Thornthwaite climate classification indices are essential to interpret climate types in Bartin City, simplifying calculation process and interpretation of climatological water balance by forests. Thus, we aimed to develop a climatological water balance by the Thornthwaite method, as well as climatic characterization using the indices proposed by Thornthwaite for Bartin (including measurement points are Amasra, Arit, Hasankadi, Kozcagiz, Kurucasile, Ulus, Ulus Cubukeli, Ulus Ceyupler Koyu). We used historical series of climate data from all 15 metrological stations of Bartin between 1988 and 2019, which were divided into measurements regions. Air temperature and precipitation were collected on a daily scale. Precipitation and potential evapotranspiration data allowed calculating water balance by the Thornthwaite method. We characterized all locations as wet and dry using aridity indices proposed by Thornthwaite. Maps were generated from climate indices of Bartin using kriging interpolation method with spherical model, one neighbor, and 0.25° resolution. The measurement regions showed different patterns regarding water balance components and humidity index. Humidity index had a mean of 16.97. The prevailing climate in Bartin is moist subhumid. Bartin has two well-defined periods during the year: a dry and a rainy period. Three climate types predominate in Bartin and, according to the Thornthwaite classification, are humid, moist subhumid, and dry subhumid. Water characterization in Bartin showed 123.67 mm year −1 of water surplus, 79.7 mm year −1 of water deficit, and 1003.9 mm year −1 of potential evapotranspiration. Water deficit and potential evapotranspiration decrease as latitude increases.

中文翻译：

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巴丁城市和林区聚落区与气候条件决策的整合管理

Thornthwaite 气候分类指数对于解释 Bartin 市的气候类型、简化计算过程和森林对气候水平衡的解释至关重要。因此，我们旨在通过 Thornthwaite 方法开发气候水平衡，以及使用 Thornthwaite 为 Bartin 提出的指数（包括测量点为 Amasra、Arit、Hasankadi、Kozcagiz、Kurucasile、Ulus、Ulus Cubukeli、Ulus Ceyupler）进行气候表征小鱼）。我们使用了 1988 年至 2019 年间 Bartin 所有 15 个计量站的历史气候数据系列，这些数据被划分为测量区域。每天收集气温和降水。降水和潜在蒸散数据允许通过 Thornthwaite 方法计算水平衡。我们使用 Thornthwaite 提出的干旱指数将所有地点描述为干湿两用。地图是根据 Bartin 的气候指数生成的，使用克里金插值法和球形模型、一个邻居和 0.25° 分辨率。测量区域在水平衡成分和湿度指数方面表现出不同的模式。湿度指数的平均值为 16.97。Bartin 的主要气候是潮湿半湿润的。Bartin 在一年中有两个明确定义的时期：旱季和雨季。三种气候类型在 Bartin 占主导地位，根据 Thornthwaite 分类，潮湿、半湿润和干燥半湿润。Bartin 的水特征表明，123.67 毫米年 -1 年的水盈余，79.7 毫米年 -1 年的缺水，以及 1003.9 毫米年 -1 年的潜在蒸散量。