The first climograph (A) shows average monthly temperatures and precipitation. The blue bars represent precipitation, and the red line represents temperature. The precipitation is highest in the summer months and lowest in the winter months. The temperature is coldest in winter, with average temperatures below -20°C, and warmest in summer, with average temperatures around 10°C. The total annual precipitation is 724 mm. This type of climate is characterized by cold winters, warm summers, and significant precipitation, especially in summer. Considering the provided list of climate zones/types, this pattern is most consistent with a humid continental climate with a monsoon influence. The second climograph (B) also shows average monthly temperatures and precipitation. The precipitation is generally low throughout the year, with a slight increase in summer. The temperature is cold in winter, with average temperatures below -20°C, and mild in summer, with average temperatures around 20°C. The total annual precipitation is 481 mm. This type of climate, with cold, dry winters and relatively mild, wet summers, is characteristic of a moderate continental climate with continental features. The provided list includes 'умеренный / континентальный' and 'умеренный / резко континентальный'. Given the overall cold winter temperatures and relatively moderate summer temperatures with lower precipitation, this leans towards a continental climate. However, without more specific information or precise geographical context for 'A' and 'B', distinguishing between continental and sharply continental can be nuanced. Generally, Murmansk is known for its subarctic or tundra climate, while Vladivostok has a monsoon climate. Let's re-evaluate based on typical climate characteristics of these cities, which are mentioned in the text. Murmansk, located in the Arctic region, has a subarctic or tundra climate, characterized by very cold winters and short, cool summers. Vladivostok, on the Pacific coast, has a monsoon climate, with cold, dry winters and warm, humid summers. Looking at climograph A, the very low winter temperatures (below -20°C) and relatively cool summers (around 10°C) with high precipitation (724 mm), especially in summer, are more indicative of a subarctic or tundra climate. Climograph B shows very cold winters (below -20°C) and warmer summers (around 20°C) with moderate precipitation (481 mm), particularly a dry winter and wetter summer. This is characteristic of a monsoon climate. Therefore, let's match the climographs to the cities and then to the climate types. If A represents Murmansk, it would be subarctic. If B represents Vladivostok, it would be temperate monsoon. Now, let's map these to the provided list: 'арктический', 'субарктический', 'умеренный / морской', 'умеренный / континентальный', 'умеренный / резко континентальный', 'умеренный / муссонный', 'субтропический'. Climograph A: Very cold winters, cool summers, high precipitation, particularly in summer. This strongly suggests a subarctic climate. Climograph B: Cold winters, warmer summers, dry winters, wet summers, moderate total precipitation. This strongly suggests a temperate monsoon climate. Thus, A corresponds to 'субарктический' and B corresponds to 'умеренный / муссонный'. The problem asks to identify the climatic zone/type for each climograph. Based on the typical climates of Murmansk (subarctic) and Vladivostok (monsoon), and observing the provided climographs: Climograph A shows very cold winters and cool summers with substantial precipitation, fitting a subarctic climate. Climograph B shows cold winters and warmer summers with a distinct dry winter and wet summer pattern, fitting a temperate monsoon climate. Therefore, A is subarctic, and B is temperate monsoon.