Geography Geographical position and climate
The urban area covers 405.17 km² (230.25 km² on the left bank of the Rhine, 174.87 km² on the right bank). Only the city-states of Berlin and Hamburg and four small and medium-sized cities in Saxony-Anhalt and Brandenburg have a larger urban area in Germany.
The city's topographic reference point, the top of the northern cathedral tower, is located at 50° 56′ 33″ north latitude and 6° 57′ 32″ east longitude. The highest point is 118.04 meters (Monte Troodelöh in the Königsforst); the lowest 37.5 meters above sea level (in the Worringer Bruch).
The city is located in the Cologne Bay, a funnel-shaped river valley landscape shaped by the Rhine between the stepped slopes of the Bergisches Land and the Eifel immediately after the Rhine emerges from the Rhenish Slate Mountains. This protected, favorable location results in a mild climate for Cologne.
| Cologne-Stammheim (43 m) 2015-2020 |
| Climate diagram |
| J | F | M | A | M | J | J | A | S | O | N | D | | | | | | | | | | | | | | | Temperature in °C, precipitation in mm | | Source: [1] | |
Monthly average temperatures and precipitation for Cologne-Stammheim (43 m) 2015-2020 | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | | | | Max. Temperature (°C) | 6,7 | 8,5 | 11,8 | 17,0 | 20,7 | 24,5 | 26,1 | 26,1 | 21,6 | 15,7 | 11,0 | 8,7 | Ø | 16,6 | | Min. temperature (°C) | 1,7 | 1,8 | 3,6 | 6,0 | 9,8 | 14,1 | 15,4 | 15,4 | 11,6 | 8,7 | 5,1 | 3,9 | Ø | 8,1 | | Temperature (°C) | 4,2 | 5,0 | 7,6 | 11,6 | 15,3 | 19,3 | 20,6 | 20,5 | 16,2 | 12,0 | 8,0 | 6,3 | Ø | 12,3 | | | Precipitation (mm) | 72,8 | 58,5 | 65,0 | 37,0 | 44,4 | 73,0 | 60,0 | 67,6 | 55,7 | 54,4 | 66,2 | 71,3 | Σ | 725,9 | | Temperature | | | | | | | | | | | | | | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | | Precipitation | 72,8 | 58,5 | 65,0 | 37,0 | 44,4 | 73,0 | 60,0 | 67,6 | 55,7 | 54,4 | 66,2 | 71,3 | | | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | |
Cologne is located in the greater area of the transition zone from a temperate maritime climate to a continental climate with mild winters (January average: 3.0 °C) and moderately warm summers (July average: 19.0 °C). The average annual precipitation is 802 millimeters, which is in line with the German average and considerably higher than in the neighboring Rhine-Erft district to the west (Erftstadt-Bliesheim: 631 mm) or the Jülich-Zülpicher Börde (Zülpich: 582 mm), which gives commuters the impression of a "rain hole".
The weather station Cologne-Stammheim can be used as a representative of the urban climate of Cologne. It can be seen that the winter temperatures are among the mildest in all of Germany and the temperature minima are very high due to the urban microclimate. The mean values from the period 2015-2020 are quite similar to the values from the climate mean of Lyon over the years 1961-1990.
| Cologne |
| Climate diagram |
| J | F | M | A | M | J | J | A | S | O | N | D | | | | | | | | | | | | | | | Temperature in °C, precipitation in mm | | Source: DWD, data: 1991-2020 | |
Climate data Cologne Station Cologne/Bonn (Flugh.), 91 m above sea level | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | | | | Max. Temperature (°C) | 5,9 | 7,2 | 11,4 | 16,1 | 19,7 | 22,7 | 24,9 | 24,5 | 20,4 | 15,2 | 9,8 | 6,5 | Ø | 15,4 | | Min. temperature (°C) | 0,0 | 0,1 | 2,0 | 4,5 | 8,1 | 11,2 | 13,3 | 12,8 | 9,7 | 6,8 | 3,5 | 1,0 | Ø | 6,1 | | Temperature (°C) | 3,0 | 3,6 | 6,7 | 10,4 | 14,1 | 17,1 | 19,0 | 18,5 | 14,8 | 10,8 | 6,7 | 3,8 | Ø | 10,7 | | | Precipitation (mm) | 61,7 | 53,8 | 55,0 | 48,2 | 62,1 | 86,3 | 87,4 | 83,3 | 66,9 | 64,7 | 63,5 | 69,2 | Σ | 802,1 | | | Sunshine hours (h/d) | 1,8 | 2,8 | 4,0 | 5,8 | 6,4 | 6,7 | 6,7 | 6,3 | 5,0 | 3,4 | 2,0 | 1,5 | Ø | 4,4 | | Temperature | | | | | | | | | | | | | | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | | Precipitation | 61,7 | 53,8 | 55,0 | 48,2 | 62,1 | 86,3 | 87,4 | 83,3 | 66,9 | 64,7 | 63,5 | 69,2 | | | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | Source: DWD, data: 1991-2020 |
| Cologne |
| Climate diagram |
| J | F | M | A | M | J | J | A | S | O | N | D | | | | | | | | | | | | | | | Temperature in °C, precipitation in mm | | Source: DWD, data: 1961-1990 | |
Climate data Cologne Station Cologne/Bonn (Flugh.), 91 m above sea level | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | | | | Max. Temperature (°C) | 4,5 | 6,2 | 9,8 | 13,8 | 18,5 | 21,4 | 23,1 | 23,0 | 19,7 | 15,0 | 8,9 | 5,5 | Ø | 14,2 | | Min. temperature (°C) | −1,3 | −1,2 | 1,1 | 3,6 | 7,6 | 10,7 | 12,4 | 12,1 | 9,5 | 6,3 | 2,4 | −0,2 | Ø | 5,3 | | Temperature (°C) | 1,8 | 2,5 | 5,3 | 8,8 | 13,3 | 16,4 | 18,0 | 17,5 | 14,3 | 10,4 | 5,7 | 2,9 | Ø | 9,8 | | | Precipitation (mm) | 62,0 | 48,0 | 64,0 | 55,0 | 74,0 | 86,0 | 84,0 | 77,0 | 62,0 | 55,0 | 66,0 | 72,0 | Σ | 805 | | | Sunshine hours (h/d) | 1,5 | 2,8 | 3,5 | 5,2 | 6,2 | 6,2 | 6,3 | 5,9 | 4,8 | 3,6 | 2,0 | 1,4 | Ø | 4,1 | | | Rainy days (d) | 13,0 | 10,0 | 13,0 | 11,0 | 12,0 | 12,0 | 11,0 | 10,0 | 10,0 | 9,0 | 12,0 | 13,0 | Σ | 136 | | | Humidity (%) | 82 | 78 | 75 | 70 | 69 | 70 | 71 | 73 | 78 | 80 | 82 | 83 | Ø | 75,9 | | Temperature | | | | | | | | | | | | | | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | | Precipitation | 62,0 | 48,0 | 64,0 | 55,0 | 74,0 | 86,0 | 84,0 | 77,0 | 62,0 | 55,0 | 66,0 | 72,0 | | | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | Source: DWD, data: 1961-1990 |
Over the past 30 years, temperatures in Cologne have risen noticeably on a long-term average; while the average daily maximum temperature in July for the period 1961 to 1990 was still around 23 °C, it is around 25 °C for the years 1991 to 2020. Winters have also become warmer; while the average daily maximum temperature in January for the years 1961 to 1990 was still 4.5 °C, it was 5.9 °C for the period 1991 to 2020.
The mean precipitation profile, however, has hardly changed, the annual precipitation amount has remained about the same on average. On the other hand, the number of sunshine hours has increased from 4.1 to 4.4 hours per day over the last 30 years.
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Cologne panorama seen from Severinsbrücke bridge looking north, October 2019
Air quality and environmental protection
Energy production, industry and traffic are the most important causes of anthropogenic air pollution. Within the framework of air pollution control planning to date, considerable successes have been achieved for almost all air pollutants, in particular for particulate matter, which was still critical at the beginning of the 2000s. To protect human health, the annual limit value of 40 µg/m³ was set for nitrogen dioxide (NO₂) throughout Europe in 2010, and a critical value of 30 µg/m³ NOx is used as the annual mean value to protect vegetation. These limit values are still exceeded over large areas in Cologne.
In order to permanently reduce air pollution, the Cologne district government drew up a clean air plan for the first time in 2006 in accordance with Section 47 (1) of the Federal Immission Control Act (BImSchG). The purpose of such an air pollution control plan is to describe the situation in which air pollution levels are exceeded, to analyze the causes, to consider the probable development of the pollution situation, and to develop measures that should lead to a reduction in air pollutants. On January 1, 2008, the first environmental zone in North Rhine-Westphalia was therefore established in Cologne, covering the inner area of the city. Since compliance with the limit values for nitrogen dioxide could not yet be achieved as a result, the clean air plan was updated and the environmental zone was extended to almost the entire city area on April 1, 2012. Following a gradual introduction, only vehicles with a green sticker have been allowed to enter the low emission zone since July 1, 2014.
As the applicable limit value for nitrogen dioxide was still exceeded at nine measuring stations in Cologne in 2016, the district government had to update the current clean air plan for the Cologne urban area. Overall, at all measuring points affected by limit value exceedance, the emission share of road traffic has the highest share in the existing pollution situation. A large proportion of this results from nitrogen dioxide emissions from diesel vehicles. The annual mean limit value for particulate matter has been complied with at all measuring points in Cologne since 2009. The location of the areas where elevated levels of pollution occur covers a larger area around the city center and individual areas in the outer parts of the city. The five largest problem areas are the Clevischer Ring (Cologne-Mülheim), Justinianstrasse (Deutz), Neumarkt (City), along Aachener Strasse (Weiden) and Luxemburger Strasse (Sülz). In this respect, there is a need for action to further reduce air pollution in the planning area.
Since mid-August 2019, trucks over 7.5 tons have been banned from passing through Cologne's city center as part of the clean air plan. Delivery traffic and residents are not affected by the ban. The city of Cologne participates in the annual "Earth Hour" organized by the World Wide Fund For Nature (WWF) since 2007.
Geology
→ Main article: Geology of the Lower Rhine Bight
Cologne is located on the southern edge of the Lower Rhine Bay for the most part in the area of the low terraces, which rise slightly from the Rhine like terraces. The geological substructure in the city area is formed by deposits of the glacial period (Quaternary) up to 35 meters thick. They consist of gravels and sands of the Rhine-Meuse system. The foothills of the Rhenish lignite mining area extend as far as Kalk: The lignite mine Gewerkschaft Neu-Deutz was founded there around 1860. Today, the site is home to the brewery of the Sünner brothers, which was able to use the groundwater seeping into the adit. Tertiary and Devonian strata follow in the deeper subsoil.
The soil composition is characterized by the fertile soils of the alluvial plain along the Rhine. In the western parts of the city, they are covered by loess, which has weathered into productive loamy soils used for agriculture (parabraunerden). They are often associated with fertile colluvia, which developed in depressions from washed away soil material. At the end of the last ice age, the Rhine deposited sandy to loamy sediments in the Rhine plain to the east, which is divided by silted-up oxbow lakes. From this, productive parabraunerden and braunerden were formed, which are also used for agriculture. In the Rhine floodplain, fertile brown alluvial soils were formed by periodic flooding of alluvial soil material. The extreme east of the urban area already belongs to the base of the Rhenish slate mountains. Here, geologically older terrace sands and drift sands are widespread, from which mostly poorer brown soils, acidic podsol brown soils and, in the case of dense subsoil, waterlogged pseudogleyes developed. These rather inferior soils are used as heaths and forestry, respectively. Along streams and in gullies, as in the Rhine floodplain, groundwater-influenced gleye formed.
Tectonic movements of the Rhine Graben fault created pronounced terrain ridges around Cologne, such as the Ville near Frechen. Immediately to the west is Germany's most active earthquake zone, whose epicenter is in the Düren district. For earthquake prevention, the Department of Earthquake Geology at the University of Cologne installed a measuring network with 19 "Strong Motion Stations" between Aachen, Bensberg, Meckenheim and Viersen in 2006 and expanded it to 24 stations by 2018. Microearthquakes that are not perceptible occur several times a month in the Cologne Bay area.
Cologne and the Rhine
The Rhine, known as the Lower Rhine after it emerges from the slate mountains south of Cologne, reaches the city at Godorf and leaves it at Worringen. The gradient of the river is about 0.2 per mille. Its current water level can be read from the clock at the Cologne gauge. Normally, this shows 3.48 meters, which stands for a water depth in the navigation channel of about 4.48 meters.
Cologne was affected by floods on several occasions. The worst recorded flood occurred in February 1784, when a temperature surge set in after the extremely long and cold winter of 1783/84. The Rhine was frozen solid and the melting snow and breaking ice caused a record level of 13.55 meters. The floods, on which heavy ice floes floated, devastated large parts of the riverbank development and all the ships. The floes destroyed individual buildings, including fortifications; there were 65 deaths. The flood of water and ice completely destroyed the Bergisch district town of Mülheim am Rhein on the right bank of the Rhine, now a district of Cologne.
In the 20th century, the three floods of the century in 1926, 1993 and 1995 reached levels of up to 10.69 meters. Since 2005, a flood protection concept has been implemented that uses fixed or mobile walls to protect the city up to a level of 11.90 meters. On several occasions, the Rhine was at low water. On September 20, 2003, at 8 a.m., the Rhine reached 0.8 meters at the Cologne gauge. This was below the lowest recorded value from 1947. However, this negative record was broken in October 2018. First, the record level was reached on October 18. On October 23, the water level was only 0.67 meters. However, the 0 meter level means that the 150 meter wide navigation channel in the middle of the river still has one meter of water depth. Inland navigation had to accept restrictions and was not completely stopped, as on the Elbe.
The following list shows the water volumes that move through the city depending on the water level: 0.80 m (lowest water level): 630 cubic meters/second; 3.48 m (normal water level): 2000 m³/s; 6.20 m (high water mark I): 4.700 m³/s; 8.30 m (high water mark II): 7200 m³/s; 10.0 m (high water mark in Altstadt, Rodenkirchen and Zündorf): 9700 m³/s; 10.69 m (high water in January 1995): 11,500 m³/s.
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Panorama of the Old Town embankment. In the center Groß St. Martin, on the right Kölner Philharmonie and Museum Ludwig, on the very outside Hohenzollernbrücke with entrance to Kölner Hauptbahnhof, July 2006.
Neighboring communities
Cologne is the center of a metropolitan area comprising about two million inhabitants. In a closed settlement area, the following cities border directly on the city area in a clockwise direction, starting in the northeast: Leverkusen (independent city), Bergisch Gladbach and Rösrath (Rheinisch-BergischerKreis), Troisdorf and Niederkassel (Rhein-Sieg-Kreis), Wesseling, Brühl, Hürth, Frechen and Pulheim (all Rhein-Erft-Kreis), Dormagen (Rhein-Kreis Neuss) and Monheim (Kreis Mettmann).
The town of Wesseling had been incorporated into Cologne on January 1, 1975, but regained its independence on July 1, 1976, following a court decision.
City breakdown
See also: List of Cologne's boroughs and districts
The city of Cologne is divided into 86 districts, which are grouped into 9 boroughs. The city of Cologne numbers the boroughs from 1-9 and the districts from 101-105, 201-213, 301-309, 401-406, 501-507, 601-612, 701-716, 801-809 and from 901-909, where the hundreds digit corresponds to the number of the borough. However, the district number has nothing to do with the postal code.
Within the districts, the people of Cologne still distinguish between different "Veedeln" (Kölsch for neighborhoods), whose residents often maintain social ties and contacts reminiscent of village communities. However, the boundaries and designations of the Veedel vary, sometimes considerably, depending on how the residents view them. The Office for Urban Development and Statistics has defined 371 neighborhoods - strictly speaking, parts of neighborhoods including the neighborhoods themselves - for statistical evaluations, which include residential places with few inhabitants and settlements as well as commercial areas.
| Cologne city division |
| No. | Municipality | Coat of arms | Residents Dec. 31, 2019 with primary or secondary residence. | Surface area km² | Inhabitants per km² | Districts |
| 1 | Downtown | - – | 129.055 | 16,37 | 7.884 | Old Town South, New Town South, Old Town North, New Town North, Deutz |
| 2 | Rodenkirchen | | 111.040 | 54,55 | 2.035 | Bayenthal, Marienburg, Raderberg, Raderthal, Zollstock, Rondorf, Hahnwald, Rodenkirchen, Weiß, Sürth, Godorf, Immendorf, Meschenich |
| 3 | Lindenthal | - – | 153.600 | 41,80 | 3.675 | Klettenberg, Sülz, Lindenthal, Braunsfeld, Müngersdorf, Junkersdorf, Weiden, Lövenich, Widdersdorf |
| 4 | Ehrenfeld | | 109.770 | 23,98 | 4.578 | Ehrenfeld, Neuehrenfeld, Bickendorf, Vogelsang, Bocklemünd/Mengenich, Ossendorf |
| 5 | Nippes | - – | 118.577 | 31,75 | 3.735 | Nippes, Mauenheim, Riehl, Niehl, Weidenpesch, Longerich, Bilderstöckchen |
| 6 | Chorweiler | - – | 82.732 | 67,16 | 1.232 | Merkenich, Fühlingen, Seeberg, Heimersdorf, Lindweiler, Pesch, Esch/Auweiler, Volkhoven/Weiler, Chorweiler, Blumenberg, Roggendorf/Thenhoven, Worringen |
| 7 | Porz | | 114.699 | 78,92 | 1.453 | Poll, Westhoven, Ensen, Gremberghoven, Eil, Porz, Urbach, Elsdorf, Grengel, Wahnheide, Wahn, Lind, Libur, Zündorf, Langel, Finkenberg |
| 8 | Lime | | 121.637 | 38,16 | 3.187 | Humboldt/Gremberg, Kalk, Vingst, Höhenberg, Ostheim, Merheim, Brück, Rath/Heumar, Neubrück |
| 9 | Mülheim | | 150.709 | 52,20 | 2.887 | Mülheim, Buchforst, Buchheim, Holweide, Dellbrück, Höhenhaus, Dünnwald, Stammheim, Flittard |
| Total | City of Cologne | | 1.091.819 | 404,9 | 2.697 | |
63 percent of Cologne's inhabitants live on the left bank of the Rhine (as of 2016). Since the historic city center is located on the left bank of the Rhine, the right side of the Rhine is referred to condescendingly in dialect as the "Schäl Sick".
Flora and fauna
Cologne has extensive green spaces, which are designed as parks in the urban area and are mostly managed forests in the outer districts. In addition, there are 22 nature reserves, for example the Worringer Bruch in the extreme north of Cologne on the left bank of the Rhine, a former branch of the Rhine that is now silted up. It provides a home for rare animal and plant species and a characteristic floodplain and forest landscape. On the right bank of the Rhine, there are mainly open forest and heath landscapes, such as the Wahn Heath, the Königsforst nature reserve and the Dünnwald Forest. According to the area survey of 2016, Cologne has 5406 hectares of forest area, which corresponds to 13.3% of the city area.
The fauna has a very high number of cultural followers. In addition to pigeons, mice and rats, which are ubiquitous and often perceived as a nuisance, red foxes have migrated into the urban area in significant numbers. They can now be found in the inner city, where they use allotments and parks as their hunting grounds. As a result of improvements in water quality, the Rhine flowing through Cologne has once again become home to many formerly present and newly immigrated species.
Various non-native animals have settled in Cologne's green spaces, favored by the mild climate. Larger populations of collared parakeets and the Great Alexander Parakeet live, among other places, in the Melaten cemetery and the grounds of the Riehler Heimstätten. Originally introduced to Germany from Asian mountain regions (India, Afghanistan) for zoo and home keeping, these parrots/parakeets have become established as neozoa. Information about the size of the populations ranges from a few 100 specimens to over 1000.