the humidity in coastal areas is usually

Visibility: 8 mi. Humans are sensitive to humid air because the human body uses evaporative cooling as the primary mechanism to regulate temperature. WebUpslope winds more than 10 to 12 knots usually result in stratus rather than fog. Naturally aspirated internal combustion engines have a further danger of ice forming inside the carburetor. Nashville Advisory/Warning Criteria, Radar The humidity of an air and water vapor mixture is determined through the use of psychrometric charts if both the dry bulb temperature (T) and the wet bulb temperature (Tw) of the mixture are known. Winds blow inward toward these areas. Ice crystal processes (including deposition and aggregation) also are important for particle growth. "Were in quite of a drought. In the summer the hot dry air is absorbed by this ocean and the temperature rarely climbs above 35C (95F). p It's near giant bodies of water, heat takes up water vapor at that point, and voila, you have humidity in abundance The annual rainfall is 1000 to over 1500 mm (39 to 59 inches). , divided by the volume of the air and water vapor mixture It forms at low latitudes, generally within 25 degrees of the equator. metropolitan France: generally cool winters and mild summers, but mild winters and hot summers along the Mediterranean; occasional strong, cold, dry, north-to-northwesterly wind known as the mistral; French Guiana: tropical; hot, humid; little seasonal temperature variation; Guadeloupe and Martinique: subtropical tempered by trade winds; moderately high humidity; rainy season (June to October); vulnerable to devastating cyclones (hurricanes) every eight years on average; Mayotte: tropical; marine; hot, humid, rainy season during northeastern monsoon (November to May); dry season is cooler (May to November); Reunion: tropical, but temperature moderates with elevation; cool and dry (May to November), hot and rainy (November to April). Decision Support Page Although humidity is an important factor for thermal comfort, humans are more sensitive to variations in temperature than they are to changes in relative humidity. Bouvet Island. A humidistat is a humidity-triggered switch, often used to control a dehumidifier. 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. This explains the low levels (in the absence of measures to add moisture) of humidity in heated structures during winter, resulting in dry skin, itchy eyes, and persistence of static electric charges. To me, there is a huge difference between a hot and humid day, and a hot and dry day. I strongly prefer hot and dry. So much so that during my care Rivers and swamps are plentiful and dominate the landscape. For example, according to the heat index, a relative humidity of 75% at air temperature of 80.0F (26.7C) would feel like 83.6F 1.3F (28.7C 0.7C).[13][14]. National Weather Service WebIn geography, the temperate climates of Earth occur in the middle latitudes (23.5 to 66.5 N/S of Equator), which span between the tropics and the polar regions of Earth. Coast This dependence is demonstrated by considering the airwater system shown below. e Finally, there can be a significant change in wind direction and/or speed. A study concluded, "Maintaining indoor relative humidity >40% will significantly reduce the infectivity of aerosolized virus. The most humid cities on Earth are generally located closer to the equator, near coastal regions. When an electronic item is moved from a cold place (e.g., garage, car, shed, air conditioned space in the tropics) to a warm humid place (house, outside tropics), condensation may coat circuit boards and other insulators, leading to short circuit inside the equipment. Warming some air containing a fog may cause that fog to evaporate, as the air between the water droplets becomes more able to hold water vapour. If the air is totally saturated at a particular level (e.g., the surface), then the dewpoint temperature is the same as the actual air temperature, and the relative humidity is 100 percent. Hot and sticky can happen anywhere the temperatures are high and so is the humidity. When there is enough moisture in the air the air can't except Baker, Howland, and Jarvis Islands: equatorial; scant rainfall, constant wind, burning sun; Johnston Atoll and Kingman Reef: tropical, but generally dry; consistent northeast trade winds with little seasonal temperature variation; Midway Islands: subtropical with cool, moist winters (December to February) and warm, dry summers (May to October); moderated by prevailing easterly winds; most of the 107 cm of annual rainfall occurs during the winter; Palmyra Atoll: equatorial, hot; located within the low pressure area of the Intertropical Convergence Zone (ITCZ) where the northeast and southeast trade winds meet, it is extremely wet with between 400-500 cm of rainfall each year, warm temperate; freezing temperatures almost unknown, mostly mid-latitude desert, long, hot summers, mild winters; semiarid grassland in east, tropical; moderated by southeast trade winds from May to October; moderate rainfall from November to April; may be affected by cyclones from December to April, tropical in south; monsoonal in north with hot, rainy season (May to September) and warm, dry season (October to March), subtropical, tempered by easterly trade winds, relatively low humidity, little seasonal temperature variation; rainy season September to November, tropical; hot, rainy season (November to April); cool, dry season (May to October); rains 250-300 cm per year (80% humidity); average temperature 26.6 degrees Celsius, temperate; temperature and precipitation vary with altitude, warm to hot summers, cool to mild winters, a wide equatorial band of hot and humid tropical climates, bordered north and south by subtropical temperate zones that separate two large areas of cold and dry polar climatesten driest places on earth (average annual precipitation): McMurdo Dry Valleys, Antarctica 0 mm (0 in)Arica, Chile 0.76 mm (0.03 in)Al Kufrah, Libya 0.86 mm (0.03 in)Aswan, Egypt 0.86 mm (0.03 in)Luxor, Egypt 0.86 mm (0.03 in)Ica, Peru 2.29 mm (0.09 in)Wadi Halfa, Sudan 2.45 mm (0.1 in)Iquique, Chile 5.08 mm (0.2 in)Pelican Point, Namibia 8.13 mm (0.32 in)El Arab (Aoulef), Algeria 12.19 mm (0.48 in)ten wettest places on earth (average annual precipitation): Mawsynram, India 11,871 mm (467.4 in)Cherrapunji, India 11,777 mm (463.7 in)Tutunendo, Colombia 11,770 mm (463.4 in)Cropp River, New Zealand 11,516 mm (453.4 in)San Antonia de Ureca, Equatorial Guinea 10,450 mm (411.4 in)Debundsha, Cameroon 10,299 mm (405.5 in)Big Bog, US (Hawaii) 10,272 mm (404.4 in)Mt Waialeale, US (Hawaii) 9,763 mm (384.4 in)Kukui, US (Hawaii) 9,293 mm (365.9 in)Emeishan, China 8,169 mm (321.6 in)ten coldest places on earth (lowest average monthly temperature): Verkhoyansk, Russia (Siberia) -47C (-53F) JanuaryOymyakon, Russia (Siberia) -46C (-52F) JanuaryEureka, Canada -38.4C (-37.1F) FebruaryIsachsen, Canada -36C (-32.8F) FebruaryAlert, Canada -34C (-28F) FebruaryKap Morris Jesup, Greenland -34C (-29F) MarchCornwallis Island, Canada -33.5C (-28.3F) FebruaryCambridge Bay, Canada -33.5C (28.3F) FebruaryIlirnej, Russia -33C (-28F) JanuaryResolute, Canada -33C (-27.4F) Februaryten hottest places on earth (highest average monthly temperature): Death Valley, US (California) 39C (101F) JulyIranshahr, Iran 38.3C (100.9F) June Ouallene, Algeria 38C (100.4F) JulyKuwait City, Kuwait 37.7C (100F) JulyMedina, Saudi Arabia 36C (97F) JulyBuckeye, US (Arizona) 34C (93F) JulyJazan, Saudi Arabia 33C (91F) JuneAl Kufrah, Libya 31C (87F) JulyAlice Springs, Australia 29C (84F) JanuaryTamanrasset, Algeria 29C (84F) June, mostly desert; hot and humid along west coast; temperate in western mountains affected by seasonal monsoon; extraordinarily hot, dry, harsh desert in east, tropical; modified by altitude; rainy season (October to April), tropical; moderated by altitude; rainy season (November to March), Saint Helena, Ascension, and Tristan da Cunha, United States Pacific Island Wildlife Refuges, Center for the Study of Intelligence (CSI). Items of Interest ABSOLUTE HUMIDITY: Absolute humidity (expressed as grams of water vapor per cubic meter volume of air) is a measure of the actual amount of water vapor The low humidity is a consequence of drawing in the very cold air with a low absolute humidity, which is found at airliner cruising altitudes. Humidity depends on the temperature and pressure of the system of interest. The same amount of water vapor results in higher humidity in cool air t At the top end of the range, moisture may increase the conductivity of permeable insulators leading to malfunction. Data Discuss. Atlantic Ocean - Climate So when water molecules (vapor) are introduced into that volume of dry air, the number of air molecules in the volume must decrease by the same number, if the temperature and pressure remain constant. A device used to measure humidity is called a hygrometer; one used to regulate it is called a humidistat, or sometimes hygrostat. Learn More What are weather observations? Humidity is also measured on a global scale using remotely placed satellites. 1-Stop Severe Forecast While dewpoint gives one a quick idea of moisture content in the air, relative humidity does not since the humidity is relative to the air temperature. {\displaystyle e_{w}^{*}} This entry includes a brief description of typical weather regimes throughout the year; in the World entry only, it includes four subfields that describe climate extremes:ten driest places on earth (average annual precipitation) describes the annual average precipitation measured in both millimeters and inches for selected countries with climate extremes. Nearness of a large body of water which adds to the moisture content of the atmosphere making it humid. Chapter 10: Progress Questions Flashcards | Quizlet Liquid water evaporates from oceans, lakes, rivers, plants, the ground, and fallen rain. Absolute humidity in the atmosphere ranges from near zero to roughly 30g (1.1oz) per cubic metre when the air is saturated at 30C (86F).[8][9]. 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. [38], Very low humidity can create discomfort, respiratory problems, and aggravate allergies in some individuals. Therefore, when applying more pressure to a gas saturated with water, all components will initially decrease in volume approximately according to the ideal gas law. [31] Humidity has a small effect on thermal comfort outdoors when air temperatures are low, a slightly more pronounced effect at moderate air temperatures, and a much stronger influence at higher air temperatures.[32]. (c) Himalayan. answer choices Ocean surfaces change temperature more slowly than land surfaces. Relative humidity is an important metric used in weather forecasts and reports, as it is an indicator of the likelihood of precipitation, dew, or fog. Remote Sensing | Free Full-Text | Aerosol Physical–Optical Therefore, the enhancement factor is normally slightly greater than unity for real systems. Why is the weather different in high and 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. Also, if the atmosphere is as warm or warmer than the skin during times of high humidity, blood brought to the body surface cannot dissipate heat by conduction to the air. At 100% relative humidity, the air is saturated and is at its dew point. However, in real systems the interaction effects between gas molecules result in a small increase of the equilibrium vapor pressure of water in air relative to equilibrium vapor pressure of pure water vapor. Humidity depends on water vaporization and condensation, which, in turn, mainly depends on temperature. Moisture The field concerned with the study of physical and thermodynamic properties of gasvapor mixtures is named psychrometrics. It varies with the temperature of the air: colder air can hold less vapour. The relative humidity As the sun heats the land, the air rises and thus reduces the local air pressure. This causes surrounding higher air pressure air masses to flow in to the saturated vapor pressure of pure water: The enhancement factor is equal to unity for ideal gas systems. Torrential rains from the storm can cause rivers to flood their banks and mudslides to form. In the winter, there is another index we use to determine how cold our bodies feel when we are outside. WebSimilar to rainfall, the relative humidity in Nigeria decreases from the south to the north, with an annual mean of 88% around Lagos. The sampling of air containing salt fogs is divided into two modes: long-term and short-term. Past Derby/Oaks/Thunder Weather Humidity plays an important role for surface life. WebThe air near the center of this low-pressure system usually will. Normally our weather, notably rain, comes from the oceans. The sun heats ocean waters causing warm water to rise. As this warm water rises it pushe A coast means there is a large body of water nearby such as a large lake, an inland sea, or an ocean. Water evaporates into the air. Water in air i Absolute humidity is the total mass of water vapor present in a given volume or mass of air. t This cooling means the density increases again forming a small area of high pressure (4). It isnt always, it depends on if the moist air is blowing in from the ocean or dry air is blowing out from the land. Also, in winter if the water Question 2. Similarly, during summer in humid climates a great deal of liquid water condenses from air cooled in air conditioners. For animal life dependent on perspiration (sweating) to regulate internal body temperature, high humidity impairs heat exchange efficiency by reducing the rate of moisture evaporation from skin surfaces. ) Tornado Machine Plans, Weather Safety {\displaystyle (p)} 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. The CBE Thermal Comfort Tool can be used to demonstrate the effect of relative humidity for specific thermal comfort conditions and it can be used to demonstrate compliance with ASHRAE Standard 55-2017. For any gas, at a given temperature and pressure, the number of molecules present in a particular volume is constant. Too low humidity may make materials brittle. or This effect is calculated as the heat index or humidex. Climate Quiz As such, Due to the increasing potential for a higher water vapor partial pressure at higher air temperatures, the water content of air at sea level can get as high as 3% by mass at 30C (86F) compared to no more than about 0.5% by mass at 0C (32F). 1-Stop Drought Common construction methods often produce building enclosures with a poor thermal boundary, requiring an insulation and air barrier system designed to retain indoor environmental conditions while resisting external environmental conditions. Spotter Training Therefore, some of the abiotic components possessed by the coastal ecosystem include sand, land, temperature, air, humidity, rocks, and also sunlight. have more fog. National Oceanic and Atmospheric Administration 1-Stop Climate Station History February Climate & Weather Averages in Oregon Coast. Specific humidity is the ratio of water vapor mass to total moist air parcel mass. Humidity affects the energy budget and thereby influences temperatures in two major ways. All humidity sensors face problems in measuring dust-laden gas, such as exhaust streams from clothes dryers. The term relative humidity is reserved for systems of water vapor in air. Conversely, decreasing temperature would also make some water condense, again making the final volume deviate from predicted by the ideal gas law. Long-term average salt-fog concentrations are determined through the placement of an absorption device directly in the environment of interest, where ambient air is pumped at a constant flow rate of 0.8 L/min (Fig. Heating cold outdoor air can decrease relative humidity levels indoors to below 30%. Fire Weather Houses dry out when cold winter air enters the house through infiltration and is warmed up by the heating system. Droplets grow through a process called "collision-coalescence" whereby droplets of varying sizes collide and fuse together (coalesce). ) Down to a certain temperature, winters can be humid, yes. When it gets colder than that, the moisture in the air freezes and settles, giving you a Theres a good reason why city dwellers flee to the countryside to cool off in the heat of summer: Rural areas are usually not as hot. Warm air can possess more water vapor (moisture) than cold air, so with the same amount of absolute/specific humidity, air will have a HIGHER relative humidity if the air is cooler, and a LOWER relative humidity if the air is warmer. {\displaystyle (p_{s})} Questions for Class 9 Geography Chapter 5 Natural Vegetation is the equilibrium vapor pressure expressed in millibars. Webcoastal areas, where the outside relative humidity may be quite high year round, outside ventilation air may produce little drying effect. Under moderate humidity (Figure 5d), the value of AOD in the south of China is generally low. Remote Sensing | Free Full-Text | Aerosol Physical–Optical High temperatures combine with the high dew point to create heat index in excess of 65C (149F). "[49], Mucociliary clearance in the respiratory tract is also hindered by low humidity. What we "feel" outside is the actual amount of moisture (absolute humidity) in the air. is the absolute pressure expressed in millibars, and As temperature decreases, the amount of water vapor needed to reach saturation also decreases. There are various devices used to measure and regulate humidity. Lack of humidity can be a problem in houses with very high air-exchange rates. the glasses become foggy). Do These Moisture Meter Readings Mean It raises the surface temperature substantially above its theoretical radiative equilibrium temperature with the sun, and water vapor is the cause of more of this warming than any other greenhouse gas. About 78% of the molecules in dry air are nitrogen (N2). Likewise, warming air decreases the relative humidity. Earth Syst. Mean annual temperature for Nigeria is 26.9C , with average monthly temperatures ranging between 24C (December, January) and Buck has reported that, at sea level, the vapor pressure of water in saturated moist air amounts to an increase of approximately 0.5% over the equilibrium vapor pressure of pure water.[19]. P f In situations where time is critical, increasing air flow through the device's internals, such as removing the side panel from a PC case and directing a fan to blow into the case, will reduce significantly the time needed to acclimatise to the new environment. On this Wikipedia the language links are at the top of the page across from the article title. Darwin experiences an extremely humid wet season from December to April. If the system at State A is isobarically heated (heating with no change in system pressure), then the relative humidity of the system decreases because the equilibrium vapor pressure of water increases with increasing temperature. [39] Extremely low (below 20%) relative humidities may also cause eye irritation. ( The average summer temperature ranges from 13-24 C; winter temperatures are 5 C or below. Botswana. Even with saturation (100% relative humidity) outdoors, heating of infiltrated outside air that comes indoors raises its moisture capacity, which lowers relative humidity and increases evaporation rates from moist surfaces indoors (including human bodies and household plants.). This makes it unsuitable for chemical engineering calculations, e.g. Humans can be comfortable within a wide range of humidities depending on the temperaturefrom 30 to 70%[33]but ideally not above the Absolute (60F Dew Point),[34] between 40%[35] and 60%. Alertness and mental capacity also may be affected, resulting in heat stroke or hyperthermia. {\displaystyle (e'_{w})} CoCoRaHS Climate The detection rate of V. parahaemolyticus was significantly higher in the eastern coastal areas and northwest compared with the southwest. 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). WRCC: Washington Climate - DRI The air at the beach has a higher humidity because of the proximity to the sea. Satellite water vapor imagery plays an important role in monitoring climate conditions (like the formation of thunderstorms) and in the development of weather forecasts. is the dry-bulb temperature expressed in degrees Celsius (C), Hazardous Weather Outlook 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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