Arazi Örtüsü ile Kentsel Isı Adası Etkisi Arasındaki İlişki: Ordu Kent Merkezi (Türkiye) Örneği

Yıl 2025, Cilt: 15 Sayı: 1, 35 - 55, 30.06.2025

Mesut Güzel , Pervin Yeşil

https://doi.org/10.54370/ordubtd.1580231

Öz

Bu çalışmada, üç temel arazi örtüsü tipi ile Arazi Yüzey Sıcaklığı (AYS) ve Kentsel Isı Adası (KIA) etkisi arasındaki ilişkinin ortaya konulması amaçlanmıştır. Bu amaç doğrultusunda; AYS’nin hesaplanmasında Landsat 8 OLI/TIRS görüntüleri ve arazi örtüsünün sınıflandırılmasında denetimsiz sınıflandırma algoritmaları kullanılmıştır. Elde edilen bulgular istatistiksel yöntemler kullanılarak incelenmiştir. Çalışmanın sonuçları, Karadeniz kıyı kentlerinden biri olan Ordu’da KIA etkisinin ve AYS’nin mekânsal dağılımının arazi örtüsünün tipine göre değiştiğini göstermiştir. AYS ortalaması, yapılaşmış alanlarda bitki örtüsü ile kaplı alanlara göre ortalama 3 °C ve su yüzeylerine göre 8.3 °C daha yüksektir. Kent merkezindeki KIA ve KIA olmayan alanlar arasında ise 4.7 °C’lik sıcaklık farkı bulunmaktadır. Sonuç olarak; KIA etkisinin mekânsal örüntüsü ortaya konulmuş ve Ordu kent merkezi ölçeğinde, iklim değişikliğinin zararlı etkilerine karşı etkili stratejilerin geliştirilmesi noktasında karar vericilere referans sağlanmıştır.

Anahtar Kelimeler

arazi yüzey sıcaklığı , alan kullanımı/arazi örtüsü , kentsel ısı adası etkisi , uzaktan algılama , Landsat 8

Etik Beyan

Bu makalenin yayınlanmasıyla ilgili herhangi bir etik sorun bulunmamaktadır.

Relationship Between Land Cover and Urban Heat Island Effect: The Case of Ordu City Center (Türkiye)

Öz

This study aims to reveal the relationship between three land cover types and Land Surface Temperature (LST) and Urban Heat Island (UHI) effects. For this purpose, Landsat 8 OLI/TIRS images were used in calculating LST, and unsupervised classification algorithms were used in classifying land cover. The findings were examined using statistical methods. The results of the study showed that the spatial distribution of LST and UHI in Ordu, one of the Black Sea coastal cities, varies according to the type of land cover. The mean LST is 3 °C higher in built-up areas than in vegetated areas and 8.3 °C higher than in water bodies. There is a temperature difference of 4.7 °C between UHI and non-UHI areas in the city center. As a result, the spatial pattern of the UHI effect was revealed, and a reference was provided to decision makers in terms of developing effective strategies against the detrimental effects of global climate change at the Ordu city center.

Anahtar Kelimeler

land surface temperature , land use/land cover , urban heat island effect , remote sensing , landsat 8

Kaynakça

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