paragraph_text: The Malton Range is a mountain range in southeastern British Columbia, Canada, located southwest of the Canoe Reach of Kinbasket Lake and east of the Albreda River, north of Dominion Mountain. It has an area of 451 km and is a subrange of the Monashee Mountains which in turn form part of the Columbia Mountains.

paragraph_text: The Badshot Range is a subrange of the Duncan Ranges of the Selkirk Mountains of the Columbia Mountains in southeastern British Columbia, Canada, located west of Duncan Lake and Westfall River east of Trout Lake.

paragraph_text: Otoroncane (possibly from Aymara "uturunqa, uturunqha, uturunqu, uturunqhu" tiger (here referring to the jaguar), "-ni" a suffix to indicate ownership, "the one with the jaguar") is a mountain in the Vilcanota mountain range in the Andes of Peru. It is situated in the Puno Region, Carabaya Province, Corani District. Otoroncane lies northwest of the mountains Pomanota, Jampatune and Sapanuta. The river Challapampa (possibly from Aymara for "sand plain") flows along its southern slopes.

paragraph_text: The Columbia Bar, also frequently called the Columbia River Bar, is a system of bars and shoals at the mouth of the Columbia River spanning the U.S. states of Oregon and Washington. The bar is about 3 miles (5 km) wide and 6 miles (10 km) long.

paragraph_text: The Klappan Range is a small subrange of the Skeena Mountains of the Interior Mountains, located between Klappan River and Iskut River in northern British Columbia, Canada.

paragraph_text: The area receives about 820 millimetres (32.3 in) of annual rainfall, which is concentrated from June through September/October with little or no precipitation the remainder of the year. The area has two main seasons. The rainy season runs from June to October when winds bring in tropical moisture from the sea. The dry season runs from November to May, when the air is relatively drier. This dry season subdivides into a cold period and a warm period. The cold period spans from November to February when polar air masses push down from the north and keep the air fairly dry. The warm period extends from March to May when tropical winds again dominate but do not yet carry enough moisture for rain.

paragraph_text: The Balkan mountains run laterally through the middle of the country. The mountainous southwest has two distinct alpine ranges—Rila and Pirin, which border the lower but more extensive Rhodope Mountains to the east. Musala, at 2,925 metres (9,596 ft), is the highest point in both Bulgaria and the Balkan peninsula, and the Black Sea coast is the country's lowest point. Plains occupy about one third of the territory, while plateaux and hills occupy 41%. Most rivers are short and with low water levels. The longest river located solely in Bulgarian territory, the Iskar, has a length of 368 kilometres (229 mi). Other major rivers include the Struma and the Maritsa in the south.Bulgaria has a changeable climate, which results from being positioned at the meeting point of the Mediterranean and continental air masses combined with the barrier effect of its mountains. Northern Bulgaria averages 1 °C (1.8 °F) cooler, and registers 200 millimetres (7.9 in) more precipitation, than the regions south of the Balkan mountains. Temperature amplitudes vary significantly in different areas. The lowest recorded temperature is −38.3 °C (−36.9 °F), while the highest is 45.2 °C (113.4 °F). Precipitation averages about 630 millimetres (24.8 in) per year, and varies from 500 millimetres (19.7 in) in Dobrudja to more than 2,500 millimetres (98.4 in) in the mountains. Continental air masses bring significant amounts of snowfall during winter.

paragraph_text: The Salloomt River is a river in the Bella Coola Valley of the Central Coast region of British Columbia, Canada. It is a tributary of the Bella Coola River, flowing southwest out of the southernmost Kitimat Ranges to meet that river just upstream from the community of Hagensborg.

paragraph_text: Klinaklini Canyon is a canyon on the Klinaklini River in the Pacific Ranges of the Coast Mountains in British Columbia, Canada, located to the north of the head of Knight Inlet in the river's lowermost reaches, upstream from the confluence of the West Klinaklini River.

paragraph_text: Although the centre and the eastern parts of the country are mostly flat, the west is mountainous. 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. Here, the Andes exert an important influence on the climate. 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. Thus, much of Argentina north of 40 S is dominated by wind circulation patterns from the South Atlantic High. 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. However, the north -- south orientation of the Andes creates a barrier for humid air masses originating from the Pacific Ocean. This is because they force these air masses upwards, cooling adiabactically. 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. Thus, an extensive rain -- shadow is present in much of Patagonia, causing it to receive very little precipitation. The Sierras Pampeanas influences the climate on a much smaller scale than the Andes.

paragraph_text: Hernán Gumy (born 5 March 1972) is a former tennis player from Argentina, who turned professional in 1991. He represented his native country at the 1996 Summer Olympics in Atlanta, Georgia, where he was defeated in the first round by Venezuela's Nicolas Pereira. Gumy made two finals in his career; both of them ATP 250s on clay in 1996. He won Santiago, Chile (his final tournament of 1996) by beating the Spanish World No. 15 Félix Mantilla in a tough three-setter: in the semi-finals, and the Chilean world number 11 Marcelo Ríos in the final 6-4, 7-5. He lost the other final he was in, in Oporto, Portugal to Spain's Félix Mantilla despite winning the first set.

paragraph_text: The Valhalla Ranges are a subrange of the Selkirk Mountains of the Columbia Mountains in southeastern British Columbia, Canada, located between Lower Arrow Lake of the Arrow Lakes and Slocan River.

paragraph_text: The Slamgeesh Range is a small subrange of the Skeena Mountains of the Interior Mountains, located between the Skeena River and Slamgeesh River in northern British Columbia, Canada.

paragraph_text: There is an average of forty - five inches of rain a year (fifty in the mountains). July storms account for much of this precipitation. As much as 15% of the rainfall during the warm season in the Carolinas can be attributed to tropical cyclones. Mountains usually see some snow in the fall and winter. Moist winds from the southwest drop an average of 80 inches (2,000 mm) of precipitation on the western side of the mountains, while the northeast - facing slopes average less than half that amount.

paragraph_text: The Driftwood Range is a small subrange of the Skeena Mountains of the Interior Mountains, located between the headwaters of Driftwood River and Nilkitkwa River in northern British Columbia, Canada.

paragraph_text: Taylor Pass is a mountain pass in the Chilcotin Ranges of the Coast Mountains of British Columbia, Canada, located at the divide between the headwaters of the Taseko River and those of Gun Creek, a tributary of the Bridge River.

paragraph_text: The Ratchford Range is a subrange of the Monashee Mountains of the Columbia Mountains, located east of the Seymour River in British Columbia, Canada.

paragraph_text: The Red River is a tributary of the Kechika River in the far north of British Columbia, Canada, flowing east to meet the Kechika from headwaters in the Cassiar Mountains. In its middle reaches it forms the boundary between the Dease Plateau (N) and the Cassiar Mountains (S) and for its final stretch it crosses part of the Liard Plain. It is crossed by an unnamed road about upstream from its confluence with the Kechika, and is just to the north of Aeroplane Lake.

paragraph_text: Tropical and equatorial air masses are hot as they develop over lower latitudes. 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. Maritime tropical air masses are sometimes referred to as trade air masses. Monsoon air masses are moist and unstable. Superior air masses are dry, and rarely reach the ground. 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. Continental Polar air masses (cP) are air masses that are cold and dry due to their continental source region. Continental polar air masses that affect North America form over interior Canada. 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. 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. Continental tropical air masses are extremely hot and dry.

paragraph_text: The Inambari River in southeastern Peru flows from the Cordillera Apolobamba in the Andes to the Madre de Dios River. The river spans the Puno and Madre de Dios regions.

Question: Where does the columbia river meet the body of water where warm moist air mass over the Andes in the country Hernán Gumy originates?
Answer: Columbia Bar