qin2·intermediate

Has the monsoon's arrival date over my region shifted earlier or later?

hydrologyprecipitationagricultureclimate Datasets: 4 15–40 min
Find the data for your area

Draw a rectangle to pick your area of interest, then see what NASA data covers it (live, here in your browser) or download a ready-to-run notebook with your AOI pre-filled. The notebook runs in any Python environment — it needs a free Earthdata Login to fetch the data.

Current AOI: 74, 8 → 78, 13 (Kerala (monsoon onset gateway))
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Has the monsoon’s arrival date over my region shifted earlier or later?

What you can answer

  • Onset day-of-year for each year over your AOI from an explicit, reproducible rainfall rule
  • Multi-year trend in the onset date (Theil–Sen slope) and whether it’s significant (Mann–Kendall)
  • Sensitivity of onset to the threshold and consecutive-day definition
  • Circulation confirmation — whether monsoon westerlies / moisture flux (ERA5) accompany the rainfall jump
  • Year-to-year variability and the spread of onset dates around the mean

What you can NOT answer with these alone

  • The official IMD onset date — IMD uses station networks, winds and OLR criteria; satellite-only onset is an estimate, not a declaration.
  • Long pre-2000 trends — IMERG begins in 2000; for multi-decadal records use gauge products (IMD gridded) or reanalysis, each with their own caveats.
  • Withdrawal / break-monsoon timing without a separate rule.
  • Causal attribution (why onset shifted) — requires climate-model and large-scale-driver analysis beyond these products.

Code template

import earthaccess
import xarray as xr
import numpy as np

earthaccess.login(strategy="netrc")

# AOI: Kerala (monsoon onset gateway)
aoi = (74, 8, 78, 13)
years = range(2001, 2025)

# --- Onset rule (IMD-style family — SET AND VERIFY for your region) ---
# Onset = first day on/after an earliest date where area-mean rainfall
# stays above a threshold for N consecutive days. Thresholds vary by
# definition; tune and report a couple of choices for robustness.
EARLIEST = "05-10"      # earliest permitted onset (mm-dd)
RAIN_MM  = 5.0          # daily area-mean rainfall threshold (mm/day) — verify
CONSEC   = 5            # consecutive wet days required — verify

def onset_doy(da_daily):
    """da_daily: 1-D xarray of area-mean daily rainfall for one year."""
    wet = da_daily >= RAIN_MM
    roll = wet.rolling(time=CONSEC).sum()  # count wet days in window
    hit = roll.where(roll == CONSEC, drop=True)
    return int(hit.time.dt.dayofyear[0]) if hit.size else np.nan

onsets = []
for yr in years:
    g = earthaccess.search_data(short_name="GPM_3IMERGDF",
                                bounding_box=aoi,
                                temporal=(f"{yr}-{EARLIEST}", f"{yr}-07-15"))
    # open -> area-weighted daily mean of 'precipitation' -> onset_doy()
    # optionally gate on ERA5 850 hPa westerlies / moisture flux here
    onsets.append(onset_doy(...))  # fill with computed series

# Trend: Theil–Sen slope + Mann–Kendall significance
import scipy.stats as ss
yrs = np.array(list(years)); od = np.array(onsets, float)
mask = ~np.isnan(od)
slope = ss.theilslopes(od[mask], yrs[mask])[0]   # days per year
tau, p = ss.kendalltau(yrs[mask], od[mask])      # MK-style monotonic test
print(f"trend = {slope*10:.2f} days/decade, p = {p:.3f}")

Expected output

  • Series: onset day-of-year per year (2001–present), with the mean and ±1σ band
  • Trend line: Theil–Sen slope in days/decade, annotated with Mann–Kendall p-value
  • Sensitivity panel: onset dates under 2–3 threshold/consecutive-day definitions
  • Optional: ERA5 850 hPa wind / moisture-flux composite around detected onset to confirm circulation
  • Comparison markers: IMD official onset dates overlaid where available

Caveats

  • Threshold sensitivity — onset can swing by many days with small changes to the rainfall threshold or consecutive-day count; always report the rule and test alternatives.
  • Satellite rainfall bias — IMERG underestimates orographic rain over the Western Ghats and is uncertain for extremes; onset timing inherits this.
  • Short record — ~25 years of IMERG limits statistical power; a slope can look like a shift yet have p > 0.05. Report the confidence interval.
  • Bogus onset — strong pre-monsoon showers can trip a rainfall-only rule; gating on established westerlies/moisture (ERA5) reduces false onsets.
  • IMERG latency / version — Final has ~3.5-month latency; use V07 and reprocess older cached granules.

Cross-DAAC composition

GES DISC (GPM IMERG, MERRA-2) + Copernicus/C3S (ERA5) — single DAAC if you stay on IMERG + MERRA-2; add a second auth only if pulling ERA5 from Copernicus.

Sources

How a scientist answers this
Parameters
Daily precipitation from GPM IMERG (2000–present, ~10 km) over your region, plus low-level winds and moisture flux from ERA5 (or MERRA-2) to confirm the large-scale monsoon circulation, not just a stray pre-monsoon shower. The output is one onset day-of-year per year and the multi-year trend in that date.
Method
Build an area-averaged daily rainfall series each year, then apply a sustained-rainfall onset rule of the IMD-style family — rainfall exceeding a threshold over several consecutive days after an earliest-permitted date, optionally requiring the monsoon westerlies/moisture flux to be established. Record the onset day-of-year per year, then fit a Theil–Sen slope and test significance with Mann–Kendall. Exact thresholds vary by definition and region — set them explicitly and verify against the local convention rather than treating one number as canonical.
Validation
Compare your detected onset dates against IMD's official onset declarations (especially the Kerala onset), which use station rainfall, winds and outgoing longwave radiation — satellite-only onset can differ by days. Satellite rainfall is biased (orographic underestimation over the Western Ghats; extremes), and the onset date is sensitive to the threshold and consecutive-day rule, so report results for a couple of definitions to show robustness. With ~25 years of IMERG, modest trends may not be statistically significant — state the p-value and confidence interval.
In plain EnglishEach year we find the first day the steady monsoon rains really kick in over your region, write down that date, and line up 20+ years of those dates to see if the start is drifting earlier or later. Because the 'start' depends on exactly how you define it, we report the trend cautiously and check it against the official onset.

Make it yours → Pick your region, the rainfall threshold and number of consecutive wet days that define 'onset', and the earliest date the clock can start. Choose whether to also require monsoon winds/moisture (ERA5) to be established, and the years to trend over; the notebook returns onset day-of-year per year plus the Theil–Sen + Mann–Kendall trend.

Run the core method · no login

The robust trend (Theil–Sen + Mann–Kendall) at the heart of this question — runnable on synthetic data, right here. The full earthaccess code template further down does it on real NASA data (needs an Earthdata login).

editable · runs in your browser

Datasets used