REMO B1 SCENARIO RUN, UBA PROJECT, DATASTREAM 3

The regional climate model REMO has been used to simulate future climate of Germany for different climate scenarios (IPCC).
The simulations have been initiated by Umweltbundesamt (P. Mahrenholz) and performed by Max-Planck-Institute for Meteorology (D. Jacob).
The use of the data is possible after acceptance of the user conditions. A special user contract has to be signed, contact [e-mail] for further details.
The experiment REMO_UBA_B1_D3 starts 2001 and calculates in 0.088 degree horizontal resolution the future climate of the IPCC scenario B1 from 2001 to 2100.
For initialization and as boundary condition the coarse REMO IPCC consortial run (REMO_IPCC044_B1_1_R001502) in 0.44 degree horizontal resolution is used.
In the possible future climate scenario B1 a change in economic structures towards a service and information economy is assumed with introduction of clean and resource efficient technologies. The development of global population is assumed to peak in mid-century like in scenario A1B.
Data stream 3 (D3) denotes a part of the regular variables of REMO and additionally derived quantities. Data stream 3 is derotated and interpolated (bilinear interpolation using CDO routines) on a regular geographical grid with 0.1 degree horizontal resolution in netCDF format. For some model variables statistics on daily, monthly and yearly basis are available.
The model domain covers Germany starting at 45.85/3.95 (lat/lon, lower left corner) with an increment of 0.1 degrees. The number of grid points is 92/134 (lat/lon).
After interpolation the cutout of the model domain has been chosen in a way that the river Rhine and Switzerland are lying completely in the model domain. Therefore there exist missing values at the western and southern boundary which are set on -9.x10**33. All surface quantities are not corrected in height. The correction in height is necessary for comparisons with observational data particularly for mountainous terrain.

区域气候模型 REMO 已被应用于模拟德国在未来不同气候情景（IPCC）下的气候。该模拟由联邦环境保护局（Umweltbundesamt，负责人 P. Mahrenholz）发起，并由马克斯·普朗克气象研究所（Max-Planck-Institute for Meteorology，负责人 D. Jacob）执行。用户在使用数据前需接受用户条件，并签署特别用户协议，具体详情请联系 [e-mail]。实验 REMO_UBA_B1_D3 从 2001 年开始，以 0.088 度的水平分辨率计算 IPCC 情景 B1 从 2001 年至 2100 年的未来气候。初始化及边界条件采用粗分辨率 REMO IPCC 联合运行（REMO_IPCC044_B1_1_R001502），其水平分辨率为 0.44 度。在可能的未来气候情景 B1 中，假设经济结构向服务和信息经济转变，并引入清洁和资源高效的技术。全球人口的增长预计在世纪中叶达到峰值，与情景 A1B 类似。数据流 3（D3）表示 REMO 的常规变量及其派生量的一部分。数据流 3 在净CDF格式下，以 0.1 度的水平分辨率进行去倾斜和插值（使用 CDO 程序的双线性插值）。对于某些模型变量，提供每日、每月和每年的统计数据。模型域覆盖德国，从 45.85/3.95（纬/经，左下角）开始，以 0.1 度的增量。网格点数量为 92/134（纬/经）。经过插值后，选择模型域的裁剪部分，使得莱茵河和瑞士完全位于模型域内。因此，在西部和南部的边界存在缺失值，被设置为 -9.x10**33。所有表面量未进行高度校正。高度校正对于与观测数据的比较是必要的，尤其是对于山区地形。