Respuesta:
A, C, D
Clarificación:
La Corriente del Golfo es una corriente oceánica caliente en el Atlántico que transporta agua cálida desde los trópicos hacia las latitudes más norteñas de Europa Occidental. El impacto de esta corriente en el clima de la parte occidental del continente europeo es enorme. Muchas ciudades europeas que se encuentran en latitudes similares a ciudades canadienses con climas subpolares disfrutan de climas moderados gracias al efecto que tiene la Corriente del Golfo, que disminuye los efectos de continentalidad y de latitud alta que tendría su ubicación.
Answer:
C. Isasaalang-alang ko ang klimatiko ng isang lugar.
Paliwanag:
Ang pinakamainam na paraan upang paghiwalayin ang isang rehiyon ay batay sa klima dahil ang bawat rehiyon ay may natatanging klima dahil sa taas at distansya mula sa ekwador. Ang mga rehiyon na nasa mataas na lugar ay may malamig na klima, habang ang mga nasa ekwador o malapit dito ay may mainit at humid na kondisyon; mula rito, makikita natin na ang klima ang isang mahalagang salik sa paghahati ng mga rehiyon.
Answer:
y = 32,000 + 2560(x)
Explanation:
After maintaining a stable population of 32,000 for several years, an exponential growth of 8% from 32,000 occurs in the next year, raising the population to 34560.
To calculate this,
8% of 32000 = 8/100 × 32000 = 2560
Now, adding this growth to the original population results in:
2560 + 32000 = 34, 560
The figure of 34560 represents the population after 1 year.
To predict the town's population over x years, expressed with y as the population, the following formula can be applied:
y = 32,000 + 2560(x)
Testing the equation with values of x = 4 years and 3 years yields:
y = 32,000 + 2560(4) = 32,000 + 10240 = 42240 people will reside in the town in four years
y = 32,000 + 2560(3) = 32,000 + 7680 = 39680 people will reside in the town in three years.
Ang anyo ng silangang asya ay hindi regular, karaniwang pook ito ay bundok, at may ilang bahagi rin na pabilog o maburol.
The response is a fjord/fiord coastline. Such coastlines are formed by the submersion of U-shaped glacial troughs and are characterized by profound waters; generally, the fjord's inlet is relatively shallow, alongside steep high cliffs that rise sharply from the water, with tributaries meeting the main inlet at right angles. This type of coastline is exclusively found in areas with fjords.
