.x.zm collapses longitude (regridding first if the field isn’t already on a
regular grid), so a (time, lat) field falls into the same non-map, 2-D branch as
a vertical section — a Hovmöller-style contour of latitude against time.
import os
import numpy as np
import xarray as xr
import matplotlib.pyplot as plt
import nc_time_axis # registers the cftime axis converter for matplotlib
import x4c
x4c.set_style('journal')
# after set_style: it resets rcParams from matplotlibrc defaults, which includes the
# backend, so assert the inline backend last or figures are never captured
%matplotlib inline
# The tutorial runs against a reduced copy of a real CESM case. It is published as a
# GitHub Release asset rather than committed, so the first call downloads it into
# ~/.cache/x4c (override with $X4C_CACHE_DIR) and later calls reuse it. Set
# $X4C_SAMPLE_DIR to point at a copy you already have.
case_dir = x4c.fetch_sample_data(case='cesm1', verbose=False)
casename = os.path.basename(case_dir)
print('x4c', x4c.__version__)x4c 2026.6.11
ts_path = os.path.join(
case_dir, 'atm', 'proc', 'tseries', 'month_1',
f'{casename}.cam.h0.TS.000101-000512.nc',
)
ds = x4c.open_dataset(ts_path, comp='atm', grid='ne16np4', vn='TS', shift_time=True)ts_ann = ds.x.da.x.annualize()
ts_zm = ts_ann.x.zm
print(dict(ts_zm.sizes))
fig, ax = ts_zm.x.plot(title='Zonal-mean surface temperature')
x4c.showfig(fig){'time': 5, 'lat': 180}
