Altitude shows the height from earth. when Aeroplanes flying in the sky, Pilot announces we are flying at an altitude of 30,000 feet.
Altitude is your height above sea level.
the lenght meassure for one feet is 12 inches wether in longitud or altitud. For example a 6.5 feet measuring person is concidered tall.
Yeah yeah next you will ask why is arctic cold and Africa hot
Ang uri ng klima ng isang lugar ay may kinalaman sa iba't ibang salik tulad ng latitud, altitud, at proximity ng lugar sa mga anyong tubig. Ang latitud ay nakakaapekto sa sikat ng araw na natatanggap ng isang lugar, samantalang ang altitud ay maaaring magdulot ng mas malamig na temperatura. Ang mga anyong tubig, tulad ng dagat at karagatan, ay nakakatulong sa pag-regulate ng temperatura at halumigmig, na nagreresulta sa iba’t ibang uri ng klima. Gayundin, ang mga hangin at mga sistemang panahon ay may papel sa pagbuo ng tiyak na klima sa isang rehiyon.
they can jump as far as 5000 meters hotizontal but vertical they can reach an altitud of 100 000 000 meters
the temperatures increase as altitud incresesatoms of nitrogen and oxygen absorb higer-energy solar radiation and release thermal energy, which causes temperatures in the thermospher to be 1,000degrees C
Ang klima ng Indonesia ay tropikal, na may dalawang pangunahing panahon: tag-ulan at tag-init. Ang tag-ulan ay karaniwang nagaganap mula Nobyembre hanggang Marso, habang ang tag-init ay mula Abril hanggang Oktubre. Ang temperatura ay mainit at mataas, na karaniwang umaabot ng 25°C hanggang 30°C. Ang klima ay nag-iiba-iba sa bawat rehiyon, na may mga lugar na mas basa at may mataas na altitud na mas malamig.
Un valle es una depresión de terreno entre dos montañas o montes, mientras que una llanura es una extensión de terreno plano o ligeramente ondulado. Los valles suelen ser más estrechos y alargados, con una mayor variabilidad en la altitud del terreno, mientras que las llanuras son más extensas y uniformes en su topografía. Los valles suelen estar atravesados por ríos o arroyos, mientras que las llanuras son propicias para la agricultura.
Ang mga anyong-lupa na mainam taniman ng pananim ay ang mga patag na lupa o kapatagan, tulad ng mga lambak at baybayin ng ilog, dahil ito ay mayaman sa lupa at madaling maabot ng sinag ng araw. Ang mga burol at bundok na may angkop na klima at lupa ay maaari ring maging mabuting taniman, lalo na sa mga pananim na nangangailangan ng mas mataas na altitud. Mahalagang isaalang-alang ang uri ng lupa, pagkakaroon ng tubig, at klima upang masiguro ang matagumpay na pagtatanim.
Ang gulay ang pangunahing produkto sa mga lugar na matataas tulad ng lalawigan ng bulubundukin at lambak ng Trinidad dahil sa malamig na klima na angkop para sa pagtatanim ng iba't ibang uri ng gulay. Ang fertile na lupa sa mga bulubundukin ay nagbibigay ng magandang kondisyon para sa paglago ng mga pananim. Bukod dito, ang mataas na altitud ay nagpoprotekta sa mga gulay mula sa mga peste at sakit, na nagreresulta sa mas mataas na ani. Ang mga lokal na komunidad ay umaasa sa mga produktong gulay na ito para sa kanilang kabuhayan at nutrisyon.
Yes it is. Heat from the sun warms up lakes, rivers, and the oceans as well as land surfaces such as forests, grass and croplands. These surfaces then heat the air above them. This heated air rises drawing up water the water from these surfaces into the air. Air heats up differently over different surfaces, and this is what causes the wind. The warming air rises creating a low pressure center, where as a nother surface is cooler and the colder air aloft sinks creating a high pressure center. Wind is the energy of moving air from the cooler high to the warmer low. As the warmer air rises, it begins to cool and as it cools the amount of water in can hold drops. When it reaches a certain altitude and the the colder air can no longer hold the water it contains, it condenses out as clouds. Air moving aloft, like the jet stream; high altitud high speed winds move the clouds along as more and more air is drawn up into the clouds the updraft winds can no longer hold the water aloft and it falls as rain or snow. If rain falls through a cold layer of air it could be cooled down to then fall to the ground as sleet. It becomes freezing rain only if it falls as liquid and hits the surfaces on the ground and immediately freezes on impact. The rain hits the ground and soaks in down to the water table. Some drains off into rivers and lakes or directly onto these bodies of water and oceans too. Rivers carry this water to the oceans and still more water waters the trees and the grasses and our crops. The warmth draws moisture up out of the ground into the plants and up from the plants back into the air forming clouds, the same directly from the lakes and rivers and oceans. And the water cycle starts all over again. But without energy transfer, the water cycle can't work. The heat energy of the sun is transferred into other forms of energy by the land, plants and other surfaces which then is converted kinetic energy as the air rises. This heat energy tranferring from one source to another, as well as converting one form of energy to another form. So you actually have two diferent energy connections to the water cycle, energy transfer and energy conversion.
El Rio Camuy.RÍO CAMUY- se origina en el río en la Cordillera Central al noroeste de Puerto Rico. Fluye generalmente con dirección norte hacia el océano Altlántico por una distancia de 30km. El este del pueblo de Lares entra en un cañon estrecho. El cañon termina en forma abrupta en el sumidero"Blue Hole" donde el Río Camuy se VA subterráneos. Es visto nuevamente al fondo del sumidero Espiral, 200 metros al nortoeste de este sumidero aparece de nuevo al fondo del sumidero de Tres Pueblos, fluyendo desde el noreste a través de él como 100 metros y luego se VA subterráneo. Aparece brevemente al fondo del sumidero Empalme, lléndose subterráneso nuevamente para aparecer en el valle 800 metros al norte de este sumidero. Desde ese punto, fluye hacia el norte sobre la superficie hasta el océano Atlántico. El Río Camuy tiene un área de capacitación de aproximadamente 62 millas cuadradas. Cruza por los municipios de Utuado, Lares. Hatillo y Camuy.
Low pressure areas form when an airmass warms, either from being over a warm land or ocean surface, or from being warmed by condensation of water vapour in large rain or snow systems. The warming causes the air layer to expand upward, becoming slightly thicker. This expansion then causes air in the upper troposphere to flow away, leaving less mass, and so less weight (pressure) at the surface. The lower pressure air at the surface then causes higher pressure air around it to flow toward lower pressure, but as it does, the rotation of the Earth turns the wind to the right, resulting in the counter-clockwise wind flow around low pressure (in the Northern Hemisphere...it flows in the opposite direction in the Southern Hemisphere). High pressure areas form when an airmass cools over a cool land or ocean surface. The cooling causes the air layer to shrink, becoming slightly thinner. This shrinkage then causes surrounding air in the upper troposphere to fill up the extra space. The added weight of the extra air causes higher pressure at the surface. The higher pressure air at the surface then tries to flow outward toward lower pressure, but as it does, the rotation of the Earth turns the wind to the right, resulting in the clockwise wind flow around the high pressure (in the Northern Hemisphere...it flows in the opposite direction in the Southern Hemisphere).