the humidity in coastal areas is usually
Because of the drastic changes in relative humidity inside the vehicle, components must be qualified to operate in those environments. w This effect is calculated as the heat index or humidex. Scientists at Columbia Universitys Earth Institute estimate that, worldwide, the number of people living within 60 miles of a coast will rise 35 percent by the year 2025 compared to 1995 levels. ASHRAE Standard 55 (2017). For example, a maximum of about 30 grams of water vapor can exist in a cubic meter volume of air with a temperature in the middle 80s. Even though it is an inanimate object, the existence of these components can affect the survival of living things around the coastal ecosystem. Relative humidity is normally expressed as a percentage; a higher percentage means that the airwater mixture is more humid. Abu Dhabi: Humidity levels have risen at night in the coastal areas of the UAE since Friday and are expected to remain on the higher side over the next few days. If significant, these added factors help explain why rainfall totals from thunderstorms can exceed actual PW values of the air in which the storms are occurring. [36] In general, higher temperatures will require lower humidities to achieve thermal comfort compared to lower temperatures, with all other factors held constant. 1-Stop Climate , which can be expressed as: The absolute humidity changes as air temperature or pressure changes, if the volume is not fixed. 8. Air Masses and Fronts WebThe word that describes humidity (maritime or continental) is paired with the word that describes temperature (equatorial, tropical, polar or arctic). Humans are sensitive to humid air because the human body uses evaporative cooling as the primary mechanism to regulate temperature. 2 The humidity in coastal areas is usually than that of the Weather Radio The gravimetric method, while the most accurate, is very cumbersome. It's near giant bodies of water, heat takes up water vapor at that point, and voila, you have humidity in abundance In contrast, a very low humidity level favors the build-up of static electricity, which may result in spontaneous shutdown of computers when discharges occur. [39] Extremely low (below 20%) relative humidities may also cause eye irritation. Nearness of a large body of water which adds to the moisture content of the atmosphere making it humid. Cloud condensation nuclei lower the level of supersaturation required to form fogs and clouds - in the absence of nuclei around which droplets or ice can form, a higher level of supersaturation is required for these droplets or ice crystals to form spontaneously. All humidity sensors face problems in measuring dust-laden gas, such as exhaust streams from clothes dryers. ten hottest places on earth (highest average monthly temperature) describes the temperature measured both in degrees Celsius and Fahrenheit as well the month of the year for selected countries with climate extremes. Therefore, some of the abiotic components possessed by the coastal ecosystem include sand, land, temperature, air, humidity, rocks, and also sunlight. The air is able to pick up water from the ocean, the water in the air makes it more humid. mostly tropical, but temperate in south. Decision Support Page When the humidity is slight (Figure 5a), under the influence of northeasterly airflow, the AOD in the Guangxi area is high, but the effect of the GBA is relatively small, for which the AOD is 0.61. The term relative humidity is reserved for systems of water vapor in air. By comparison, thermal comfort standard ASHRAE 55 requires systems designed to control humidity to maintain a dew point of 16.8C (62.2F) though no lower humidity limit is established.[46]. Although weather conditions affect people differently, in general in the spring and summer, surface dewpoint temperatures in the 50s usually are comfortable to most people, in the 60s are somewhat uncomfortable (humid), and in the 70s are quite uncomfortable (very humid). For a given dew point and its corresponding absolute humidity, the relative humidity will change inversely, albeit nonlinearly, with the temperature. In the winter, there is another index we use to determine how cold our bodies feel when we are outside. Brainstorm and discuss the pros of coastal living. This index combines the effect of the air temperature with the speed of the wind. If the system at State A is isothermally compressed (compressed with no change in system temperature), then the relative humidity of the system increases because the partial pressure of water in the system increases with the volume reduction. of water at the same temperature, usually expressed as a percentage:[11][12][5]. Weather Averages in Oregon Coast O NOAA's Ten Signs of a Warming World: Humidity For example, a parcel of air near saturation may contain 28 g of water per cubic metre of air at 30C (86F), but only 8 g of water per cubic metre of air at 8C (46F). National Oceanic and Atmospheric Administration A device used to measure humidity of air is called a psychrometer or hygrometer. Relative humidity increases as well, going from 33% in June, to 55% in July, and to 51% in August and September, thus making the heat sweltering. mostly temperate, but tropical in Hawaii and Florida, arctic in Alaska, semiarid in the great plains west of the Mississippi River, and arid in the Great Basin of the southwest; low winter temperatures in the northwest are ameliorated occasionally in January and February by warm chinook winds from the eastern slopes of the Rocky Mountainsnote: many consider Denali, the highest peak in the US, to be the worlds coldest mountain because of its combination of high elevation and its subarctic location at 63 degrees north latitude; permanent snow and ice cover over 75 percent of the mountain, and enormous glaciers, up to 45 miles long and 3,700 feet thick, spider out from its base in every direction; it is home to some of the worlds coldest and most violent weather, where winds of over 150 miles per hour and temperatures of -93F have been recorded. Such short circuits may cause substantial permanent damage if the equipment is powered on before the condensation has evaporated. [46] However, the recommended range of indoor relative humidity in air conditioned buildings is generally 3060%. Without other greenhouse gases, Earth's blackbody temperature, below the freezing point of water, would cause water vapor to be removed from the atmosphere. As the temperature of a parcel of air decreases it will eventually reach the saturation point without adding or losing water mass. Absolute humidity is the total mass of water vapor present in a given volume or mass of air. Houston, Miami, San Diego, Osaka, Shanghai, Shenzhen and Tokyo also have an extreme humid period in their summer months. Event Ready A major source of water vapor in Kentucky is the Gulf of Mexico. Relative humidity only considers the invisible water vapour. As a condensible greenhouse gas, it precipitates, with a much lower scale height and shorter atmospheric lifetime weeks instead of decades. In general, the higher the PW, the higher the potential for very heavy rain from thunderstorms if they were to develop. Find an answer to your question The humidity in coastal areas is usually.. than that of the inland areas. Ile Amsterdam et Ile Saint-Paul: oceanic with persistent westerly winds and high humidity; Iles Crozet: windy, cold, wet, and cloudy; Iles Kerguelen: oceanic, cold, overcast, windy; tropical; hot, rainy season (June to November); cooler, dry season (November to May), temperate, mild winters, dry and warm to hot summers, warm and pleasant; Mediterranean-like on Black Sea coast, temperate and marine; cool, cloudy, wet winters and summers; occasional warm mountain (foehn) wind, tropical; warm and comparatively dry along southeast coast; hot and humid in southwest; hot and dry in north, Mediterranean with mild winters and warm summers, temperate; mild, wet winters; hot, dry summers, arctic to subarctic; cool summers, cold winters, tropical; tempered by northeast trade winds, tropical marine; generally warm and humid, moderated by northeast trade winds; dry season (January to June), rainy season (July to December); little seasonal temperature variation, tropical; hot, humid in lowlands; cooler in highlands, temperate with mild winters and cool summers; about 50% of days are overcast, generally hot and humid; monsoonal-type rainy season (June to November) with southwesterly winds; dry season (December to May) with northeasterly harmattan winds, tropical; generally hot and humid; monsoonal-type rainy season (June to November) with southwesterly winds; dry season (December to May) with northeasterly harmattan winds, tropical; hot, humid, moderated by northeast trade winds; two rainy seasons (May to August, November to January), tropical; semiarid where mountains in east cut off trade winds, temperate; mild, rainy winters (September to May) with hot, dry summers (May to September), subtropical in lowlands, temperate in mountains, subtropical monsoon; cool and humid in winter, hot and rainy from spring through summer, warm and sunny in fall, temperate; cold, cloudy, humid winters; warm summers, temperate; moderated by North Atlantic Current; mild, windy winters; damp, cool summers, varies from tropical monsoon in south to temperate in north, northeast monsoon (December to April), southwest monsoon (June to October); tropical cyclones occur during May/June and October/November in the northern Indian Ocean and January/February in the southern Indian Ocean, tropical; hot, humid; more moderate in highlands, mostly arid or semiarid, subtropical along Caspian coast, mostly desert; mild to cool winters with dry, hot, cloudless summers; northern mountainous regions along Iranian and Turkish borders experience cold winters with occasionally heavy snows that melt in early spring, sometimes causing extensive flooding in central and southern Iraq, temperate maritime; modified by North Atlantic Current; mild winters, cool summers; consistently humid; overcast about half the time, temperate; cool summers and mild winters; overcast about a third of the time, temperate; hot and dry in southern and eastern desert areas, predominantly Mediterranean; alpine in far north; hot, dry in south, arctic maritime with frequent storms and persistent fog, varies from tropical in south to cool temperate in north, mostly arid desert; rainy season in west (November to April), continental, cold winters and hot summers, arid and semiarid, varies from tropical along coast to arid in interior, tropical; marine, hot and humid, moderated by trade winds, temperate, with rainfall concentrated in summer; long, bitter winters, temperate, with rainfall heavier in summer than winter; cold winters, influenced by continental air masses resulting in relatively cold winters with heavy snowfall and hot, dry summers and autumns; Mediterranean and alpine influences create regional variation; maximum rainfall between October and December, dry desert; intensely hot summers; short, cool winters, dry continental to polar in high Tien Shan Mountains; subtropical in southwest (Fergana Valley); temperate in northern foothill zone, tropical monsoon; rainy season (May to November); dry season (December to April), Mediterranean; mild to cool, wet winters with hot, dry summers; the Lebanon Mountains experience heavy winter snows, temperate; cool to cold, dry winters; hot, wet summers, tropical; hot, humid; dry winters with hot days and cool to cold nights; wet, cloudy summers with frequent heavy showers, Mediterranean along coast; dry, extreme desert interior, continental; cold, cloudy winters with frequent snow or rain; cool to moderately warm, cloudy, humid summers, transitional, between maritime and continental; wet, moderate winters and summers, modified continental with mild winters, cool summers, subtropical; marine with cool winters, warm summers, tropical along coast, temperate inland, arid in south, sub-tropical; rainy season (November to May); dry season (May to November), tropical; annual southwest (April to October) and northeast (October to February) monsoons, tropical; hot, humid; dry, northeast monsoon (November to March); rainy, southwest monsoon (June to August), subtropical to arid; hot and dry (February to June); rainy, humid, and mild (June to November); cool and dry (November to February), Mediterranean; mild, rainy winters; hot, dry summers, tropical; hot and humid; wet season May to November; islands border typhoon belt, tropical, modified by southeast trade winds; warm, dry winter (May to November); hot, wet, humid summer (November to May), tropical; heavy year-round rainfall, especially in the eastern islands; located on southern edge of the typhoon belt with occasionally severe damage, Mediterranean with mild, wet winters and hot, dry summers, desert; continental (large daily and seasonal temperature ranges), Mediterranean climate, hot dry summers and autumns and relatively cold winters with heavy snowfalls inland, tropical; little daily or seasonal temperature variation, Mediterranean in the north, becoming more extreme in the interior; in the south, hot, dry desert; rain is rare; cold offshore air currents produce fog and heavy dewnote: data does not include former Western Sahara, desert; hot, dry; rainfall sparse and erratic, tropical with a monsoonal pattern; rainy season (November to February), varies from cool summers and severe winters in north to subtropical summers and mild winters in south, temperate; marine; cool summers and mild winters, tropical; modified by southeast trade winds; hot, humid, tropical in lowlands, cooler in highlands, desert; mostly hot, dry, dusty; tropical in extreme south, varies; equatorial in south, tropical in center, arid in north, tropical; modified by southeast trade winds, subtropical; mild, little seasonal temperature variation, warm, dry summers and autumns; relatively cold winters with heavy snowfall, tropical marine; moderated by northeast trade winds, little seasonal temperature variation; dry season December to June, rainy season July to October, temperate along coast, modified by North Atlantic Current; colder interior with increased precipitation and colder summers; rainy year-round on west coast, dry desert; hot, humid along coast; hot, dry interior; strong southwest summer monsoon (May to September) in far south, planetary air pressure systems and resultant wind patterns exhibit remarkable uniformity in the south and east; trade winds and westerly winds are well-developed patterns, modified by seasonal fluctuations; tropical cyclones (hurricanes) may form south of Mexico from June to October and affect Mexico and Central America; continental influences cause climatic uniformity to be much less pronounced in the eastern and western regions at the same latitude in the North Pacific Ocean; the western Pacific is monsoonal - a rainy season occurs during the summer months, when moisture-laden winds blow from the ocean over the land, and a dry season during the winter months, when dry winds blow from the Asian landmass back to the ocean; tropical cyclones (typhoons) may strike southeast and east Asia from May to December, mostly hot, dry desert; temperate in northwest; arctic in north, tropical; hot and humid; wet season May to November, tropical maritime; hot, humid, cloudy; prolonged rainy season (May to January), short dry season (January to May), tropical; northwest monsoon (December to March), southeast monsoon (May to October); slight seasonal temperature variation, subtropical to temperate; substantial rainfall in the eastern portions, becoming semiarid in the far west, varies from tropical in east to dry desert in west; temperate to frigid in Andes, tropical marine; northeast monsoon (November to April); southwest monsoon (May to October), tropical; hot and humid; modified by southeast trade winds; rainy season (November to March), temperate with cold, cloudy, moderately severe winters with frequent precipitation; mild summers with frequent showers and thundershowers, maritime temperate; cool and rainy in north, warmer and drier in south, tropical marine, mild; little seasonal temperature variation, temperate; cold, cloudy winters with frequent snow and fog; sunny summers with frequent showers and thunderstorms, ranges from steppes in the south through humid continental in much of European Russia; subarctic in Siberia to tundra climate in the polar north; winters vary from cool along Black Sea coast to frigid in Siberia; summers vary from warm in the steppes to cool along Arctic coast, temperate; two rainy seasons (February to April, November to January); mild in mountains with frost and snow possible, tropical, with practically no variation in temperature; has two seasons (dry and humid). 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Because of the drastic changes in relative humidity inside the vehicle, components must be qualified to operate in those environments. w This effect is calculated as the heat index or humidex. Scientists at Columbia Universitys Earth Institute estimate that, worldwide, the number of people living within 60 miles of a coast will rise 35 percent by the year 2025 compared to 1995 levels. ASHRAE Standard 55 (2017). For example, a maximum of about 30 grams of water vapor can exist in a cubic meter volume of air with a temperature in the middle 80s. Even though it is an inanimate object, the existence of these components can affect the survival of living things around the coastal ecosystem. Relative humidity is normally expressed as a percentage; a higher percentage means that the airwater mixture is more humid. Abu Dhabi: Humidity levels have risen at night in the coastal areas of the UAE since Friday and are expected to remain on the higher side over the next few days. If significant, these added factors help explain why rainfall totals from thunderstorms can exceed actual PW values of the air in which the storms are occurring. [36] In general, higher temperatures will require lower humidities to achieve thermal comfort compared to lower temperatures, with all other factors held constant. 1-Stop Climate , which can be expressed as: The absolute humidity changes as air temperature or pressure changes, if the volume is not fixed. 8. Air Masses and Fronts WebThe word that describes humidity (maritime or continental) is paired with the word that describes temperature (equatorial, tropical, polar or arctic). Humans are sensitive to humid air because the human body uses evaporative cooling as the primary mechanism to regulate temperature. 2 The humidity in coastal areas is usually than that of the Weather Radio The gravimetric method, while the most accurate, is very cumbersome. It's near giant bodies of water, heat takes up water vapor at that point, and voila, you have humidity in abundance In contrast, a very low humidity level favors the build-up of static electricity, which may result in spontaneous shutdown of computers when discharges occur. [39] Extremely low (below 20%) relative humidities may also cause eye irritation. Nearness of a large body of water which adds to the moisture content of the atmosphere making it humid. Cloud condensation nuclei lower the level of supersaturation required to form fogs and clouds - in the absence of nuclei around which droplets or ice can form, a higher level of supersaturation is required for these droplets or ice crystals to form spontaneously. All humidity sensors face problems in measuring dust-laden gas, such as exhaust streams from clothes dryers. ten hottest places on earth (highest average monthly temperature) describes the temperature measured both in degrees Celsius and Fahrenheit as well the month of the year for selected countries with climate extremes. Therefore, some of the abiotic components possessed by the coastal ecosystem include sand, land, temperature, air, humidity, rocks, and also sunlight. The air is able to pick up water from the ocean, the water in the air makes it more humid. mostly tropical, but temperate in south. Decision Support Page When the humidity is slight (Figure 5a), under the influence of northeasterly airflow, the AOD in the Guangxi area is high, but the effect of the GBA is relatively small, for which the AOD is 0.61. The term relative humidity is reserved for systems of water vapor in air. By comparison, thermal comfort standard ASHRAE 55 requires systems designed to control humidity to maintain a dew point of 16.8C (62.2F) though no lower humidity limit is established.[46]. Although weather conditions affect people differently, in general in the spring and summer, surface dewpoint temperatures in the 50s usually are comfortable to most people, in the 60s are somewhat uncomfortable (humid), and in the 70s are quite uncomfortable (very humid). For a given dew point and its corresponding absolute humidity, the relative humidity will change inversely, albeit nonlinearly, with the temperature. In the winter, there is another index we use to determine how cold our bodies feel when we are outside. Brainstorm and discuss the pros of coastal living. This index combines the effect of the air temperature with the speed of the wind. If the system at State A is isothermally compressed (compressed with no change in system temperature), then the relative humidity of the system increases because the partial pressure of water in the system increases with the volume reduction. of water at the same temperature, usually expressed as a percentage:[11][12][5]. Weather Averages in Oregon Coast O NOAA's Ten Signs of a Warming World: Humidity For example, a parcel of air near saturation may contain 28 g of water per cubic metre of air at 30C (86F), but only 8 g of water per cubic metre of air at 8C (46F). National Oceanic and Atmospheric Administration A device used to measure humidity of air is called a psychrometer or hygrometer. Relative humidity increases as well, going from 33% in June, to 55% in July, and to 51% in August and September, thus making the heat sweltering. mostly temperate, but tropical in Hawaii and Florida, arctic in Alaska, semiarid in the great plains west of the Mississippi River, and arid in the Great Basin of the southwest; low winter temperatures in the northwest are ameliorated occasionally in January and February by warm chinook winds from the eastern slopes of the Rocky Mountainsnote: many consider Denali, the highest peak in the US, to be the worlds coldest mountain because of its combination of high elevation and its subarctic location at 63 degrees north latitude; permanent snow and ice cover over 75 percent of the mountain, and enormous glaciers, up to 45 miles long and 3,700 feet thick, spider out from its base in every direction; it is home to some of the worlds coldest and most violent weather, where winds of over 150 miles per hour and temperatures of -93F have been recorded. Such short circuits may cause substantial permanent damage if the equipment is powered on before the condensation has evaporated. [46] However, the recommended range of indoor relative humidity in air conditioned buildings is generally 3060%. Without other greenhouse gases, Earth's blackbody temperature, below the freezing point of water, would cause water vapor to be removed from the atmosphere. As the temperature of a parcel of air decreases it will eventually reach the saturation point without adding or losing water mass. Absolute humidity is the total mass of water vapor present in a given volume or mass of air. Houston, Miami, San Diego, Osaka, Shanghai, Shenzhen and Tokyo also have an extreme humid period in their summer months. Event Ready A major source of water vapor in Kentucky is the Gulf of Mexico. Relative humidity only considers the invisible water vapour. As a condensible greenhouse gas, it precipitates, with a much lower scale height and shorter atmospheric lifetime weeks instead of decades. In general, the higher the PW, the higher the potential for very heavy rain from thunderstorms if they were to develop. Find an answer to your question The humidity in coastal areas is usually.. than that of the inland areas. Ile Amsterdam et Ile Saint-Paul: oceanic with persistent westerly winds and high humidity; Iles Crozet: windy, cold, wet, and cloudy; Iles Kerguelen: oceanic, cold, overcast, windy; tropical; hot, rainy season (June to November); cooler, dry season (November to May), temperate, mild winters, dry and warm to hot summers, warm and pleasant; Mediterranean-like on Black Sea coast, temperate and marine; cool, cloudy, wet winters and summers; occasional warm mountain (foehn) wind, tropical; warm and comparatively dry along southeast coast; hot and humid in southwest; hot and dry in north, Mediterranean with mild winters and warm summers, temperate; mild, wet winters; hot, dry summers, arctic to subarctic; cool summers, cold winters, tropical; tempered by northeast trade winds, tropical marine; generally warm and humid, moderated by northeast trade winds; dry season (January to June), rainy season (July to December); little seasonal temperature variation, tropical; hot, humid in lowlands; cooler in highlands, temperate with mild winters and cool summers; about 50% of days are overcast, generally hot and humid; monsoonal-type rainy season (June to November) with southwesterly winds; dry season (December to May) with northeasterly harmattan winds, tropical; generally hot and humid; monsoonal-type rainy season (June to November) with southwesterly winds; dry season (December to May) with northeasterly harmattan winds, tropical; hot, humid, moderated by northeast trade winds; two rainy seasons (May to August, November to January), tropical; semiarid where mountains in east cut off trade winds, temperate; mild, rainy winters (September to May) with hot, dry summers (May to September), subtropical in lowlands, temperate in mountains, subtropical monsoon; cool and humid in winter, hot and rainy from spring through summer, warm and sunny in fall, temperate; cold, cloudy, humid winters; warm summers, temperate; moderated by North Atlantic Current; mild, windy winters; damp, cool summers, varies from tropical monsoon in south to temperate in north, northeast monsoon (December to April), southwest monsoon (June to October); tropical cyclones occur during May/June and October/November in the northern Indian Ocean and January/February in the southern Indian Ocean, tropical; hot, humid; more moderate in highlands, mostly arid or semiarid, subtropical along Caspian coast, mostly desert; mild to cool winters with dry, hot, cloudless summers; northern mountainous regions along Iranian and Turkish borders experience cold winters with occasionally heavy snows that melt in early spring, sometimes causing extensive flooding in central and southern Iraq, temperate maritime; modified by North Atlantic Current; mild winters, cool summers; consistently humid; overcast about half the time, temperate; cool summers and mild winters; overcast about a third of the time, temperate; hot and dry in southern and eastern desert areas, predominantly Mediterranean; alpine in far north; hot, dry in south, arctic maritime with frequent storms and persistent fog, varies from tropical in south to cool temperate in north, mostly arid desert; rainy season in west (November to April), continental, cold winters and hot summers, arid and semiarid, varies from tropical along coast to arid in interior, tropical; marine, hot and humid, moderated by trade winds, temperate, with rainfall concentrated in summer; long, bitter winters, temperate, with rainfall heavier in summer than winter; cold winters, influenced by continental air masses resulting in relatively cold winters with heavy snowfall and hot, dry summers and autumns; Mediterranean and alpine influences create regional variation; maximum rainfall between October and December, dry desert; intensely hot summers; short, cool winters, dry continental to polar in high Tien Shan Mountains; subtropical in southwest (Fergana Valley); temperate in northern foothill zone, tropical monsoon; rainy season (May to November); dry season (December to April), Mediterranean; mild to cool, wet winters with hot, dry summers; the Lebanon Mountains experience heavy winter snows, temperate; cool to cold, dry winters; hot, wet summers, tropical; hot, humid; dry winters with hot days and cool to cold nights; wet, cloudy summers with frequent heavy showers, Mediterranean along coast; dry, extreme desert interior, continental; cold, cloudy winters with frequent snow or rain; cool to moderately warm, cloudy, humid summers, transitional, between maritime and continental; wet, moderate winters and summers, modified continental with mild winters, cool summers, subtropical; marine with cool winters, warm summers, tropical along coast, temperate inland, arid in south, sub-tropical; rainy season (November to May); dry season (May to November), tropical; annual southwest (April to October) and northeast (October to February) monsoons, tropical; hot, humid; dry, northeast monsoon (November to March); rainy, southwest monsoon (June to August), subtropical to arid; hot and dry (February to June); rainy, humid, and mild (June to November); cool and dry (November to February), Mediterranean; mild, rainy winters; hot, dry summers, tropical; hot and humid; wet season May to November; islands border typhoon belt, tropical, modified by southeast trade winds; warm, dry winter (May to November); hot, wet, humid summer (November to May), tropical; heavy year-round rainfall, especially in the eastern islands; located on southern edge of the typhoon belt with occasionally severe damage, Mediterranean with mild, wet winters and hot, dry summers, desert; continental (large daily and seasonal temperature ranges), Mediterranean climate, hot dry summers and autumns and relatively cold winters with heavy snowfalls inland, tropical; little daily or seasonal temperature variation, Mediterranean in the north, becoming more extreme in the interior; in the south, hot, dry desert; rain is rare; cold offshore air currents produce fog and heavy dewnote: data does not include former Western Sahara, desert; hot, dry; rainfall sparse and erratic, tropical with a monsoonal pattern; rainy season (November to February), varies from cool summers and severe winters in north to subtropical summers and mild winters in south, temperate; marine; cool summers and mild winters, tropical; modified by southeast trade winds; hot, humid, tropical in lowlands, cooler in highlands, desert; mostly hot, dry, dusty; tropical in extreme south, varies; equatorial in south, tropical in center, arid in north, tropical; modified by southeast trade winds, subtropical; mild, little seasonal temperature variation, warm, dry summers and autumns; relatively cold winters with heavy snowfall, tropical marine; moderated by northeast trade winds, little seasonal temperature variation; dry season December to June, rainy season July to October, temperate along coast, modified by North Atlantic Current; colder interior with increased precipitation and colder summers; rainy year-round on west coast, dry desert; hot, humid along coast; hot, dry interior; strong southwest summer monsoon (May to September) in far south, planetary air pressure systems and resultant wind patterns exhibit remarkable uniformity in the south and east; trade winds and westerly winds are well-developed patterns, modified by seasonal fluctuations; tropical cyclones (hurricanes) may form south of Mexico from June to October and affect Mexico and Central America; continental influences cause climatic uniformity to be much less pronounced in the eastern and western regions at the same latitude in the North Pacific Ocean; the western Pacific is monsoonal - a rainy season occurs during the summer months, when moisture-laden winds blow from the ocean over the land, and a dry season during the winter months, when dry winds blow from the Asian landmass back to the ocean; tropical cyclones (typhoons) may strike southeast and east Asia from May to December, mostly hot, dry desert; temperate in northwest; arctic in north, tropical; hot and humid; wet season May to November, tropical maritime; hot, humid, cloudy; prolonged rainy season (May to January), short dry season (January to May), tropical; northwest monsoon (December to March), southeast monsoon (May to October); slight seasonal temperature variation, subtropical to temperate; substantial rainfall in the eastern portions, becoming semiarid in the far west, varies from tropical in east to dry desert in west; temperate to frigid in Andes, tropical marine; northeast monsoon (November to April); southwest monsoon (May to October), tropical; hot and humid; modified by southeast trade winds; rainy season (November to March), temperate with cold, cloudy, moderately severe winters with frequent precipitation; mild summers with frequent showers and thundershowers, maritime temperate; cool and rainy in north, warmer and drier in south, tropical marine, mild; little seasonal temperature variation, temperate; cold, cloudy winters with frequent snow and fog; sunny summers with frequent showers and thunderstorms, ranges from steppes in the south through humid continental in much of European Russia; subarctic in Siberia to tundra climate in the polar north; winters vary from cool along Black Sea coast to frigid in Siberia; summers vary from warm in the steppes to cool along Arctic coast, temperate; two rainy seasons (February to April, November to January); mild in mountains with frost and snow possible, tropical, with practically no variation in temperature; has two seasons (dry and humid).
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