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Difference between revisions of "Physical Environment: Pirtuni"

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''This page is a section of [[Pirtuni]].''[[File:Atropia.png|thumb|Atropia]]
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''This page is a section of [[Pirtuni]].''
 
[[Category:DATE|170]]
 
[[Category:DATE|170]]
 
[[Category:Caucasus]]
 
[[Category:Caucasus]]
 
[[Category:Pirtuni]]
 
[[Category:Pirtuni]]
 
[[Category:Physical Environment]]
 
[[Category:Physical Environment]]
Over 200,000 square miles comprise the Caucasus, a mountainous region located between the Black Sea and Caspian Sea. The Caucasus includes Atropia, Limaria, and Gorgas, as well as parts of Ariana, Donovia, and Kalaria. The Caucasus Mountains, consisting of the Greater and Lesser Caucasus ranges, traditionally form the separation between Europe and Asia. The Caucasus region contains two major parts—the North Caucasus and the South Caucasus—that are divided by the Greater Caucasus Mountains. The North Caucasus region is contained entirely within Donovia,  while the South Caucasus contains Gorgas, Limaria, Atropia, and parts of Ariana and Kalaria.
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Located on the northern shore of the Black Sea in Eastern Europe, Pirtuni consists primarily of relatively flat uplands and lowlands. Fertile soil, adequate precipitation, and favorable terrain contribute to the country’s booming agricultural industry, while navigable rivers and access to the world’s oceans via the Black and Azov Seas support both internal transportation and international commerce. The Carpathian Mountains lie to the far west, providing a natural barrier to entry, while heavy forests and marshes impede travel to northern neighbors. The country enjoys four distinct seasons, with winter being longer in the mountains and summer longer in the south.
  
 
=== Table of Physical Environment Data ===
 
=== Table of Physical Environment Data ===
 
{| class="wikitable"
 
{| class="wikitable"
!Measure
+
| colspan="4" |'''Pirtuni Physical Environment Data'''
!Data
 
!Remarks
 
 
|-
 
|-
|Land Area (sq. miles)
+
|'''Measure'''
|31,848
+
|'''Data'''
|includes inland water
+
|'''Measure'''
 +
|'''Data'''
 
|-
 
|-
|Land Border (miles)
+
|'''Land Area (sq miles)'''
|1,073
+
|223,681
|Ariana (289); Donovia (119); Gorgas (188); Limaria (467)
+
|'''Mean Elevation (ft)'''
 +
|574
 
|-
 
|-
|Coastline (miles)
+
|'''Water Area (sq miles)'''
|556
+
|9,351
|Caspian Sea
+
|'''Arable Land (%)'''
 +
|58
 
|-
 
|-
|Arable (Cultivated) Land (%)
+
|'''Land Border (miles)'''
|23
+
|3,491
|
+
|'''Permanent Crops (%)'''
 +
|1
 +
|-
 +
|'''Coastline (miles)'''
 +
|1,729
 +
|'''Permanent Pasture (%)'''
 +
|14
 
|-
 
|-
|Perm. Crops (%)
+
|'''Lowest Elevation (ft)'''
 +
|0
 +
|'''Irrigated Land (%)'''
 
|3
 
|3
|
 
 
|-
 
|-
|Perm Pasture (%)
+
|'''Highest Elevation (ft)'''
|28
+
|6,762
|
+
|'''Forested Land (%)'''
|-
 
|Irrigated Land (%)
 
 
|17
 
|17
|
 
|-
 
|Forested Land (%)
 
|10
 
|Primarily in the mountains
 
 
|}
 
|}
 
 
__TOC__  
 
__TOC__  
  
 
==Terrain==
 
==Terrain==
[[File:Topography of Atropia.png|thumb|Topography of Atropia]]
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[[File:Pirtunian topography.png|thumb|Topography of Pirtuni]]
The Greater and Lesser Caucasus mountain ranges dominate Atropia’s topography and extend beyond its borders. Atropia occupies a total land area of 31,848 square miles. The country possesses two geographic regions: the mountain ranges and the vast flatlands (sometimes referred to as the Kura-Aras lowland).
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Pirtuni lies in Eastern Europe and possesses a total of 233,032 square miles of territory. It shares a 1,208-mile border with Donovia on its east and abuts the Black Sea and the Sea of Azov to the south. From the highest point of Mt. Hoverla, located in the Carpathian Mountains in the far west, the land descends eastward to the fertile plateaus and plains of the uplands. Lowlands lie to the northeast of the Dnieper River and along the seacoasts, while marshes lie in the northwest. Hills define the far eastern region. The Azov Peninsula, which separates the Black and Azov seas, is lowland except for a small mountain range on its southern edge. The elevation of most of the country is less than 1,000 feet above sea level, though both mountainous areas exceed five times that height.
  
 
===Bodies of Water===
 
===Bodies of Water===
A dam on the Kura River in the northwestern part of the country creates Atropia’s largest body of water, the Mingachevir Reservoir, at 233.5 square miles. The reservoir possesses a flow capacity of 15,730 million cubic meters per year and is used for flood control, irrigation, and hydroelectric power. The Kura is the longest river in Atropia and in the Caucasus region. The river originates in Kalaria and flows 932 miles to the Caspian Sea, with 559 miles in Atropia. The Kura plays an important role in maritime transportation as Atropia’s only navigable river, with only the lower 310 miles passable for ships. The Kura is rated at more than 2.5 grams of suspended particle per liter of river water, making it one of the most turbid (cloudy) rivers in the world. The Aras River also originates in Kalaria and flows along the southern border with Ariana to form Atropia’s second-longest river.
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The country borders two bodies of water on the south: the Black Sea and the Sea of Azov. The Black Sea is shallow in the gulf formed by the southwestern mainland and the Azov Peninsula, but quickly deepens along the southern coast of the latter. Separated from the Black Sea by the Kerch Strait, the Sea of Azov is the world’s shallowest sea, with a maximum depth of only 46 feet. It is rich in fish and other marine life, and is fished extensively. Its far western region, between the Azov Peninsula and the Pirtunian mainland, consists of salt marshes. There are multiple ports on both bodies of water.
 +
 
 +
Pirtuni possesses an extensive river system, with the vast majority of rivers eventually flowing into the Black or Azov Seas. The Dnieper, which follows a meandering 680-mile path from the northern border to the Black Sea, is the country’s largest and most important river. Containing multiple reservoirs along its course, the waterway is used extensively for irrigation, transportation, and hydroelectric power generation. The Dniester is the second-largest river in Pirtuni; other major watercourses include the Desna, Donets, Prypyats, Prut, Southern Buh, and Western Buh. At least parts of all of these rivers are navigable in Pirtuni.
  
 
==Mobility Classification==
 
==Mobility Classification==
Heavily populated areas such as Baku, Ganja, Sumgayit, Shirvan, and Mingachevir will slow down troop movement and hinder operations because of their construction patterns. The close construction provides numerous hideouts and concealed movement opportunities for fighters. Underground passageways, rooftops, and narrow streets will allow fighters to move easily from building to building. On the other hand, houses in rural villages remain relatively small and dispersed, and  their low population density will favor military activities. Roads throughout Atropia exhibit poor condition, lighting, and signage that will further complicate vehicular traffic. Inadequate maintenance of those roads and bridges leads to poor trafficability and could increase vehicle maintenance requirements.
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Much of Pirtuni consists of relatively flat, open terrain bisected by multiple streams and rivers. Ravines and gorges are common in the upland areas, but less so at the lower elevations. Marshes, bogs, and forests interfere with mobility in the far north. The heavily-treed Carpathian Mountains in the southwest are a considerable obstacle for those wishing to enter the country from that direction. The Azov Mountains provide a natural barrier on the southern shore of that peninsula, and marshes on the shore of the Azov Sea prevent easy access from the east. Seasonal barriers to mobility include snowstorms and ice in the winter—especially in the mountains; dust storms and flooding in the spring; and thunderstorms and flooding in the summer. Fog occurs frequently in the mountains, but is a rare visitor to the lowlands.
 
 
The central lowlands offer the best opportunity for military travel in Atropia as the rolling hills and flat plains in the Kura-Aras lowland will expedite the travel of armored or mechanized forces. The defender will use the Kura-Aras lowland terrain to defend his avenues of approach. This lowland terrain will offer adequate cover and concealment to both the offense and the defense.
 
 
 
Atropia’s mountainous regions serve as perfect hideouts for fighters and facilitate smuggling. The mountainous terrain will force mechanized or armored forces to slow their movements or find alternate routes to conduct missions. The rugged terrain will also pose an obstacle to dismounted infantry forces. The Greater and Lesser Caucasus mountain ranges will make movement across the mountainous terrain difficult and suitable for enemy ambushes. In winter, heavy snowfalls and frost may close some mountain passes for three to six months and force planners to find longer alternate routes. Unpredictable mud volcanoes west of Sangacal (southwest of Baku) and northeast of Baku will negatively influence military missions in those areas.
 
  
 
==Natural Hazards==
 
==Natural Hazards==
Atropia suffers from a few types of natural disasters—earthquakes, floods, and landslides. Atropia lies in an area with high seismic activity. The United Nations Development Programme suggests that Atropia could receive magnitude 8-9 earthquakes on the Richter scale. The northern region and the Tramaz and Hachzi peninsulas in the eastern part of the country suffer the most earthquakes. The most dangerous areas include the slopes of the Greater Caucasus Mountains.
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Many of Pirtuni’s natural hazards are seasonally-dependent. Snowstorms are common in the winter in the southeast, and ice is heavy in the Carpathian Mountains. Come spring, the melting snowpack can create flooding and cause rivers to overrun their banks. Strong wind gusts and dust storms are also common at that time of year, and thunderstorms—sometimes accompanied by hail—occur frequently in the summer. Drought can occur any time from spring through fall, affecting the country’s agricultural output.
  
Snow melts and heavy rains during the spring and fall often cause the Kura and Aras Rivers to overflow and initiate flooding in Atropia. Heavy rains, snow melts, and strong precipitation trigger many landslides in Atropia. Landslides generally occur in the spring season and mostly in the country’s northern part.
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Earthquakes occur primarily in the Azov Peninsula and the Carpathian Mountains, though tremors in the central part of the country are not unknown. Most quakes range from 3.0–4.9 on the Richter scale, though both larger and smaller ones have occurred. The largest earthquake in recent history took place just off the southern coast of the Azov Peninsula on 11 September 1927. It measured 6.7 on the Richter scale and triggered a small tsunami with waves less than two feet high.
  
 
==Subterranean Environment==
 
==Subterranean Environment==
Atropia, in its defensive military efforts against Limaria, has developed a small subterranean environment consisting of tunnels near the Atropian-Limarian border. These tunnels, while small, facilitate the movement of people and supplies for Atropian troops. In addition to the the government-regulated tunnels, insurgent forces supported by the Donovian government have created a network of tunnels to facilitate easy movement between Donovia and Atropia. These tunnels are also used for the movement of personnel and supplies to support the operations of these forces, including the Bilasuvar Freedom Brigade (BFB), within the borders of Atropia.
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Pirtuni has a large subterranean environment due to the prevalence of limestone. Naturally-occurring caves can be found throughout the country—both in the mountains and in the plains—as well as man- made tunnels resulting from mining operations. Criminal and insurgent elements are known to create tunnel systems for smuggling and for freedom of movement, as well as to serve as cache locations and safehouses. It is reported that the government has built at least one underground complex—though its purpose remains unclear and is subject to much rumor and speculation.
 
 
Both regular forces and insurgents involved in the Lower Janga conflict—the Limarian Liberation Front (LLF) and the Free Lower Janga Movement (FLJM)—have established tunnels in Lower Janga for freedom of movement and logistical purposes, with some of the FLJM’s tunnels crossing over into Atropian-controlled territory.
 
 
 
There are two violent extremist organizations based on religion that operate in Atropia and use UGFs. The first is One Right Path (ORP), which is a Shia Muslim violent extremist splinter group of about 5,000 active members whose goal is the establishment of a regional Islamic Caliphate. ORP wants to overthrow the Atropian government and, while there are rumors of some sort of association with Ariana, there is nothing confirmed by any authority. In cities that have underground passageways, this group will often meet in them or use them to move clandestinely around the city.
 
 
 
The second violent extremist splinter group is The True Believers (TTB), a Sunni-based group of about 5,000 members. Its goal is the transformation or elimination of any Muslims of the Shia faith, but eventually a worldwide Islamic Caliphate. While this group does not build tunnels, it will take full advantage of any UGFs it happens across in its area of operations.
 
 
 
To further complicate the subterranean environment, there are several organized criminal organizations that operate throughout Atropia. These organizations have sponsored their own networks of tunnels in northern Atropia, where the Al Iksir Cartel operates, and in Baku, where the Bocyowicz Crime Family operates. Criminal groups from outside the country, including the Donovian Mafia, have also constructed their own tunnels into the country. Atropian law enforcement also estimates that there are around 20–30 cross-border smuggling tunnels into neighboring countries.
 
  
 
==Vegetation==
 
==Vegetation==
 
===Land Cover===
 
===Land Cover===
Forests cover only about 10% of Atropia and most consist of broad-leaf trees. The Greater Caucasus Mountains possess vast forest areas on the northern slopes of their eastern section. In Atropia’s southeast region, the forests disappear and more arid areas generally dominate. While the forests exhibit a very diverse variety of trees, the main broad-leaf trees include hornbeam, pistachio, and oak.
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Forests cover 17% of Pirtuni’s area, and lie primarily in the mountainous areas and in the far north of the country. The country can be broken into five regions based on vegetation: Carpathian Mountain zone, Azov Mountain zone; polissya zone; forest-steppe zone; and steppe zone. The Carpathian Mountains contain deciduous trees at lower elevations, followed by conifer forests higher up and alpine meadows at the highest elevations. The Azov Mountains possess deciduous trees and shrubs in abundance. The polissya zone occupies the northern part of the country and consists of a mix of conifers and deciduous trees, as well as marshes, bogs, and natural pastureland. The forest-steppe zone lies south of the polissya zone. Containing primarily rich agricultural land and some deciduous trees, it accounts for one- third of the country. The steppe zone takes up the southern third of the country, and is characterized by flat, treeless plains. Common tree species in Pirtuni include Alder, Beech, Birch, Hornbeam, Oak, Pine, and Spruce.
  
 
===Agriculture===
 
===Agriculture===
While 38% of Atropians work in agriculture-related occupations, farming only produces 5.5% of the country’s GDP. The agriculture sector employs over three times the number involved in industry.  The arable land and variable climate allow for diverse crop cultivation that includes vegetables, fruits, tea, grains, and nuts, the with majority of agricultural activity occurring in the Kura- Aras Lowland. Cotton reigns as Atropia’s largest agricultural product.
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Pirtuni has a rich agricultural heritage stemming from its abundant resources in this area. Over half of the country (59%) consists of cropland that produces corn, grains (primarily wheat), grapes and other fruits, legumes, potatoes, sugar beets, sunflower seeds, tobacco, and vegetables. An additional 14% is pastureland for livestock, primarily cattle. Most agricultural activity takes place in the forest-steppe and steppe zones, with irrigation being practiced in some areas of the latter. Farmers make use of Western agricultural techniques—though not to the level of sophistication found in the most advanced countries—that allow only 7% of the populace to farm great expanses of land. Agriculture makes up 13% of Pirtuni’s GDP, and the country is a net food exporter.
  
 
==Climate==
 
==Climate==
Atropia exhibits a wide variety of climates dependent on location, elevation, and proximity to the Caspian Sea. Based on altitude and distance from the Caspian Sea coastline, parts of Atropia enjoy dry-subtropical, wet-subtropical, temperate, and alpine climates. The Kura-Aras lowland, the Tramaz Peninsula, and the Hachzi Peninsula exhibit a dry-subtropical climate, while the Talish Mountains feature a wet-subtropical climate. Temperate climates dominate the slopes of the Greater and Lesser Caucasus Mountains, while the ridges and peaks feature an alpine climate.
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Nearly all of Pirtuni enjoys a continental climate, with the southern coast of the Azov Peninsula experiencing a Mediterranean climate. Summers are warm and sunny, with nearly 10 hours of sunlight per day. Winters are cold and cloudy, with only 2–3 hours of sunshine daily. Hours of sunlight are higher in the south than in the north, as are average temperatures. Precipitation occurs primarily in the summer (rain) and winter (snow), with lulls in the spring and fall. Climate in the mountains varies with elevation, with lower temperatures and longer winters associated with the higher altitudes.
  
 
===Seasons===
 
===Seasons===
 
{| class="wikitable"
 
{| class="wikitable"
 +
| colspan="3" |'''Pirtunian Seasons'''
 +
|-
 
|'''Season'''
 
|'''Season'''
|Months
+
|'''Months'''
 +
|'''Remarks'''
 
|-
 
|-
|Winter
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|'''Winter'''
|Jan – Mar
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|December–March
 +
|Longer in the mountains
 
|-
 
|-
|Spring
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|'''Spring'''
|Mar – End May
+
|April–May
 +
|
 
|-
 
|-
|Summer
+
|'''Summer'''
|Jun – Oct
+
|June–September
 +
|Longer in the south
 
|-
 
|-
|Fall
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|'''Fall'''
|Mid Oct – Dec
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|October–November
 +
|
 
|}
 
|}
  
 
===Weather===
 
===Weather===
 
====Precipitation====
 
====Precipitation====
The location and the season dramatically affect precipitation throughout Atropia. In the east, along the Caspian Sea, most precipitation occurs in the fall and winter. In that period, communication systems can lose effectiveness. In the west, most precipitation occurs in spring and early summer. The southern coast of the Tramaz Peninsula receives the lowest annual precipitation, which varies from 8 to 12 inches. Along the Caspian Sea to the south, precipitation can reach between 47 to 55 inches annually.
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Most precipitation in the country occurs in the summer in the form of rain, and snow covers most of the country during the winter. Average precipitation amounts are highest in the mountains, and decrease from west to east and from north to south, with the Azov Mountains being a notable exception. The Carpathian and Azov Mountains receive 30–60 inches of precipitation per year, the polissya zone experiences 23–30, the forest-steppe zone has 19–27, and the steppe zone receives under 20 inches.
  
 
====Temperature-Heat Index====
 
====Temperature-Heat Index====
July and August produce the hottest temperatures in Atropia, especially in the lowlands. The lowest summer average daily temperatures in the lowlands may only fall to 79°F, and temperatures in Baku often surpass 100°F.
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June through August produce the hottest temperatures in Pirtuni, especially along the coasts. The lowest summer average temperature—54°F—is found in the Carpathian and Azov Mountains, while the highest (75°F) is on the Azov Peninsula. Most areas of the country experience average summer highs of 63–72°F, with temperatures increasing from north to south and from west to east. Absolute highs range from 101–106°F. Combined with relative humidity in the 55–75% range, summer weather can be very uncomfortable in the country.
  
 
====Temperature-Wind Chill Index====
 
====Temperature-Wind Chill Index====
In winter, the highest Atropian mountain areas can become very cold, with sub-zero temperatures. January represents Atropia’s coldest month, with daily temperatures around 36°F in the lowlands and 14°F in the mountains.
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Average lows in Pirtuni are sub-freezing, and range from 15–32°F during December–February. Winter temperatures follow a different pattern than summer ones: while temperatures still increase from north to south, they also increase from east to west—opposite of what is seen in the summer months. The warmest area of the country is the western shore of the Azov Peninsula, with an average temperature lying above 32°F. Absolute lows in Pirtuni range from -30°F to -42°F.
  
 
====Relative Humidity====
 
====Relative Humidity====
Relative humidity varies dependent on location. In the drier areas of the country, such as the Kura-Aras lowland and the Tramaz Peninsula, humidity is around 60–65% in the summer and higher in the winter. The lower elevations of the Greater and Lesser Caucasus Mountains are considerably more humid. The most humid part of the country is the Talish Mountains region, with humidity peaking in spring and summer.
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Relative humidity is moderate to high and varies seasonally in Pirtuni. The months of April–August are the driest, with the monthly average ranging between 55–75% in all but the western coastal areas, where the humidity is slightly higher. The November–February timeframe experiences the highest relative humidity, which ranges from 75–90%. Relative humidity is higher in the western part of the country, and can drop significantly in the southeast during periods of drought.
  
 
====Wind====
 
====Wind====
Numerous winds traverse Atropia, but the most common winds include the Gilavar and Khazri. The Khazri blows from the north and the Gilavar from the southwest. In the lowlands, winds usually  blow in the southeastern and northwestern directions. Winds reach higher speeds in the Tramaz and Hachzi peninsulas, where strong, stormy winds are considered normal. Generally, winds throughout the rest of the country reflect lower speeds that favor air assault, airborne, and aviation operations.
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The country experiences mild to moderate wind year-round, with relatively modest seasonal variation in wind speed. Winds are stronger from November–March—particularly in the spring months—and  weaker from June–October, with many areas experiencing a noticeable lull in August–September. Average monthly wind speed ranges from 5–14 mph in winter to 2–10 mph in summer, depending on region, but does not vary by more than 6 mph for any fixed location. Moist air from the Atlantic and Mediterranean plays a larger role in the winter and in the western part of the country, while dry air from Central Asia has greater influence in the south and east, and during the summer. Gale-force winds are possible on the Black Sea, and dust storms occur in the southeast regions during the summer.
  
 
==Summary==
 
==Summary==
The Caucasus region, containing the Greater and Lesser Caucasus Mountains, forms the traditional division between Europe and Asia. All countries contain different weather and terrain, and soldiers must prepare for seasonal extremes—winter and summer. Areas with flat plains and valleys, such as coastal plains, will favor troop mechanized movement. The mountainous regions, especially in the Greater and Lesser Caucasus Mountains, will compound vehicle and equipment breakdowns. Numerous roads, already in poor condition in most of the countries, will become inaccessible for vehicular traffic because of winter snow. Military planners will need to anticipate the closure of mountain passes for up to six months a year due to snow.
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Pirtuni enjoys favorable terrain for military movement with seasons that, while varied, are not extreme. Mountains, forests, and marshes are the primary obstacles in the far west, the far north, and on the Azov Peninsula, while ravines—including some that are man-made, due to mining—and bodies of water are the main impediments throughout the remainder of the country. Seasonal weather presents additional challenges, including snow in the mountains and warm, humid weather in the south. Black Sea access and navigable rivers provide additional options for transportation.

Revision as of 16:38, 26 March 2018

This page is a section of Pirtuni. Located on the northern shore of the Black Sea in Eastern Europe, Pirtuni consists primarily of relatively flat uplands and lowlands. Fertile soil, adequate precipitation, and favorable terrain contribute to the country’s booming agricultural industry, while navigable rivers and access to the world’s oceans via the Black and Azov Seas support both internal transportation and international commerce. The Carpathian Mountains lie to the far west, providing a natural barrier to entry, while heavy forests and marshes impede travel to northern neighbors. The country enjoys four distinct seasons, with winter being longer in the mountains and summer longer in the south.

Table of Physical Environment Data

Pirtuni Physical Environment Data
Measure Data Measure Data
Land Area (sq miles) 223,681 Mean Elevation (ft) 574
Water Area (sq miles) 9,351 Arable Land (%) 58
Land Border (miles) 3,491 Permanent Crops (%) 1
Coastline (miles) 1,729 Permanent Pasture (%) 14
Lowest Elevation (ft) 0 Irrigated Land (%) 3
Highest Elevation (ft) 6,762 Forested Land (%) 17

Terrain

Topography of Pirtuni

Pirtuni lies in Eastern Europe and possesses a total of 233,032 square miles of territory. It shares a 1,208-mile border with Donovia on its east and abuts the Black Sea and the Sea of Azov to the south. From the highest point of Mt. Hoverla, located in the Carpathian Mountains in the far west, the land descends eastward to the fertile plateaus and plains of the uplands. Lowlands lie to the northeast of the Dnieper River and along the seacoasts, while marshes lie in the northwest. Hills define the far eastern region. The Azov Peninsula, which separates the Black and Azov seas, is lowland except for a small mountain range on its southern edge. The elevation of most of the country is less than 1,000 feet above sea level, though both mountainous areas exceed five times that height.

Bodies of Water

The country borders two bodies of water on the south: the Black Sea and the Sea of Azov. The Black Sea is shallow in the gulf formed by the southwestern mainland and the Azov Peninsula, but quickly deepens along the southern coast of the latter. Separated from the Black Sea by the Kerch Strait, the Sea of Azov is the world’s shallowest sea, with a maximum depth of only 46 feet. It is rich in fish and other marine life, and is fished extensively. Its far western region, between the Azov Peninsula and the Pirtunian mainland, consists of salt marshes. There are multiple ports on both bodies of water.

Pirtuni possesses an extensive river system, with the vast majority of rivers eventually flowing into the Black or Azov Seas. The Dnieper, which follows a meandering 680-mile path from the northern border to the Black Sea, is the country’s largest and most important river. Containing multiple reservoirs along its course, the waterway is used extensively for irrigation, transportation, and hydroelectric power generation. The Dniester is the second-largest river in Pirtuni; other major watercourses include the Desna, Donets, Prypyats, Prut, Southern Buh, and Western Buh. At least parts of all of these rivers are navigable in Pirtuni.

Mobility Classification

Much of Pirtuni consists of relatively flat, open terrain bisected by multiple streams and rivers. Ravines and gorges are common in the upland areas, but less so at the lower elevations. Marshes, bogs, and forests interfere with mobility in the far north. The heavily-treed Carpathian Mountains in the southwest are a considerable obstacle for those wishing to enter the country from that direction. The Azov Mountains provide a natural barrier on the southern shore of that peninsula, and marshes on the shore of the Azov Sea prevent easy access from the east. Seasonal barriers to mobility include snowstorms and ice in the winter—especially in the mountains; dust storms and flooding in the spring; and thunderstorms and flooding in the summer. Fog occurs frequently in the mountains, but is a rare visitor to the lowlands.

Natural Hazards

Many of Pirtuni’s natural hazards are seasonally-dependent. Snowstorms are common in the winter in the southeast, and ice is heavy in the Carpathian Mountains. Come spring, the melting snowpack can create flooding and cause rivers to overrun their banks. Strong wind gusts and dust storms are also common at that time of year, and thunderstorms—sometimes accompanied by hail—occur frequently in the summer. Drought can occur any time from spring through fall, affecting the country’s agricultural output.

Earthquakes occur primarily in the Azov Peninsula and the Carpathian Mountains, though tremors in the central part of the country are not unknown. Most quakes range from 3.0–4.9 on the Richter scale, though both larger and smaller ones have occurred. The largest earthquake in recent history took place just off the southern coast of the Azov Peninsula on 11 September 1927. It measured 6.7 on the Richter scale and triggered a small tsunami with waves less than two feet high.

Subterranean Environment

Pirtuni has a large subterranean environment due to the prevalence of limestone. Naturally-occurring caves can be found throughout the country—both in the mountains and in the plains—as well as man- made tunnels resulting from mining operations. Criminal and insurgent elements are known to create tunnel systems for smuggling and for freedom of movement, as well as to serve as cache locations and safehouses. It is reported that the government has built at least one underground complex—though its purpose remains unclear and is subject to much rumor and speculation.

Vegetation

Land Cover

Forests cover 17% of Pirtuni’s area, and lie primarily in the mountainous areas and in the far north of the country. The country can be broken into five regions based on vegetation: Carpathian Mountain zone, Azov Mountain zone; polissya zone; forest-steppe zone; and steppe zone. The Carpathian Mountains contain deciduous trees at lower elevations, followed by conifer forests higher up and alpine meadows at the highest elevations. The Azov Mountains possess deciduous trees and shrubs in abundance. The polissya zone occupies the northern part of the country and consists of a mix of conifers and deciduous trees, as well as marshes, bogs, and natural pastureland. The forest-steppe zone lies south of the polissya zone. Containing primarily rich agricultural land and some deciduous trees, it accounts for one- third of the country. The steppe zone takes up the southern third of the country, and is characterized by flat, treeless plains. Common tree species in Pirtuni include Alder, Beech, Birch, Hornbeam, Oak, Pine, and Spruce.

Agriculture

Pirtuni has a rich agricultural heritage stemming from its abundant resources in this area. Over half of the country (59%) consists of cropland that produces corn, grains (primarily wheat), grapes and other fruits, legumes, potatoes, sugar beets, sunflower seeds, tobacco, and vegetables. An additional 14% is pastureland for livestock, primarily cattle. Most agricultural activity takes place in the forest-steppe and steppe zones, with irrigation being practiced in some areas of the latter. Farmers make use of Western agricultural techniques—though not to the level of sophistication found in the most advanced countries—that allow only 7% of the populace to farm great expanses of land. Agriculture makes up 13% of Pirtuni’s GDP, and the country is a net food exporter.

Climate

Nearly all of Pirtuni enjoys a continental climate, with the southern coast of the Azov Peninsula experiencing a Mediterranean climate. Summers are warm and sunny, with nearly 10 hours of sunlight per day. Winters are cold and cloudy, with only 2–3 hours of sunshine daily. Hours of sunlight are higher in the south than in the north, as are average temperatures. Precipitation occurs primarily in the summer (rain) and winter (snow), with lulls in the spring and fall. Climate in the mountains varies with elevation, with lower temperatures and longer winters associated with the higher altitudes.

Seasons

Pirtunian Seasons
Season Months Remarks
Winter December–March Longer in the mountains
Spring April–May
Summer June–September Longer in the south
Fall October–November

Weather

Precipitation

Most precipitation in the country occurs in the summer in the form of rain, and snow covers most of the country during the winter. Average precipitation amounts are highest in the mountains, and decrease from west to east and from north to south, with the Azov Mountains being a notable exception. The Carpathian and Azov Mountains receive 30–60 inches of precipitation per year, the polissya zone experiences 23–30, the forest-steppe zone has 19–27, and the steppe zone receives under 20 inches.

Temperature-Heat Index

June through August produce the hottest temperatures in Pirtuni, especially along the coasts. The lowest summer average temperature—54°F—is found in the Carpathian and Azov Mountains, while the highest (75°F) is on the Azov Peninsula. Most areas of the country experience average summer highs of 63–72°F, with temperatures increasing from north to south and from west to east. Absolute highs range from 101–106°F. Combined with relative humidity in the 55–75% range, summer weather can be very uncomfortable in the country.

Temperature-Wind Chill Index

Average lows in Pirtuni are sub-freezing, and range from 15–32°F during December–February. Winter temperatures follow a different pattern than summer ones: while temperatures still increase from north to south, they also increase from east to west—opposite of what is seen in the summer months. The warmest area of the country is the western shore of the Azov Peninsula, with an average temperature lying above 32°F. Absolute lows in Pirtuni range from -30°F to -42°F.

Relative Humidity

Relative humidity is moderate to high and varies seasonally in Pirtuni. The months of April–August are the driest, with the monthly average ranging between 55–75% in all but the western coastal areas, where the humidity is slightly higher. The November–February timeframe experiences the highest relative humidity, which ranges from 75–90%. Relative humidity is higher in the western part of the country, and can drop significantly in the southeast during periods of drought.

Wind

The country experiences mild to moderate wind year-round, with relatively modest seasonal variation in wind speed. Winds are stronger from November–March—particularly in the spring months—and  weaker from June–October, with many areas experiencing a noticeable lull in August–September. Average monthly wind speed ranges from 5–14 mph in winter to 2–10 mph in summer, depending on region, but does not vary by more than 6 mph for any fixed location. Moist air from the Atlantic and Mediterranean plays a larger role in the winter and in the western part of the country, while dry air from Central Asia has greater influence in the south and east, and during the summer. Gale-force winds are possible on the Black Sea, and dust storms occur in the southeast regions during the summer.

Summary

Pirtuni enjoys favorable terrain for military movement with seasons that, while varied, are not extreme. Mountains, forests, and marshes are the primary obstacles in the far west, the far north, and on the Azov Peninsula, while ravines—including some that are man-made, due to mining—and bodies of water are the main impediments throughout the remainder of the country. Seasonal weather presents additional challenges, including snow in the mountains and warm, humid weather in the south. Black Sea access and navigable rivers provide additional options for transportation.

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