-моушне, да
Чувствую себя, будто астронавт в океане, эй
Что ты знаешь о том, каково это — идти ко дну?
Когда твой мозг немеет
Можешь называть это заморозкой разума
Когда эти люди говорят слишком много
Запускаю их бред в слоу-моушне, да
Чувствую себя, будто астронавт в океане
Источник
Ocean circulation is key to understanding uncertainties in climate change predictions
Thirty state-of-the-art IPCC-climate models predict dramatically different climates for the Northern Hemisphere, especially Europe. An analysis of the range of responses now reveals that the differences are mostly down to the individual model’s simulations of changes to the North Atlantic ocean currents and not only—as normally assumed—atmospheric changes. The work, by Katinka Bellomo, National Research Council of Italy, Institute of Atmospheric Sciences and Climate, and colleagues is published today in Nature Communications and is part of the European science collaboration, TiPES, coordinated by the University of Copenhagen.
All climate models vary in the details. Variables such as atmospheric pressure, cloud cover, temperature gradients, sea surface temperatures, and many more are tuned to interact slightly differently for every model. This means that the predictions of the many models also vary.
International modeling centers run a coordinated set of climate model simulations, which are then assessed by the IPCC and summarized in a balanced report. But naturally, an uncertainty remains, reflecting the many different tunings of models.
«We want to understand the differences among these models. Why does one model project an overall global temperature change of two degrees while another one of four degrees? Our objective is to narrow down this inter-model uncertainty. We also want to understand the differences in these models in terms of regional climate change,» explains Dr. Katinka Bellomo.
Two types of climate scenarios
Bellomo and colleagues analyzed simulations from 30 climate models and found an important difference. There is disagreement among the models on the rate of the decline in the Atlantic meridional overturning circulation (AMOC), a large system of ocean currents in the North Atlantic which overturns surface water to a deep ocean current and plays a crucial role in the distribution of heat from the tropics to the Northern Hemisphere.
«To see how this difference was reflected in projections of the future climate, we grouped together the top 10 models (from a total of 30) in which the AMOC decline is smaller. We then compared the group with the average of the 10 models that have the largest decline,» explains Bellomo.
The analysis revealed two distinct types of climate scenarios. In models where the AMOC decline is large, Europe warms only slightly, but wind patterns in Europe and precipitation patterns in the tropics change dramatically. However, in models where the AMOC decline is smaller, the Northern hemisphere heats up considerably, and a well-known pattern emerges in which wet regions get wetter and dry get dryer.
This means that the uncertainties in predictions of the future climate may to a large degree depend on how climate models predict changes in the overturning circulation in the North Atlantic. Thus, the result challenges the previous understanding of mechanisms controlling climate change over the North Atlantic, in which parameterizations of the atmosphere have been suspected to cause the main part of the uncertainty.
«This is important, because it points to the AMOC as one of the largest sources of uncertainties in climate prediction,» says Katinka Bellomo.
«I am excited about this research because there is so much more that can be done in addition to this. We need to investigate the processes leading to the inter-model differences in the ocean circulation response, the link between the ocean circulation response and precipitation change, and we also need to compare this with near-future projections of climate change,» says Bellomo.
Источник
*ОБНОВА* ГДЕ ИСКАТЬ КЛЮЧ В ОКЕАНЕ АДОПТ МИ? WHERE FIND KEY IN THE OCEAN IN ADOPT ME!
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- Опубликовано: 3 апр 2020
- УРА Я СПАТЬ, ВСЕМ СПОКИ!
люблю подписчиков!
►донат для развития канала — www.donationalerts.ru/r/barsonya
►сервер в дискорд — discord.gg/5pPrCxx
Комментарии • 0
А где это место?
Я смотрю видео в 2021
кто из 2021 года ? ._.
Я которая начала играть в адопт 3 месяца назад и сейчас эту корону мне не получить 🥲
Я туда с багом попала без ключа
А если уже нет этого океана? Пожалуйста можно способ где найти ключ с обновлениям которое сейчас
эх это старый адопт теперь адопт ми не тот
Эх я не магу это зделат ПАТАМУШТА я не была на этой абнови)))):
Ааа понимаю у меня эта корона в игре есть ппц
У меня есть этот ключ!Но он не открывает дверь(
Шо делоть, сейчас все замерзло(, как ключи получить
А сейчас это уже не работает?(
У меня есть этот ключ кому дать за шо
У Мена нет мора 🥺😞
Блин я в 2020 году и этот корабль уже давно не затонувший а просто магаз одежди😂😂😂 у кого также лайк
Почему у вас это есть я зашёл там нет ни пиратов ни ни этого водного города
Источник
Ocean circulation is key to understanding uncertainties in climate change predictions
Thirty state-of-the-art IPCC-climate models predict dramatically different climates for the Northern Hemisphere, especially Europe. An analysis of the range of responses now reveals that the differences are mostly down to the individual model’s simulations of changes to the North Atlantic ocean currents and not only—as normally assumed—atmospheric changes. The work, by Katinka Bellomo, National Research Council of Italy, Institute of Atmospheric Sciences and Climate, and colleagues is published today in Nature Communications and is part of the European science collaboration, TiPES, coordinated by the University of Copenhagen.
All climate models vary in the details. Variables such as atmospheric pressure, cloud cover, temperature gradients, sea surface temperatures, and many more are tuned to interact slightly differently for every model. This means that the predictions of the many models also vary.
International modeling centers run a coordinated set of climate model simulations, which are then assessed by the IPCC and summarized in a balanced report. But naturally, an uncertainty remains, reflecting the many different tunings of models.
«We want to understand the differences among these models. Why does one model project an overall global temperature change of two degrees while another one of four degrees? Our objective is to narrow down this inter-model uncertainty. We also want to understand the differences in these models in terms of regional climate change,» explains Dr. Katinka Bellomo.
Two types of climate scenarios
Bellomo and colleagues analyzed simulations from 30 climate models and found an important difference. There is disagreement among the models on the rate of the decline in the Atlantic meridional overturning circulation (AMOC), a large system of ocean currents in the North Atlantic which overturns surface water to a deep ocean current and plays a crucial role in the distribution of heat from the tropics to the Northern Hemisphere.
«To see how this difference was reflected in projections of the future climate, we grouped together the top 10 models (from a total of 30) in which the AMOC decline is smaller. We then compared the group with the average of the 10 models that have the largest decline,» explains Bellomo.
The analysis revealed two distinct types of climate scenarios. In models where the AMOC decline is large, Europe warms only slightly, but wind patterns in Europe and precipitation patterns in the tropics change dramatically. However, in models where the AMOC decline is smaller, the Northern hemisphere heats up considerably, and a well-known pattern emerges in which wet regions get wetter and dry get dryer.
This means that the uncertainties in predictions of the future climate may to a large degree depend on how climate models predict changes in the overturning circulation in the North Atlantic. Thus, the result challenges the previous understanding of mechanisms controlling climate change over the North Atlantic, in which parameterizations of the atmosphere have been suspected to cause the main part of the uncertainty.
«This is important, because it points to the AMOC as one of the largest sources of uncertainties in climate prediction,» says Katinka Bellomo.
«I am excited about this research because there is so much more that can be done in addition to this. We need to investigate the processes leading to the inter-model differences in the ocean circulation response, the link between the ocean circulation response and precipitation change, and we also need to compare this with near-future projections of climate change,» says Bellomo.
Источник