Question: Who was the first European in America to see the source of the warm moist air mass over the Andes Mountains in Patito Feo's country?

<P0-S0> Patito Feo (in English, Ugly Duckling) is a comedy TV series for kids and teens from Argentina, starring Laura Natalia Esquivel, Brenda Asnicar, Juan Darthes, Griselda Siciliani, Gloria Carrá and Gastón Soffritti produced by Ideas del Sur for Canal 13. <P0-S1> The show is distributed worldwide by Televisa. <P0-S2> The opening theme, "Un Rincón del Corazón" ("A Corner of the Heart"), is sung by Patito played by Laura Natalia Esquivel. <SEP> <P1-S0> the innovation was adopted quickly and new features to air conditioning like the cadillac comfort control which was a completely automatic heating and cooling system set by dial thermostat was introduced as an industry first in the 1964 model year. <P1-S1> by 1960 about 20% of all cars in the u.s. had air - conditioning, with the percentage increasing to 80% in the warm areas of the southwest. <P1-S2> american motors made air conditioning standard equipment on all amc ambassadors starting with the 1968 model year, a first in the mass market, with a base price starting at $2,671. <P1-S3> by 1969, 54% of domestic automobiles were equipped with air conditioning, with the feature needed not only for passenger comfort, but also to increase the car's resale value. <SEP> <P2-S0> Although the centre and the eastern parts of the country are mostly flat, the west is mountainous. <P2-S1> Both the Andes and Sierras Pampeanas affect the climate of Argentina, leading to differences in temperature, pressure, and spatial distribution of precipitation depending on the topography and altitude. <P2-S2> Here, the Andes exert an important influence on the climate. <P2-S3> Owing to the higher altitudes of the Andes north of 40 S, they completely block the normal westerly flow, preventing low pressure systems containing moisture from the Pacific Ocean from coming in. <P2-S4> Thus, much of Argentina north of 40 S is dominated by wind circulation patterns from the South Atlantic High. <P2-S5> South of 40 S, the Andes are lower in altitude, allowing much of Patagonia to be dominated by westerly winds and air masses from the Pacific Ocean. <P2-S6> However, the north -- south orientation of the Andes creates a barrier for humid air masses originating from the Pacific Ocean. <P2-S7> This is because they force these air masses upwards, cooling adiabactically. <P2-S8> Most of the moisture is dropped on the Chilean side, causing abundant precipitation and cloudiness while on the Argentine side, the air warms adiabatically, causing it to become drier as it descends. <P2-S9> Thus, an extensive rain -- shadow is present in much of Patagonia, causing it to receive very little precipitation. <P2-S10> The Sierras Pampeanas influences the climate on a much smaller scale than the Andes. <SEP> <P3-S0> Explorers flying the flag of Spain reached the New World beginning in 1492 with the discovery of America by Christopher Columbus. <P3-S1> Spanish expeditions colonized and explored vast areas in North and South America following the grants of the Pope (contained in the 1493 papal bull Inter caetera) and rights contained in the 1494 Treaty of Tordesillas and 1529 Treaty of Zaragoza. <P3-S2> These formal acts gave Spain the exclusive rights to colonize the entire Western Hemisphere (excluding eastern Brazil), including all of the west coast of North America. <P3-S3> The first European expedition to actually reach the west coast was led by the Spaniard Vasco Núñez de Balboa, who reached the Pacific coast of Panama in 1513. <P3-S4> In an act of enduring historical importance, Balboa claimed the Pacific Ocean for the Spanish Crown, as well as all adjoining land and islands. <P3-S5> This act gave Spain exclusive sovereignty and navigation rights over the entire west coast of North America. <SEP> <P4-S0> tropical and equatorial air masses are hot as they develop over lower latitudes. <P4-S1> those that develop over land (continental) are drier and hotter than those that develop over oceans, and travel poleward on the western periphery of the subtropical ridge. <P4-S2> maritime tropical air masses are sometimes referred to as trade air masses. <P4-S3> monsoon air masses are moist and unstable. <P4-S4> superior air masses are dry, and rarely reach the ground. <P4-S5> they normally reside over maritime tropical air masses, forming a warmer and drier layer over the more moderate moist air mass below, forming what is known as a trade wind inversion over the maritime tropical air mass. <P4-S6> continental polar air masses (cp) are air masses that are cold and dry due to their continental source region. <P4-S7> continental polar air masses that affect north america form over interior canada. <P4-S8> continental tropical air masses (ct) are a type of tropical air produced by the subtropical ridge over large areas of land and typically originate from low - latitude deserts such as the sahara desert in northern africa, which is the major source of these air masses. <P4-S9> other less important sources producing ct air masses are the arabian peninsula, the central arid / semi-arid part of australia and deserts lying in the southwestern united states. <P4-S10> continental tropical air masses are extremely hot and dry.