Most of Croatia has a moderately warm and rainy continental climate as defined by the Köppen climate classification. Mean monthly temperature ranges between in January and in July. The coldest parts of the country are Lika and Gorski Kotar where snowy forested climate is found at elevations above . The warmest areas of Croatia are at the Adriatic coast and especially in its immediate hinterland characterised by the Mediterranean climate, as the temperature highs are moderated by the sea. Consequently, temperature peaks are more pronounced in the continental areas. The lowest temperature of was recorded on 3 February 1919 in Čakovec, and the highest temperature of was recorded on 4 August 1981 in Ploče.
Climate
Croatia
Croatia | Climate
Moderately warm and rainy continental climate humid subtropical and Mediterranean climate A moderately warm and rainy continental climate. Moderately warm and rainy continental climate
which cities in croatia are famous for their protective walls and forts
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Dubrovnik
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in which country is this state located in ?
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Sorry. I cannot find the answer based on the context.
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which country is this city located in ?
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Croatia
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how is the weather in this country ?
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Most of Croatia has a moderately warm and rainy continental climate as defined by the Köppen climate classification. Mean monthly temperature ranges between in January and in July. The coldest parts of the country are Lika and Gorski Kotar where snowy forested climate is found at elevations above . The warmest areas of Croatia are at the Adriatic coast and especially in its immediate hinterland characterised by the Mediterranean climate, as the temperature highs are moderated by the sea. Consequently, temperature peaks are more pronounced in the continental areas. The lowest temperature of was recorded on 3 February 1919 in Čakovec, and the highest temperature of was recorded on 4 August 1981 in Ploče.
Croatia | Climate
Most of Croatia has a moderately warm and rainy oceanic climate (Cfb) as defined by the Köppen climate classification. Mean monthly temperatures range between (in January) and (in July). The coldest parts of the country are Lika and Gorski Kotar where a snowy forested climate is found at elevations above . The warmest areas of Croatia are at the Adriatic coast and especially in its immediate hinterland, which are characterised by a Mediterranean climate since temperatures are moderated by the sea. Consequently, temperature peaks are more pronounced in the continental areas: the lowest temperature of was recorded on 4 February 1929 in Gospić, and the highest temperature of was recorded on 5 August 1981 in Ploče.
Geography of Croatia | Climate
Croatia proper has a moderately warm and rainy continental climate (Dfb) as defined by the Köppen climate classification. Mean monthly temperatures range between (in January) and (in July). Temperature peaks are pronounced in the region compared to parts of Croatia closer to the Adriatic Sea, because of the absence of its moderating effect. The lowest temperature of was recorded on 3 February 1919 in Čakovec, and the highest temperature of was recorded on 5 July 1950 in Karlovac. Gorski Kotar and Lika represent the coldest parts of Croatia as mean annual temperature there ranges between at lower elevations and at greater elevations.
Croatia proper | Hydrology and climate
The sunniest parts of the country are the outer islands, Hvar and Korčula, where more than 2700 hours of sunshine are recorded per year, followed by the middle and southern Adriatic Sea area in general, and northern Adriatic coast, all with more than 2000 hours of sunshine per year.
Croatia | Climate
The sunniest parts of the country are the outer islands, Hvar and Korčula, where more than 2,700 hours of sunshine are recorded per year, followed by the southern Adriatic Sea area in general, northern Adriatic coast, and Slavonia, all with more than 2,000 hours of sunshine per year.
Geography of Croatia | Climate
Croatia is a Mediterranean country, lying to the east of Italy, across the Adriatic Sea. Towards the north lie the Alps, and to the north-east the country forms the western end of the great Pannonian Plain. The interior of Croatia has a continental climate, with cold winters, and hot summers with enough rain to make it a major agricultural area. Winegrowing is concentrated in the hilly areas bordering on the Pannonian Plain. The Dalmatian Coast is typically Mediterranean in climate, though the Dinaric Alps mountain range creates pockets of alpine climate at higher altitudes. The coastline of the Adriatic Sea is ideal for grape cultivation with its hot, humid summers and mild winters.
Croatian wine | Geography and climate
Situated on the western coast of Istria and cooled by sea breezes, the local climate is relatively mild and free of oppressive summer heat. The month of July is the hottest, with a maximum air temperature of 30°C in conditions of low humidity, while January is the coldest with an average of . There are more than 2,400 hours of sun a year, an average of more than 10 hours of sunshine during the summer days. Sea temperatures can reach , higher than one might expect compared to the coast of southern Croatia where the air temperatures are higher. The average annual rainfall of is more or less equally distributed throughout the year, although July and August are very dry.
Poreč | Climate
Mean annual precipitation ranges between and depending on geographic region and prevailing climate type. The least precipitation is recorded in the outer islands (Biševo, Lastovo, Svetac, Vis) and in the eastern parts of Slavonia. However, in the latter case, it occurs mostly during the growing season. The maximum precipitation levels are observed on the Dinara mountain range and in Gorski kotar. Prevailing winds in the interior are light to moderate northeast or southwest, and in the coastal area, prevailing winds are determined by local area features. Higher wind velocities are more often recorded in cooler months along the coast, generally as the cool northeasterly bura or less frequently as the warm southerly jugo.
Croatia | Climate
The islands of Lošinj, Cres, Krk, and Rab receive the most sunshine during the year—with 217 clear days per year on average. Seawater temperatures reach up to in summer, while dipping to in spring and autumn and as low as in winter. The predominant winter winds are the bora and jugo. The bora is significantly conditioned by wind gaps in the Dinaric Alps bringing cold and dry continental air—the point where it reaches its peak speed is at Senj, with gusts of up to . The jugo brings humid and warm air, often carrying Saharan sand that causes rain dust.
Croatian Littoral | Hydrology and climate
There are 2620 sunshine hours annually (1961–1990 average). Annual precipitation level of is the lowest of all Croatia. Maritime winds temper air temperatures compared with the mainland, with average summer daily highs of ; on the other extreme, winter average daily lows are .
Palagruža | Climate
Areas of the Croatian Littoral further away from the coast enjoy a moderately warm and rainy oceanic climate (Cfb), similar to the continental climate of most inland regions of Croatia. The mean monthly temperature varies throughout the region. On the mainland coast it ranges between (in January) and (in July). On the Kvarner Gulf islands the mean monthly temperature is somewhat higher; it ranges from (in January) to (in July), while at higher elevations, in the mountains found along the northern and eastern peripheral areas of the region, temperatures range between (in January) and (in July). The lowest air temperature recorded in the region, , was measured in Senj, on 10 February 1956.
Croatian Littoral | Hydrology and climate
The mean annual precipitation is depending on the geographic region and prevailing climate type. The least precipitation is recorded in the outer islands (Vis, Lastovo, Biševo, and Svetac) and in the eastern parts of Slavonia; however, in the latter case it is mostly during the growing season. The most precipitation is observed on the Dinara mountain range and in Gorski Kotar, where some of the highest annual precipitation totals in Europe occur. The prevailing winds in the interior are light to moderate northeast or southwest; in the coastal area, the prevailing winds are determined by local area features. Higher wind velocities are more often recorded in cooler months along the coast, generally as cool northeasterly buras or, less frequently, as warm southerly jugos.
Geography of Croatia | Climate
In Spring and Autumn maximum temperatures are typically between and . Winters are among the mildest of any Croatian city, with daytime temperatures around in the coldest months. Snow in Dubrovnik is very rare.
Dubrovnik | Climate
The karst field or polje is a common feature of the landscape. On the Adriatic and Aegean coasts the climate is Mediterranean, on the Black Sea coast the climate is humid subtropical and oceanic, and inland it is humid continental. In the northern part of the peninsula and on the mountains, winters are frosty and snowy, while summers are hot and dry. In the southern part winters are milder. The humid continental climate is predominant in Bosnia and Herzegovina, northern Croatia, Bulgaria, Kosovo, northern Montenegro, the Republic of North Macedonia, the interior of Albania and Serbia, while the other, less common climates, the humid subtropical and oceanic climates, are seen on the Black Sea coast of Bulgaria and Balkan Turkey (European Turkey); and the Mediterranean climate is seen on the coast of Albania, the coast of Croatia, Greece, southern Montenegro and the Aegean coast of Balkan Turkey (European Turkey).
Balkans | Nature and natural resources
The climate is continental. Summers are quite hot. Daily temperatures during the summer months usually range between 20 °C and 30 °C, but can reach as high as 40 °C in July and August, when they can also stay above 30 °C for several days. Thunderstorms and rapid weather changes are common throughout the summer months, as well as in late spring, with a particularly stormy period being between mid-June and mid-July, when they often occur on a daily basis. Springs and autumns are usually calm, although rapid weather changes can also be common during the two seasons. Winters can be very severe, with early-morning temperatures sometimes reaching as low as -20 °C.
Međimurje County | Climate
Most of Croatia has a moderately warm and rainy continental climate as defined by the Köppen climate classification. The mean monthly temperature ranges between and . Croatia has a number of ecoregions because of its climate and geomorphology, and the country is consequently among the most biodiverse in Europe. There are four types of biogeographical regions in Croatia: Mediterranean along the coast and in its immediate hinterland; Alpine in the elevated Lika and Gorski Kotar; Pannonian along the Drava and Danube; and Continental in the remaining areas. There are 444 protected natural areas in Croatia, encompassing 8.5% of the country; there are about 37,000 known species in Croatia, and the total number of species is estimated to be between 50,000 and 100,000.
Geography of Croatia | Introduction
Although Risnjak is of only a modest altitude, it is nevertheless a very significant climatic and vegetational barrier between coastal and continental parts of Croatia. Adriatic and continental weather patterns collide here and play a significant role in determining the park's climate. It has pleasantly warm summers and an average temperature of up to 22 °C; springs and autumns are rainy, and the winter is long and snowy. The average year-round temperature at the Risnjak mountain lodge is 2.5 °C with an annual rainfall of 3600 mm, which is amongst the highest in the country, and an average snow depth of between 122 and 448 cm.
Risnjak National Park | Climate
The climate of Zagreb is classified as an oceanic climate (Köppen climate classification "Cfb"), but with significant continental influences and very closely bordering on a humid continental climate ("Dfb") as well as a humid subtropical climate (Cfa). Zagreb has four separate seasons. Summers are generally warm, sometimes hot. In late May it gets significantly warmer, temperatures start rising and it is often very warm or even hot with frequent afternoon and evening thunderstorms. Heatwaves can occur but are short-lived. Temperatures rise above on an average 14.6 days each summer. Rainfall is abundant in the summertime and it continues to be in autumn as well.
Zagreb | Climate
Iž belongs to the area which has a borderline humid subtropical and mediterranean climate. Summers are dry, warm or hot and winters are mild and rainy. Average annual air temperature on the island is 15 degrees Celsius (59 degrees Fahrenheit). The island is relatively low and spatially small so that significant day and night winds can form there. It is relatively far from the mainland, surrounded on all sides by the sea and protected by neighboring higher islands. The most common winds are bora (Croatian: "bura") during winter, sirocco (Croatian: "jugo") during spring, autumn and winter and "maestral" - a constant humid breeze of moderate intensity - during summer.
Iž | Climate
In March and October, it is also common for the temperature to drop below 0 °C over night, even when the daily temperature is in the range between 10 °C and 15 °C.
Međimurje County | Climate
Split has a borderline humid subtropical ("Cfa") and Mediterranean climate ("Csa") in the Köppen climate classification, since only one summer month has less than of rainfall, preventing it from being classified as solely humid subtropical or Mediterranean. It has hot, moderately dry summers and mild, wet winters, which can occasionally feel cold, because of the strong northern wind bura. Average annual rainfall is more than . January is the coldest month, with an average low temperature around . November is the wettest month, with a precipitation total of nearly and 12 rainy days. July is the driest month, with a precipitation total of around .
Split, Croatia | Climate
The climate of the region is temperate continental, with mild and warm summers, refreshed by the wind coming down the Balkan Mountain, and snowy winters. The average January temperature is (with an absolute minimum of ). The average July temperature is (with an absolute maximum of ). Average total annual rainfall is , being highest in the summer , and lowest in the winter .
Karlovo | Climate
Gorski Kotar mountain peaks of Risnjak and Snježnik receive the greatest precipitation in Croatia— per year. Overall, the region has no arid periods of the year. Gorski Kotar also receives the least sunlight—1,700 hours per year on average.
Croatia proper | Hydrology and climate
After the collapse of Yugoslavia, local government system in Croatia was significantly changed and today Croatian Podunavlje in widest sense can be described as a region that is overlapping with the territory of Vukovar-Syrmia and Osijek-Baranja counties. In this sense region include the gravitation regions of towns of Našice and Županja and is significantly bigger and cover the area of 6.597 kilometres or 11,7% of territory of Croatia with 348 settlements and 598.434 inhabitants in 1991 (12,5% of total population of Croatia at that time). Climate in the region can be described as Continental climate with warm and hot summers and cold winters.
Podunavlje | Geography and demographics
Dinara is located only a few dozen kilometers away from the Adriatic Sea, and is part of the Dalmatian Hinterland, but the climate on Dinara is a much colder, mountain climate, making it one of the coldest places in Croatia with average temperatures between 2 and 4 °C at the peaks. The average precipitation is high, while the number of sunny hours per year ranges between 1,700 and 1,900. There are no inhabited areas on the mountain itself and human presence consists mostly of small shacks that belong to the herdsmen from the nearby valleys such as that of the Cetina river.
Dinara | Climate
The island of Krapanj is situated in the central part of the Croatian littoral and is characterised by a warm, dry Mediterranean climate. According to data from the nearest weather station, in Šibenik, for the period from 1986 to 1996 the average annual temperature was and the average annual precipitation .
Krapanj | Climate
During the winter months, daily temperatures usually range between -10 °C and 10 °C. January is usually the coldest month, during which daily temperatures can stay below 0 °C for several days. Snowfall usually occurs between late October and early March. Fog can be a common early-morning occurrence between late summer and early spring, with all-day fog sometimes occurring during the coldest months. Warm weather, with daily temperatures around 15 °C, can occur as early as mid-February and as late as mid-November. In early October and late March, daily temperatures can also reach as high as 20 °C. However, February and November are generally cold months, with occasional heavy snow and daily temperatures around 0 °C, while March and October are generally cool, with occasional light snow and daily temperatures ranging between 0 °C and 15 °C.
Međimurje County | Climate
Lika and Gorski Kotar are part of the Dinaric Alps, and contain five out of eight mountains in Croatia higher than . Karst topography predominates in that area, resulting in specific landforms and hydrology because of the interaction of the karst and the region's watercourses—this is exemplified by the Plitvice Lakes. Most of the region has a moderately warm and rainy continental climate, although there is considerable seasonal snow at greater elevations. The region belongs almost exclusively to the Black Sea drainage basin and includes most of the large rivers flowing in Croatia. The boundaries of Croatia proper were shaped by territorial losses of medieval Croatia to the Republic of Venice and the Ottoman conquest starting in the 15th century.
Croatia proper | Introduction
During summer and winter, temperature inversion is sometimes present. An anticyclone forms above the cold continent during winter. When its center is close to Croatia, the weather is cold and gloomy in Zagreb and warmer at Sljeme. The mean annual air temperature on Medvednica is , compared with in Zagreb. The mean temperature in summer months is on average lower by than in Zagreb. On average, 15 days have temperatures below , eight days a year have average daily maxima higher than , and only one day reaches above . The coldest month is January with a mean monthly air temperature of , while the warmest month is July with an average temperature of .
Medvednica | Temperature
The vast majority of the region is encompassed by the Black Sea drainage basin. The area includes all the largest rivers flowing in the country—Sava, Drava, Mura, and Kupa—except the Danube. The largest lakes in Croatia proper are Lake Dubrava and Lake Varaždin reservoirs, both near Varaždin, through which the Drava River flows. Croatia proper has a wealth of wetlands. Two out of the four Croatian wetlands included in the Ramsar list of internationally important wetlands are located in the region—Lonjsko Polje along the Sava and Lonja rivers near Sisak, and Crna Mlaka near Jastrebarsko. A high degree of karstification of the terrain in the Dinaric Alps has resulted in an increased permeability of soil and rocks and the formation of travertine barriers and waterfalls.
Croatia proper | Hydrology and climate
Winter is the wettest season; however, it can rain in Split at any time of the year. Snow is usually rare; since record-keeping began the months of December and January have accrued 1 snowy day on average, while February has averaged 2. In February 2012, Split received unusually large amount of snow which caused major problems with traffic. Split receives more than 2,600 sunshine hours annually. July is the hottest month, with an average high temperature around . In July 2017 Croatian firefighters battled to control a forest fire along the Adriatic coast that damaged and destroyed buildings in villages around the city of Split.
Split, Croatia | Climate
With 840 mm of precipitation per year, Zagreb is Europe's 9th wettest capital, receiving less precipitation than Luxembourg but more than Brussels, Paris and London. Autumn in its early stage often brings pleasant and sunny weather with occasional episodes of rain later in the season. Late autumn is characterised by an increase in rainy days as well as by steadily falling temperature averages. Morning fog is common from mid-October to January, with northern city districts at the foothills of the Medvednica mountain as well as the districts along the Sava river being more prone to all-day fog accumulation. Winters are relatively cold with a precipitation decrease pattern.
Zagreb | Climate
With around 2600 hours of sunshine a year, the island of Lošinj is a tourist destination for Slovenians, Italians, and Germans in the summer months. Average air humidity is 70%, and the average summer temperature is and during the winter. The interior regions Gorski kotar, Velebit and Lika have mountain peaks, forests and fields, many animal species including bears, and the national parks of Risnjak and Plitvice Lakes. The Plitvice Lakes National Park lies in the Plitvice plateau which is surrounded by three mountains part of the Dinaric Alps: Plješevica mountain (Gornja Plješevica peak 1,640 m), Mala Kapela mountain (Seliški Vrh peak at 1,280 m), and Medveđak (884 m).
Tourism in Croatia | Kvarner and Highlands
The climate is tundra (Köppen: "ET"), without the presence of trees and ice for most of the year.
Sanirajak | Climate
Rovinj is one of nine settlements officially designated as towns in Istria County in western Croatia. It has a humid subtropical climate (Köppen: "Cfa"), with an average temperature of in January and in July. The average annual temperature is . The sea temperature is more than from the mid-June to September. The average annual sea temperature is . From May to September Rovinj receives more than 10 sunshine hours a day. The rainfall averages a year and average air humidity is 72 percent. Originally the peninsula on which the city lies was an island, separated from the mainland by a channel.
Rovinj | Climate
Hvar town enjoys a sunny Mediterranean climate, typical of the southern Adriatic, with mild wet winters and hot dry summers. During June to September, the average temperature is higher than , dropping below in just two months of the year (January and February). Winter days see highs between and lows from . Daytime high temperatures in the summer months range from and from for the overnight lows. During the summer, the westerly mistral wind blows through the Pakleni channel, providing welcome cooling during the day. Rain is rare here during spring and summer, though plentiful in autumn and winter months.
Hvar (city) | Climate
Karancsalja, typically for its Central European location, has a humid continental climate.
Karancsalja | Climate
Komiža experiences warm and temperate winters with warm to hot summers with the landward breeze making it the most moderate climate in the Republic of Croatia. The climate allows for Tropical and Mediterranean vegetation, including palms, carobs, olives, grapes and lemons. The average rainfall is about per square meter. The island of Vis has a number of natural sources of drinking water from the natural spring water reservoirs. The island is also home to twelve distinct types of island vegetation. Vis has been marked as one of the ten most environmentally preserved islands in the Mediterranean by the World Organization for Environmental Protection.
Komiža | Climate
Crkvice is within the Mediterranean subtropical belt. While summers are hot and sunny, autumn, winter and spring are rainy seasons. A peculiarity of the littoral Dinarids is the precipitation regime as the settlements of Orjen receive more precipitation than any others in Europe. Like the monsoon rain it is seasonally distributed, thus November thunderstorms sometimes pour 2000 liters of water in several days, while August is frequently completely dry, leading to forest fires. With a maximum discharge of 350 m³/s water one of the biggest karst springs, the Sopot spring near Risan, is a remarkable indicator of this seasonality. Most of the time it is inactive but after heavy rain a remarkable waterfall appears 20 m above the Bay of Kotor.
Crkvice | Climate
Vis experiences warm and temperate winters with warm to hot summers. The landward breeze makes it the most moderate climate in Croatia. The climate allows for tropical and Mediterranean vegetation, including palms, carobs, olives, grapes and lemons. The average rainfall is about per square meter. The island of Vis has a number of natural sources of drinking water from natural spring water reservoirs. It is also home to 12 distinct types of island vegetation. The World Organization for Environmental Protection has named Vis one of the 10 environmentally best-preserved islands in the Mediterranean.
Vis (town) | Climate
The climate is modified Mediterranean, with the highest air temperature averaging during July and the lowest averaging , in January. Summers are usually very hot during the day, temperature goes up to 40 °C. Temperatures above last for more than 250 days a year. Two kinds of wind are common in the area - the northern to north-eastern bora, which usually brings cold and clear weather in winter, and the southern to south-eastern sirocco, which often brings rain.
Imotski | Climate
Makarska experiences a hot-summer Mediterranean climate (Köppen climate classification: "Csa"). Winters are warm and wet, while summers are hot and dry. Makarska is one of the warmest towns in Croatia. Vegetation is the evergreen Mediterranean type, and subtropical flora (palm-trees, agaves, cacti) grow in the town and its surroundings.
Makarska | Climate and vegetation
The climate of Petrovo Polje has the elements of both the cooler and harsher continental climate of the north and the warmer climate predominant in the south. In the winter, jugo and bora winds are common. The average number of frost days per year is 30, between October and April. Summers are dry.
Petrovo Polje, Croatia | Climate
Insolation exceeds Zagreb's by about 100 hours annually. This difference manifests itself during the colder period of the year, from October to March, when more fog occurs in Zagreb.
Medvednica | Temperature
Aranđelovac has a humid continental climate (Köppen climate classification: "Dfb"), that's very close to an oceanic climate (Köppen climate classification: "Cfb").
Aranđelovac | Climate
February is the driest month, averaging 39 mm of precipitation. On average there are 29 days with snowfall, with first snow usually falling in early December. However, in recent years, the number of days with snowfall has decreased sharply. Springs are generally mild and very pleasant with frequent weather changes and are windier than other seasons. Sometimes cold spells can occur, mostly in its early stages. The average daily mean temperature in the winter is around (from December to February) and the average temperature in the summer is . The highest recorded temperature at the Maksimir weather station was in July 1950, and lowest was in February 1956.
Zagreb | Climate
Ploče is the location of Croatia's high temperature record, measured at on 4 August 1981.
Ploče | Climate
Protected from the north by the mountain chain of Alps as well the inner highland, the climate is Mediterranean, very pleasant, with the highest air temperature averaging 24 °C during August, and the lowest averaging 5 °C in January. Summers are usually warm during the day and cooler near the evening, although strange heat wave patterns are common. The weather also ranges from humid to dry with over 10 hours of sunshine daily. Primarily, there is a lot of moisture in the air, especially in the coastal towns of Istra such as Poreč, Vrsar, Rovinj, Pula and others. Temperatures above 10 °C last for more than 240 days a year.
Istria County | Climate
Krivošije are within the Mediterranean subtropical belt. While summers are hot and sunny, autumn, winter and spring are rainy seasons. A peculiarity of the littoral Dinarids is the precipitation regime as the settlements of Orjen receive more precipitation than any others in Europe. Like the monsoon rain it is seasonally distributed, thus November thunderstorms sometimes pour 2000 liters of water in several days, while August is frequently completely dry, leading to forest fires. With a maximum discharge of 350 m³/s water one of the biggest karst springs, the Sopot spring near Risan, is a remarkable indicator of this seasonality. Most of the time it is inactive but after heavy rain a remarkable waterfall appears 20 m above the Bay of Kotor.
Krivošije | Climate
Excessive heat (above 30 °C) lasts for three weeks at most. Despite air temperatures being lower than those of in Dalmatia, the Adriatic sea is warmer, reaching up to 26 °C in August, coldest in March, (9-11 °C), while the freezing even in small, shallow bays is very rare. Two kinds of winds are here - the bora is bringing cold and clear weather from the north in winters, and the southern jugo (jug = south) bringing rain in summer. Maestral is the summer breeze blowing from the inland to the sea. The salinity of the sea water is 0.37%.
Istria County | Climate
A temperature of was recorded on the since defunct Borongaj Airfield in February 1940.
Zagreb | Climate
There are four seasons, with a murky dry winter between early December and early March, a sunny and wetter spring between half of March up to half of May changing to a rainy and warm summer during late May and early September when a dry autumn lasting to late November begins. There are between 1550 and 1800 hours of sunshine in most years.
České Budějovice | Geography
A climate protest attended by thousands of youth held at the European Square in Crotia's capital city of Zagreb, where protesters shouted "Time is now" and "Eco, not ego," while heading towards the city St. Mark's Square (Markov Square).
September 2019 climate strikes | Croatia
The air temperature in this region express the influence of the hot temperature that comes by the valley of the river Vardar, from south The year's average temperature in this region is 14.5C. The thing that is interesting is that during the year there aren’t a temperature that are below 3.2C. During the summer we are witnesses of the extremely high temperatures, and during the winter we can see the opposite, there are extremely low temperatures.
Bogdanci | Temperature
Parg has a cool and wet humid continental climate ("Dfb") due to its geographical position in the Gorski kotar region of Croatia, facing the Adriatic Sea. It's much cooler than either the coast or inland Croatia because of its elevation of 863 m above sea level.
Parg | Climate
Croatia is located in Central and Southeast Europe, on the coast of the Adriatic Sea. It borders Hungary to the northeast, Serbia to the east, Bosnia and Herzegovina and Montenegro to the southeast, and Slovenia to the northwest. It lies mostly between latitudes 42° and 47° N and longitudes 13° and 20° E. Part of the territory in the extreme south surrounding Dubrovnik is a practical exclave connected to the rest of the mainland by territorial waters, but separated on land by a short coastline strip belonging to Bosnia and Herzegovina around Neum. The territory covers , consisting of of land and of water.
Croatia | Geography
Kozica has a Sub-Mediterranean climate, but due to its elevation Kozica has its own microclimate which differs from the Dalmatian Coast. Kozica is situated on a plateau in between two mountains, Biokovo and Sveti Mihovil.
Kozica, Croatia | Climate
The North Adriatic, especially in this part of the Quarner Riviera experiences a mild Mediterranean climate with some continental influence. The summers are sunny, dry and hot, while the winters are rainy and relatively mild with characteristic winds. The average annual air temperature is 14.2 °C. The coldest month is January, while the hottest one is July. Average cloud cover in Dramalj is 0.51 (5.1 tenths of obscured sky), varying from 0.33 to 0.62. Average annual relative humidity is 70%, while the peak rainy period is in October and November. Air pressure averages . Bora and jugo are predominant winds, while Ostro, maestral and levant) blow less often.
Dramalj | Climate
http://www.meteo.si/uploads/probase/www/climate/table/en/by_location/bilje/climate-normals_81-10_Bilje_eng.pdf
Bilje, Miren-Kostanjevica | External links
It is the 127th largest country in the world. Elevation ranges from the mountains of the Dinaric Alps with the highest point of the Dinara peak at near the border with Bosnia and Herzegovina in the south to the shore of the Adriatic Sea which makes up its entire southwest border. Insular Croatia consists of over a thousand islands and islets varying in size, 48 of which are permanently inhabited. The largest islands are Cres and Krk, each of them having an area of around . The hilly northern parts of Hrvatsko Zagorje and the flat plains of Slavonia in the east which is part of the Pannonian Basin are traversed by major rivers such as Danube, Drava, Kupa, and Sava.
Croatia | Geography
Dubrovnik has a borderline humid subtropical ("Cfa") and Mediterranean climate ("Csa") in the Köppen climate classification, since only one summer month has less than of rainfall, preventing it from being classified as solely humid subtropical or Mediterranean. Dubrovnik has hot, muggy, moderately dry summers and mild to cool wet winters. The bora wind blows cold gusts down the Adriatic coast between October and April, and thundery conditions are common all the year round, even in summer, when they interrupt the warm, sunny days. The air temperatures can slightly vary, depending on the area or region. Typically, in July and August daytime maximum temperatures reach , and at night drop to around .
Dubrovnik | Climate
The climate is cold, but dry, conditioned by numerous factors, such as the latitude, altitude, its proximity to the ocean and the predominant vegetation. Its winters are characterized by long cold periods, interspersed by snowfalls and ice-storms, with several weeks of below zero temperatures. The spring, by rule, is very cool, and susceptible to cold-streaks until May, when the vegetation blooms. Summer temperatures are over 35/40 °C.
Boticas | Climate
Mostar, and Herzegovina area in general, enjoy a modified Humid subtropical climate (Cfa) under the Köppen Climate Classification, with cold, humid winters and hot, drier summers. In the summer months, occasional temperatures above are not uncommon, with a record temperature of . The coldest month is January, averaging about , and the warmest month is July, averaging about . The sunniest months are between June and September. The remainder of the year is wet and mild. Mostar is the sunniest city in the country with an average of 2291 solar hours a year. Snow is relatively rare and it usually melts within a few hours or days.
Mostar | Climate
The climate is considered mild and is the classification of Köppen Cfa type (mesothermic humid with hot summers). In summer, though hot, hardly ever reach the 40 °C, and its average is 25 °C. In winter, the average temperature is around 15 °C, but the minimum in the early morning cooler can attain values between 0 °C and 4 °C. The annual average is 19 °C. The climate is generally humid, with mean annual rainfall of 1,500 mm, with no defined dry season (the rainfall regime is typical of the humid subtropical type of climate). Possible floods and droughts hit the city, damaging its economy and population.
Balneário Camboriú | Climate
The relative air humidity is largest during the cold part of the year, and generally is larger on stations with higher altitude because of lower temperatures, but luxuriant vegetation. The number of days with relative humidity above 80% is greatest on Puntijarka (158 days annually), and it decreases with the decrease in elevation; for example, at the Zagreb–Grič station it is 67 days annually. On all stations, the warm part of the year (from April to September) has the most thunderstorm days; these are often connected to showers. June has the most thunderstorm days (Puntijarka 7). The annual precipitation on Medvednica is about 50% higher in comparison to Zagreb (Zagreb: , Sljeme: , Kraljičin zdenac: , Fakultetsko dobro: ).
Medvednica | Precipitation
The city experiences the following seasons and the respective average temperatures:
Dera Bassi | Climate
The warmest month of the year is July, followed by August and June. On average, summer temperatures are about 20 degrees higher than during winter. Especially in the last decade, temperatures above 30 °C are not unusual. Summer is also characterised by rain and storms.
Lčovice | Weather and climate
Regions of Croatia
Outline of Croatia | Regions of Croatia
Sirocco is a warm humid rain and is important as it brings heavy rain. It appears throughout the year but is usually centered in autumn and spring. * monthly and yearly precipitation ranges in Dalmatia, Herzegovina and Montenegro
Orjen | Climate
Köppen-Geiger climate classification system classifies its climate as tropical wet and dry (Aw).It is characterized by a very long rain season and a moderate dry season. This is a mountainous tropical climate and the temperature is under 30 Celsius degrees for the whole year.[ between 16 and 29 degrees Celsius].
Minova | Climate
Bora typically blows from November to February, peaking in strength in January, while jugo is most frequently experienced from May to August with the average maximum in July. Ostro, a southern wind, reaches its maximum in November. A particular climatic feature is the so-called "kalma", "i.e." absolutely calm weather without any wind.
Dramalj | Climate
The climate is humid subtropical (Köppen: "Cfa"), influenced by altered Mediterranean climate which penetrates along the river Bregalnica. The average temperature is with rainfall.
Kočani | Climate
Average temperature from May to September is about , and the average summer sea temperature is rather high, between . The annual average precipitation is . Relative air humidity is at its highest level, 80%, in the fall. Its lowest level, 63%, comes in the summer.
Herceg Novi | Climate
The climate of Hvar is hot-summer Mediterranean ("Csa" in the Köppen climate classification). It has mild winters and hot summers. The yearly average air temperature is , of precipitation fall on Hvar on average every year and the town has a total of 2800 sunshine hours per year. For comparison Hvar has an average of 7.7 sunshine hours per day while Dubrovnik has 7.2. The sea temperatures average from the lowest readings in February of to their warmest during summer, when the sea temperatures usually stay between to . The Köppen Climate Classification subtype for this climate is "Csa" (Mediterranean Climate).
Hvar | Climate
Palagruža has a weather station, established in 1894, which represents a major indicator of weather, especially wind, waves and precipitation on the open Adriatic. Weather conditions on the central Adriatic are dictated by movements of low-pressure area, which causes frequent changes of bora and scirocco (jugo) winds. Annually, Palagruža Island has 104 days with strong (6-7 Bf), and 21 days with stormy winds (>8 Bf). Due to its remote position in the middle of the sea, Palagruža exhibits more Mediterranean climate features than the Croatian coast. Summers are sunny and dry, while most of the rain falls in winter months.
Palagruža | Climate
The area of the municipality belongs to the zone of temperate continental climate with moderately cold winters (average temperature in January –0.7 ºC) and moderately warm summers (average temperature in July 30.9 ºC). The average number of total hours of sunshine is 1,570 hours. The average annual rainfall is about 950 mm, and is evenly distributed throughout the year.
Stanari | Climate
The Geography of Croatia is defined by its location—it is described as a part of Central Europe and Southeast Europe, a part of the Balkans and Mitteleuropa. Croatia's territory covers , making it the 127th largest country in the world. Bordered by Bosnia and Herzegovina and Serbia in the east, Slovenia in the west, Hungary in the north and Montenegro and the Adriatic Sea in the south, it lies mostly between latitudes 42° and 47° N and longitudes 13° and 20° E. Croatia's territorial waters encompass in a wide zone, and its internal waters located within the baseline cover an additional .
Geography of Croatia | Introduction
The warmest months are July and August when the air temperature is between 25 °C and 35 °C (77 °F - 95 °F) and the sea temperature reaches up to 28 °C (83 °F). Rain is rare.
Rogoznica | Climate
The climate is humid continental (Köppen climate classification: "Dfb").
Crni Vrh, Bor | Climate
Ulcinj has a mediterranean climate ("Csa"). Winters are cool and very rainy, and summers are hot and humid with possible afternoon thunder showers. Unlike Podgorica temperatures very rarely exceed and seldom drop below .
Ulcinj | Climate
Winters are usually cold and cloudy; the days are short and snow precipitation is common. January's average temperature is about . Summers are usually warm, with plenty of rain. July's average temperature is about . The highest temperature is: + The lowest temperature is:
Frýdek-Místek | Climate
The climate of the area is continental humid. The average temperature is (average in January and up to average in July). Yearly rainfall averages at , the most rainy month being July. The area's characteristic weak and medium winds blow at about 4 m/s from the south-west (Moravian Gate).
Wodzisław Śląski | Climate
Due to geographical position, climate expresses the natural setting of the relief, region benefiting from a temperate continental climate with warm summers, cold winters, high precipitation, with small differences between mountain, plain and hilly areas. In the village of Bod (Brașov County), was recorded the absolute minimum temperature (−38.5°C), on January 25, 1942.
Macroregiunea Unu | Climate
Although the town is located on the eastern side of Gran Sasso and then exposed to currents mitigatrici of the Adriatic Sea, contrary to what you might think, they are not sufficient to reach this area, which therefore present the typical mountain climate, with cold winters, dry and snowy, thanks to the current Balkan sometimes cold, and summers are dry and hot, with a low moisture content, as opposed to the coastal cities, even increased as a result of summer storms rinfescanti. These climatic conditions, characteristic of the Mediterranean climate allows the cultivation of extensive olive groves and vineyards present extensively throughout the country.
Civitella Casanova | Climate
Kistanje is located in the microregion of Bukovica, in Zagora. Kistanje is from county seat Šibenik, from Knin and from Skradin. The Adriatic Sea is to the south-west. The climate is Mediterranean, with an average of 27 °C in the summer and 8 °C in the winter.
Kistanje | Geography
The western parts of the country have a transitional Mediterranean climate. The hills and mountains are drier, colder, windier, and cloudier. The north region has a typical continental climate.
Geography of Bosnia and Herzegovina | Climate
The climate of Serbia is under the influences of the landmass of Eurasia and the Atlantic Ocean and Mediterranean Sea. With mean January temperatures around , and mean July temperatures of , it can be classified as a warm-humid continental or humid subtropical climate. In the north, the climate is more continental, with cold winters, and hot, humid summers along with well-distributed rainfall patterns. In the south, summers and autumns are drier, and winters are relatively cold, with heavy inland snowfall in the mountains. Differences in elevation, proximity to the Adriatic Sea and large river basins, as well as exposure to the winds account for climate variations.
Serbia | Climate
Climate in this area has mild differences between highs and lows, and there is adequate rainfall year-round. The Köppen Climate Classification subtype for this climate is "" (Marine West Coast Climate/Oceanic climate).
Banatski Karlovac | Climate
The temperature regime is characterized by some special features. Winter temperature inversions occur, and in the summer as a result of overheating of the daily maximum air temperatures rise to . Summer nights are mild or warm with temperatures in the range of , although temperatures tend to drop below in the early mornings for about two hours. The lowest temperature in the city is measured on 20 January 1967 at , and the highest reached both in July and August, most recently on 24 July 2007.
Kyustendil | Climate
Subarctic climate, with an average annual temperature of 0,3C. For the period 1931-1970 the lowest recorded temperature was -27,4C, while the highest - +22,7C.
Cherni Vrah | Climate
Temperate; cool summers; cold, cloudy, humid winters.
Geography of Slovakia | Climate
Croatia (, ; , ), officially the Republic of Croatia (, ), is a country at the crossroads of Central and Southeast Europe on the Adriatic Sea. It borders Slovenia to the northwest, Hungary to the northeast, Serbia to the east, and Bosnia and Herzegovina and Montenegro to the southeast, and it shares a maritime border with Italy. Its capital, Zagreb, forms one of the country's primary subdivisions, along with twenty counties. Croatia has an area of and a population of 4.07 million, most of whom are Catholics. The Croats arrived in the area in the 6th century and organised the territory into two duchies by the 9th century.
Croatia | Introduction
Most of Croatia is lowlands, with elevations of less than above sea level recorded in 53.42% of the country. Most of the lowlands are found in the country's northern regions, especially in Slavonia, representing a part of the Pannonian Basin. Areas with elevations of above sea level encompass 25.61% of Croatia's territory, and the areas between above sea level cover 17.11% of the country. A further 3.71% of the land is above sea level, and only 0.15% of Croatia's territory is elevated greater than above sea level. The greatest concentration of ground at relatively high elevations is found in the Lika and Gorski Kotar areas in the Dinaric Alps, but such areas are found in all regions of Croatia to some extent.
Geography of Croatia | Topography
The climate of the zone is tropical continental, having an annual rainfall of 198.3mm and a seasonal average temperature of more than 28c. Rainfall starts from May and ends November.
Faskari | Climate
Croatia's territory covers , making it the 127th largest country in the world. The physical geography of Croatia is defined by its location—it is described as a part of Southeast Europe Croatia borders Bosnia–Herzegovina (for 1,009.1 km) and Serbia (for 317.6 km) in the east, Slovenia for 667.8 km in the west, Hungary for 355.5 km in the north and Montenegro for 22.6 km and the Adriatic Sea in the south. It lies mostly between latitudes 42° and 47° N and longitudes 13° and 20° E. Part of the extreme south of Croatia is separated from the rest of the mainland by a short coastline strip around Neum belonging to Bosnia–Herzegovina.
Geography of Croatia | Area and borders
Zagreb saw 19 nights in a row where temperature did not fall under , breaking the previous record that was set in the 2013 heat wave. Despite the lack of extreme temperatures seen , the 2018 summer saw temperatures averaging above the mean at all official weather stations and the year as a whole was the hottest on record in Zagreb, which has the tenth oldest contiguously monitoring weather station in the world, operating since 1861.
2018 European heat wave | Croatia
Annual average temperature reaches around 10 °C (50.0 °F), with the warmest month being July with an average of 20 °C and the coldest January with -2 °C. Average annual precipitation is 556 mm.
Veľké Lovce | Geography
The park's climatic condition is a transitory zone. Moderate continental climate dominates from the north while the influence of a southern Mediterranean climate is less pronounced. The typical mountain climate is also largely moderated by the Adriatic Sea.
Sutjeska National Park | Climate
Slovenia is located in temperate latitudes. The climate is also influenced by the variety of relief, and the influence of the Alps and the Adriatic Sea. In the northeast, the continental climate type with greatest difference between winter and summer temperatures prevails. In the coastal region, there is sub-Mediterranean climate. The effect of the sea on the temperature rates is visible also up the Soča valley, while a severe Alpine climate is present in the high mountain regions. There is a strong interaction between these three climatic systems across most of the country. Precipitation, often coming from Gulf of Genoa, varies across the country as well, with over in some western regions and dropping down to in Prekmurje.
Slovenia | Climate
The average temperature is 21°C; the maximum temperature is 37°C in the summer and the minimum, 1°C in the winter. It is located in one of the departments with the highest level of rainfall, which is why the zone is excellent for the agricultural production.
Doctor Moisés Bertoni | Climate