Atmospheric gearboxes lead to the permanent La Niña

Paola Bueno Paola Bueno Meteored Brazil 6 min
Atlántico Meridional Circulation
The meridional circulation of the Atlantic is collapsing completely with the continuation of the climatic exchange rate and the global calendar. Image: Goddard Special Space Center / NASA Space Visualization Studio

The climatic exchange is balancing an important ocean circulation that operates in the Atlantic Ocean, the glide Circulation of the Atlantic Ocean Sur. ¡This circulation is responsible for distributing the heat between the tropical region and the polar latitudes, which are extremely important for the balance of the global climate!

The circulation of the Atlantic Ocean is being offset by the exchange rate induced by human activities. The studio is collapsing completely, experimenting with a global climate similar to that we experimented with in La Niña!

A new studio published in Nature Climate Changeby Australian climatic scientists, inclusive Andrea Taschetto de Brasil, has exploited many series of impacts and consequences in the Tierra’s climate as it is a complete collapse system of the Atlantic Ocean.

Investigators uncover that the collapse of this system changes the climate of the Tierra to a stage similar to that of La Niña, the negative phase of the Os Nióo Oscillation phenomenon.

This means that the circulation of the collapsed is in Australia experimentaría más lluvia e inundacionessuch as most of the United States experimenting with temporal sequences and forest peaks much larger, según el stududio. Similar episodes or including people who register and record recently in these regions debuting in La Niña that has been active since 2020.

Investigators use a global model to analyze the resulting climatic scenario of this ocean circulation collapse, applying a simulation of massive rainfall in the North Atlantic. The first to detect investigators is that as the Atlantic circulation accumulates an enormous amount of heat on the ecuador.

There is an increase in calorific value over the Atlantic tropical altering the zonal atmospheric circulation, inducing oscillating motions over the Oriental Tropical Pacific. These moving motions of the nose, and their embroidery, fortify the chains that allow the agitators to move from one end to the other, inductively negative anomalies in the superficial temperature of the sea over the Central Pacific Tropicalconfiguring a state of La Niña.

¿What is the Meridional Circulation of the Atlantic?

The Atlantic Circulation of the Atlantic Flight, comprising a robust stream of superficial and profound currents, responsible for the superficial transport of agaves of the calyx and salads hacia the north and a stream of hacia in the deepest agave.

These “esters” of transport in excess and in depth are connected in the regions of “train”, where the currents flowing or rising, this is the oceanic circulation cell.

This is circulation transporting solid water from the equatorial atlantic ocean to the north atlantic ocean. This heat is captured by the atmosphere at higher altitudes and promotes a more temperate climate in some parts of Europe. Measures that the other side of the circulating wall is more aga fria hacia el sur, it permite that the tropics pierce the excess of heat. For tanto, is the ocean circulation playing an important paper in the equilibrium of the climatic system.

Los rair conditioners that are repaired to more than 100,000 years are revealed to be circulating well and to be “agape” or to be removed much longer during glaciation. Under the embargo, since the beginning of human civilization, 5,000 years ago, the transatlantic circulation of the Atlantic was relatively stable. With the exception of the last few, those that observe indications that they are circulating are being accelerated. ¿But for whom?

One of the main factors in the series is the direction of the polar caps from Greenland and Antarctica, which Large quantities of water lilies occur in the oceans, as the sea urchin grows very dense and reduces the density of dense water in the ‘fly’ regions at high latitudes.


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