We have centuries studying the different types of clouds. What tells us the shape and color of these atmospheric phenomena

The atmosphere of the earth hides about 12.9 billion liters of watermore or less. And a good part of that water is in huge clouds that we see fly over our heads as if nothing. These huge atmospheric objects captivate our imagination in childhood, but we often stop thinking about them during our day. Knowing them can help us pay attention to them. What is a cloud The clouds are essentially water, a lot of water. Steam -shaped water, small drops and Even small ice crystals that remain in suspension in the atmosphere. This water becomes visible when condensed, generating a contrast with the blue of the sky. The clouds circulate in the atmosphere dragged through the differences in pressure and the wind that they generate. They also move as a result of the land rotation itself, since the solid surface of the earth does not rotate in the same way as the atmosphere. The clouds can be of very different types that we classify according to certain conditions, such as the height to which they occur. For example, when the clouds are formed at surface height, we do not even usually refer to them as such, but as a fog. But the fog is still a type of cloud. How a cloud is formed The atmosphere keeps water vapor, small H2O molecules that are mixed with the other gases that make up the atmosphere. The amount of water that the atmosphere can store in the form of gas depends on factors such as temperature and pressure. There is a threshold from which the atmosphere Water “sat”and that is when this water can begin to accumulate. This accumulation is good when the amount of water increases or because atmospheric conditions make the threshold reduce, and implies that the molecules go from being a gas in suspension to form microscopic water drops. When these drops, still in suspension, accumulate, the clouds are formed. Types of clouds and characteristics The clouds are usually classified according to two fundamental characteristics: Your altitude in the atmosphere and its appearance. According to its altitude, three types of clouds are distinguished (with an additional case), groups that the State Meteorology Agency (Aemet) call of “high floor” (the highest altitude), of “middle floor” (intermediate altitude) and those of low floor (those of minor antura), to which we must add the clouds of vertical development. There are different terms with which referring to these clouds, for example we can speak sympleously of high, medium and low clouds. High floor clouds The high -floor clouds are those that are at heights between 5 and 13 kilometers on the ground, and include cirro, circoum and cirrostrates. Cirrus: According to Explain Aemetcirrus are clouds of the high floor, separate and “in the form of white and delicate filaments, or banks or narrow, white or almost white bands.” Cirrus. Piccolonamek, Commons. CIRCOUM: It is a thin layer of clouds, white and shadowless, “very small elements” in the form of grains or undulations. Circummers. King of Hearts. CIRROSTRATE: These clouds for their part acquire the appearance of a “cloudy veil”, also transparent and rather white, only that this type of clouds covers the sky, totally or partially, producing “halos.” Cirros and its characteristic halo. SeanMack Medium floor clouds The clouds of the middle floor are located at heights between two and seven kilometers, and can also be of various types: altocumulos, high, and nimbostratos. Altocúmulos: The altocumulus are already located at medium heights. It is a bank or cloud layer that can be white or gray. Its structure can varybeing formed by “tiles”, “rounded masses” or “rollers”, structures that, in turn, can be “partially fibrous or diffuse,” Explain Aemet. Altocumulos. Bidgee Altostrates: This layer of clouds usually has gray or bluish colors, it can also have a fibrous appearance, it is characterized by totally or partially covering the sky allowing to distinguish vaguely, but unlike cirrostrates, it does not produce halos. Altostrates. Famartin. Nimbostrates: These clouds form an already dark gray layer, with “appearance veiled by rainfall or snow precipitation”, rainfall that usually falls from it more or less continuously. Nimbostratos. Famartin. Low floor clouds The low floor clouds are those located at heights of up to two kilometers and can be of two types: strata and strata. Stratocumulous: Again clouds that can acquire a gray color, or, on other occasions, whitish with dark parts. Stratocumulous. DjClimber. Strata: Generally gray clouds, uniform base (relatively), which can produce drizzle. The halos in this cloud only occur when very low temperatures are reached. Strata. Couch-Scratching-Cats. Vertical Development Clouds Finally, vertical development clouds can also be of two types: clusters and cumulonimbos. Clusters: These are clouds that arise in isolation, dense and well -defined contours. These clouds develop vertically with the form of “protuberances”, “domes” or “towers.” Clusters. Piccolonamek. Cumulonimbos: Finally, the cumulonimbos are clouds that Aemet describes as “Amazacotadas and Dense”, of vertical development “in the form of a mountain or huge towers.” On his cusp, a top “smooth, fibrous or striated.” Cumulonimbos. NOAA/AOML/Hurricane Research Division. How much water is there in a cloud? The clouds are ethereal objects, “cotton” and with a density low enough to keep afloat at a certain height in the atmosphere. However, they are also huge, so the amount of water they can house is enormous. A few years ago, a group of researchers proposed answer the question How much water is in a cloud. The truth is that the answer can vary greatly since the volume of these atmospheric phenomena can be the most diverse. However, the team made an estimate based on a 0.5 grams of water per cubic meter of cloud. The team took as reference an average cluster, an cloud that would have a cubic shape and a kilometer long. The result: this imaginary cloud would contain about 500 tons of water. Larger clouds, of course, would be able to house an even greater amount of water. In Xataka | “We are changing the clouds”: … Read more

It is so hot in Granada that there has been one of the most extreme phenomena of the weather: thermal burst

This Sunday on the Tropical Costa de Granada An unusual phenomenon has been recordedbut it has caused great ravages. While people were trying to pass in the water the heat wave in which we are now, in a few minutes everything changed to have a hurricane and scorching wind on top. It reached such a speed that made the umbrellas and chairs shot as projectiles. And it was not a simple summer storm, but a phenomenon known as thermal burst. What happened on the Granada coast. The sequence of the facts was dizzying. Shortly before 19:45, 112 emergency services The first calls began to receive Notice. The alerters, from different points of the Tropical Costa, talked about hurricane winds that even threw palm trees of the promenade. The climax of the phenomenon, According to the Aemet, It was recorded at 19:50 with a temperature that shot sharply until 40.1 ° C. Jointly, wind gusts reached a speed of 86.8 km/h officially, although in different social networks users suggest that these speeds They reached 100 km/h. A phenomenon that concentrated in different municipalities such as Motril, Salobreña, Torrenueva, Carchuna and Almuñécar. Click on the image to access the publication. Chaos on the beach and bailouts in the sea. Shared testimonies on social networks paint a collective horror picture. A citizen He reported: “I was there on the beach and the situation has been horrible, I have not had worse in my life.” The disseminated images In social networks they showed people running to their cars, which caused traffic jams on the exit roads of the coast. Although the greatest danger materialized in the water. The rapid evolution of this meteorological phenomenon caused people to practice aquatic sports, and the wind caught several people who saw how they crawled inside and preventing returning to the shore by their own means. This triggered an operation where Seven people had to be rescued in front of the beaches of Torrenueva Costa and Carchuna. A rescue that was carried out by maritime rescue, but also by private vessels that prevented this situation from becoming a great tragedy. A rapid official response. Given the violence of such an unpredictable phenomenon, the beaches of the affected municipalities They had to be evacuated. At 20:20, the mayor of Motril, Luisa García Chamorro, launched an urgent notice Through its social networks which reflected the seriousness of the situation, asking not to go outside and have a lot of caution. A term comfort does not arise from nothing. They require an atmospheric configuration Very specifica “recipe” that this Sunday was perfect in Granada. The main ingredient was The extreme heat accumulated during the prolonged heat wave. This heat not only affected the surface, but created a deep layer of very hot air, and crucially very dry at the average levels of the atmosphere, several kilometers high from where the burst was given. Meanwhile, on the sea, the air in contact with the water was comparatively cooler and more humble. This stratification with a very hot and dry air in height on a cooler and more wet layer near the surface is the ideal culture broth. The scenario was completed with the formation of convective storms on the mountains of the interior of Granada, which acted as the trigger for the process. Of the rain that never falls to the scorching wind. The process of formation of a thermal burst is a fascinating paradox of thermodynamics, where a process that begins with an external cooling culminates in a burst of scorching heat. It can be broken down into four key steps According to the Aemet technical guides: The descendant current: everything begins within a storm cloud where a powerful current of descending air is generated that drags rainfall. Sudden evaporation: As this column of air and rain plummets, it meets the extremely dry and hot air layer that had been formed before. The dry air ‘absorbs’ voraciously all precipitation, causing it to evaporate completely before reaching the ground, something that is known as ‘virga’. Evaporation is a process that consumes energy, abruptly cooling the air of the descending column. This air, now much colder and dense than the one that surrounds it, collapses towards the ground at a dizzying speed. Compression warming: Once all the water has evaporated, the cooling process ceases. The air column, and if “refrigerant”, continues its free fall. When descending, atmospheric pressure quickly increases by compressing the mass of air. This compression is client at an extraordinary pace, known as dry adiabatic gradient. The impact or burst. Finally, this extremely hot, dense and dry air bubble violates the ground, like an invisible hammer. Unable to continue descending, it expands horizontally in all directions at high speed, generating destructive and sudden wind gusts and intense temperature rise that characterizes the phenomenon. It is not the same as a tornado. Sometimes this phenomenon can be confused with a tornado, but There are differences. While in the tornado the wind revolves around a vertical axis, in the bursting the winds are descending and linear. Climate change will make them more frequent. Thermal bursts are a natural phenomenon, but climate change is causing them to be more frequent. The report of the IPCC scientific experts It is unequivocal: heat waves are now more frequent, more durable and more intense due to global warming. The Granada event was no exception. It was the culmination of a historical heat wave in Andalusia. As explained before, the temperature is the fundamental ingredient that creates and dry the necessary atmospheric layer for the thermal burst to activate. An ordinary storm, in a less extreme environment, could have generated a cold front that refreshes the environment. However, when interacting with an “prepared” atmosphere by anomalous heat, the result was the violent explosion of scorching air. More energy and more extreme. The connection goes beyond heat waves. One of the most direct consequences of the increase in global temperatures is that the atmosphere can retain more … Read more

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