qin8·advanced

Where is methane rising from paddies, livestock, and landfills near me?

atmospheregreenhouse-gasesagriculture Datasets: 4 15–30 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: 80, 25 → 86, 28 (Gangetic plain (UP–Bihar))
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Where is methane rising from paddies, livestock, and landfills near me?

What you can answer

  • Regional XCH4 enhancement (column minus background) for any AOI from TROPOMI
  • Persistent methane hotspots by compositing daily overpasses over weeks–months
  • Paddy vs steady-source seasonality by comparing monsoon-flood vs dry-season windows
  • Facility-scale plumes (landfills, large point sources) from EMIT 60 m imaging
  • Multi-year drift using the GOSAT long record (2009+) for context

What you can NOT answer with these alone

  • Surface emission flux in tonnes/yr — TROPOMI is a column, not a flux; conversion needs an inversion model with meteorology.
  • Source separation within a pixel — at ~5.5 km, paddy + livestock + urban + landfill mix; needs EMIT/airborne or inventories to disaggregate.
  • Cloudy / low-albedo days — retrievals drop out under cloud, haze and over dark/wet surfaces; flooded paddies themselves can lower retrieval quality.
  • Cause vs accumulation — a high column under stagnant air may be trapped methane, not a local source, without transport analysis.

Code template

import earthaccess
import xarray as xr
import numpy as np

earthaccess.login(strategy="netrc")

# AOI: Gangetic plain (UP–Bihar)
aoi = (80, 25, 86, 28)

# Monsoon window (paddy flooding) vs dry window (steady sources)
windows = {
    "monsoon": ("2024-07-01", "2024-09-30"),
    "dry":     ("2025-01-01", "2025-03-31"),
}

xch4_comp = {}
for label, (start, end) in windows.items():
    granules = earthaccess.search_data(
        short_name="S5P_L2__CH4___",     # TROPOMI L2 CH4, ~5.5 km
        bounding_box=aoi,
        temporal=(start, end),
    )
    # Open methane_mixing_ratio_bias_corrected + qa_value from each granule
    # ds = xr.open_mfdataset(...) for the PRODUCT group

    # Keep only good retrievals (recommended qa_value > 0.5)
    # ds = ds.where(ds.qa_value > 0.5)

    # Regrid scattered L2 pixels onto a regular grid (e.g. ~0.05°),
    # then composite (median) over the window
    # grid = regrid_and_median(ds.methane_mixing_ratio_bias_corrected)

    # Background = low percentile over the AOI (clean-air reference)
    # bg = np.nanpercentile(grid, 10)
    # enhancement = grid - bg   # ppb above background
    xch4_comp[label] = "<gridded enhancement>"

# Seasonality discriminator:
#   paddy signal  ~ (monsoon enhancement) - (dry enhancement)  > 0
#   steady source ~ enhancement present in BOTH windows
# For facility-scale plumes, drop in EMIT scenes (EMITL2BCH4ENH /
# EMITL2BCH4PLM) over flagged landfill locations and inspect 60 m plumes.

Expected output

  • XCH4 enhancement map (ppb above regional background) per season window
  • Persistent-hotspot composite (pixels enhanced across the whole window)
  • Monsoon-minus-dry difference map highlighting paddy-driven seasonality
  • EMIT plume insets at landfill / point-source locations (60 m)
  • Optional overlay of a bottom-up inventory (EDGAR) for sanity-checking

Caveats

  • Column, not flux: high XCH4 can mean trapped air under stagnant meteorology, not local emission. Pair with winds before naming a source.
  • Retrieval artefacts: albedo, aerosol and cloud bias XCH4 — always apply the qa_value filter (recommended > 0.5) and be wary over bright deserts, dark water and haze.
  • Coarse pixels mix sources: at ~5.5 km, paddy, livestock and landfill emissions blend; treat TROPOMI as regional, and use EMIT/airborne to attribute facility plumes.
  • Paddy retrievals are tricky: standing water lowers surface reflectance and can degrade retrieval quality exactly where paddy methane peaks — check pixel counts per window.
  • EMIT is opportunistic: 60 m plume detection has limited, scheduled coverage and detects strong point sources, not diffuse area emissions like flooded fields.
  • Verify before attribution: confirm hotspots against inventories (EDGAR), repeat overpasses, or airborne campaigns; don’t assign a single source from one coarse scene.

Cross-DAAC composition

TROPOMI/Sentinel-5P CH4 is distributed by GES DISC. EMIT plume/enhancement products (EMITL2BCH4ENH / EMITL2BCH4PLM) come from LP DAAC — a separate DAAC, so facility-scale analysis spans two auth contexts under the common Earthdata login.

Sources

How a scientist answers this
Parameters
Column-averaged dry-air methane mole fraction (XCH4) from TROPOMI / Sentinel-5P (~5.5 km, daily, near-global) for regional enhancements, with GOSAT XCH4 for the long record (2009+). For facility-scale plumes (e.g. landfills) the EMIT imaging spectrometer (60 m) and point-source plume products resolve individual sources. The answer is the XCH4 enhancement — column minus a regional background — mapped and composited to find persistent hotspots.
Method
Subtract a regional background (clean-air percentile or upwind reference) from XCH4 to get the enhancement, then composite over time to reveal persistent hotspots versus transient transport. Attribute hotspots to source type using context: flooded-paddy seasonality (enhancement tracks the monsoon transplanting/flooding cycle), livestock density (steady, co-located with herds), and landfill point plumes (sharp, localised — resolved by EMIT). Seasonality is the key discriminator: paddy emissions pulse with monsoon flooding while livestock and landfill sources stay roughly steady year-round.
Validation
TROPOMI measures a *column*, not a surface flux — high XCH4 can reflect accumulation under stagnant meteorology rather than local emission, so pair with wind/transport before claiming a source. Retrievals carry albedo, aerosol and cloud artefacts (bright/dark surfaces and haze bias XCH4); apply the quality assurance (qa_value) filter and treat low-qa pixels with caution. Coarse ~5.5 km pixels mix paddy, livestock and urban/landfill sources, so use EMIT/airborne plume imaging or bottom-up inventories (e.g. EDGAR) to confirm and disaggregate.
In plain EnglishSatellites measure how much methane is in the air column over your region. Subtract the normal background and the leftover bump shows where extra methane is coming from. Paddies pulse with the monsoon flooding season, cows and landfills leak steadily, and a fine-resolution instrument (EMIT) can pin down individual dump-site plumes.

Make it yours → Choose your region and season, set the background reference, and the notebook maps the XCH4 enhancement and composites persistent hotspots. Toggle the monsoon vs dry-season window to separate paddy pulses from steady livestock/landfill sources, and drop in EMIT plume scenes to zoom to facility scale.

Run the core method · no login

The detection / counting above a threshold 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