Datasets:
question_id stringlengths 1 3 | modality stringclasses 3
values | question stringlengths 73 1.13k | reference_answer stringclasses 5
values | choices listlengths 4 6 β |
|---|---|---|---|---|
1 | Spectrum | Calculate TVDI based on temperature and vegetation data (NDVI and LST) and analyze the annual trend | B | [
"Increasing dryness at 0.015 per year",
"Decreasing dryness at 0.019 per year",
"Decreasing dryness at 0.006 per year",
"No significant trend observed"
] |
2 | Spectrum | Calculate TVDI for the Sichuan Plain agricultural area and analyze the percentage of areas where TVDI exceeds 0.75 | C | [
"12.87%",
"22.40%",
"28.07%",
"36.56%"
] |
3 | Spectrum | Based on temperature and vegetation indicators (NDVI and LST) in the Yellow River Basin from June to September 2023, calculate the Temperature-Vegetation Dryness Index (TVDI) for each time point, and identify and count the number of spikes in the drought index. | B | [
1,
2,
5,
6
] |
4 | Spectrum | Using temperature and vegetation data (NDVI and LST) on August 13, 2022, calculate the spatial distribution of the Temperature-Vegetation Dryness Index (TVDI) in the urban area of Chengdu and its surroundings, and compute the percentage of pixels with TVDI values greater than 0.75 to identify potential urban drought ho... | A | [
"14.98%",
"22.76%",
"30.45%",
"38.79%"
] |
5 | Spectrum | Based on temperature and vegetation indices (NDVI and LST) in the Central Valley of California, U.S., from May to October 2021, first list the input TIFF files, then calculate the Temperature-Vegetation Dryness Index (TVDI) for each date, compute the proportion of pixels with TVDI values exceeding 0.7 for each image, a... | C | [
"The proportion of pixels with TVDI values exceeding 0.7 surpassed 40% occurred 10 times",
"The proportion of pixels with TVDI values exceeding 0.7 surpassed 40% occurred 8 times",
"The proportion of pixels with TVDI values exceeding 0.7 surpassed 40% occurred 4 times",
"The proportion of pixels with TVDI val... |
6 | Spectrum | Based on Landsat 8 thermal band 10 and reflectance bands (Red and NIR) data over New York City from 2018 to 2022, first list the input TIFF files, then calculate NDVI and use the single-channel NDVI-based method to estimate land surface temperature (LST). Compute the mean LST for each image, derive the annual average L... | D | [
"-1.35 K/year",
"+0.50 K/year",
"-0.50 K/year",
"+0.63 K/year"
] |
7 | Spectrum | Using Landsat 8 TOA data (Band 10) in Death Valley National Park during the 2021 heatwave season (JuneβSeptember), first list the input TIFF files, then calculate NDVI and estimate land surface temperature (LST) using the single-channel method. For each image, compute the proportion of pixels with LST values exceeding ... | A | [
"5 days",
"10 days",
"12 days",
"18 days"
] |
8 | Spectrum | Based on brightness temperature and reflectance data from Landsat 8 Band 10, Band 4, and Band 5 on August 11, 2021, in the Okavango Delta, first list the input TIFF files, then calculate NDVI and estimate land surface temperature (LST) using the single-channel method. Finally, compute the proportion of the area where L... | B | [
"28.62%",
"40.32%",
"53.76%",
"66.59%"
] |
9 | Spectrum | Based on Landsat 8 Band 10 (brightness temperature) data from January to December 2021 in the Chicago metropolitan area, first list the input TIFF files, then calculate NDVI and estimate land surface temperature (LST) using the single-channel method. For each image, compute the proportion of pixels with LST values abov... | A | [
"7 days",
"12 days",
"15 days",
"18 days"
] |
10 | Spectrum | Based on brightness temperature and reflectance values from Landsat 8 Band 10, Band 4, and Band 5 over the Black Forest region in Germany on July 29, 2021, first list the input TIFF files, then calculate NDVI and estimate land surface temperature (LST) using the single-channel method. Next, compute the average LST with... | D | [
"2.3 K higher",
"4.8 K higher",
"6.7 K higher",
"8.9 K higher"
] |
11 | Spectrum | Based on thermal Band 31 and Band 32 data over the Tokyo metropolitan area on August 10, 2022, first list the TIFF files, then estimate land surface temperature (LST) using the split-window method, and finally calculate the proportion of the area where LST exceeds 310K. | C | [
"14.36%",
"27.63%",
"49.74%",
"62.47%"
] |
12 | Spectrum | Based on thermal Band 31 and Band 32 data over the MurrayβDarling Basin in Australia during January 2023, first list the input TIFF files, then estimate land surface temperature (LST) using the split-window method. For each day, calculate the proportion of the area with LST values exceeding 310 K, and finally determine... | D | [
"5 days",
"9 days",
"14 days",
"18 days"
] |
13 | Spectrum | Based on thermal Band 31 and Band 32 data over the Sahara Desert region from 2014 to 2023, first list the input TIFF files, then estimate land surface temperature (LST) using the split-window algorithm. Next, calculate the daily average LST, derive the annual average LST, and finally compute the linear trend of the ann... | C | [
"+0.21 K/year",
"+0.38 K/year",
"-0.28 K/year",
"No significant trend"
] |
14 | Spectrum | Based on thermal Band 31 and Band 32 data over the Sahara Desert region from 2014 to 2023, first list the input TIFF files, then estimate land surface temperature (LST) using the split-window algorithm. Next, calculate the daily average LST, derive the annual average LST, and finally compute the linear trend of the ann... | C | [
"p = 0.023, slope = +1.28 K/year (significant increasing trend)",
"p = 0.015, slope = -1.91 K/year (significant decreasing trend)",
"p = 0.70, slope = -1.45 K/year (non-significant trend)",
"p = 0.46, slope = 0.00 K/year (no trend)"
] |
15 | Spectrum | Based on thermal infrared Band 31 and Band 32 data over the Tibetan Plateau from May 1 to May 15, 2022, determine the date on which the maximum average land surface temperature (LST) occurs. | A | [
"May 1, 304.57 K",
"May 7, 301.92 K",
"May 31, 300.61 K",
"May 5, 298.96 K"
] |
16 | Spectrum | Calculate atmospheric water vapor content in the Turpan region in 2020 based on surface reflectance data from MODIS bands b02 (0.865 ΞΌm), b05 (1.240 ΞΌm), b17 (0.905 ΞΌm), b18 (0.936 ΞΌm), and b19 (0.940 ΞΌm), and analyze drought conditions. | A | [
"4 days",
"17 days",
"20 days",
"26 days"
] |
17 | Spectrum | Using MODIS surface reflectance from bands b02 (0.865 ΞΌm), b05 (1.240 ΞΌm), b17 (0.905 ΞΌm), b18 (0.936 ΞΌm), and b19 (0.940 ΞΌm), first list the input TIFF files, then estimate atmospheric absorption levels over the urban region of Hangzhou on August 10, 2021, using the band ratio method. Calculate the average atmospheric... | D | [
"12.98%",
"40.38%",
"68.56%",
"61.98%"
] |
18 | Spectrum | Using MODIS surface reflectance bands b02, b05, b17, b18, and b19 (corresponding to 0.865 ΞΌm, 1.240 ΞΌm, 0.905 ΞΌm, 0.936 ΞΌm, and 0.940 ΞΌm respectively) over the Loess Plateau from 2018 to 2022, first list the input TIFF files, then apply the band ratio method to estimate daily atmospheric water vapor. Calculate the dail... | A | [
"Increase of 0.171 g/cmΒ² per year",
"Increase of 0.015 g/cmΒ² per year",
"Decrease of 0.151 g/cmΒ² per year",
"No significant trend"
] |
19 | Spectrum | Using MODIS bands b02, b05, b17, b18, and b19 (corresponding to 0.865 ΞΌm, 1.240 ΞΌm, 0.905 ΞΌm, 0.936 ΞΌm, and 0.940 ΞΌm respectively), monitor atmospheric absorption over the coast of Guangdong during the period from July 20 to 29, 2023. | C | [
"79.95 g/cmΒ²",
"73.07 g/cmΒ²",
"84.98 g/cmΒ²",
"91.88 g/cmΒ²"
] |
20 | Spectrum | Based on the daily atmospheric absorption indicator derived from MODIS bands b02, b05, b17, b18, and b19 over the Huang-Huai-Hai Plain during 2023, first list the input TIFF files, then apply the band ratio method to estimate daily atmospheric water vapor. Calculate the average water vapor content for each day, compare... | D | [
3,
6,
10,
13
] |
21 | Spectrum | Process the TIF files in the working directory and calculate the percentage of pixels meeting the conditions. | D | [
"0.15%",
"0.28%",
"0.37%",
"0.19%"
] |
22 | Spectrum | Using TES-derived land surface temperature and emissivity from ASTER Bands 10β14 on June 15, 2022, over the Los Angeles metropolitan area, identify and count pixels where LST exceeds 310 K and emissivity variation (ΞΞ΅) exceeds 0.08, representing thermal hotspots linked to intense urban heating. | B | [
528,
931,
1567,
2148
] |
23 | Spectrum | Based on TES output from ASTER thermal bands on March 30, 2020, in the Sahara Desert region near Tamanrasset, Algeria, calculate the proportion of the area where emissivity variation (ΞΞ΅) exceeds 0.06. | D | [
"7.63%",
"31.45%",
"69.85%",
"100%"
] |
24 | Spectrum | Apply the TES algorithm to ASTER thermal data (Bands 10β14) acquired on March 24, 2020, to estimate land surface temperature. Compute the proportion of valid pixels where LST is greater than 288.5 K. | C | [
"10.00%",
"15.00%",
"26.00%",
"32.00%"
] |
25 | Spectrum | Apply the TES algorithm to ASTER thermal data from June 15, 2022, to estimate LST and emissivity across the Los Angeles metro area. Identify pixels with LST > 300 K and compute the mean emissivity variation (ΞΞ΅) within those high-temperature zones. | B | [
10.78,
20.03,
29.93,
42.21
] |
26 | Spectrum | On December 23, 2022, use LST retrieved via the Three-Temperature Method (TTM) from ASTER Bands 10β12 to calculate the percentage of pixels exceeding 278 K over the specified region (as defined by polygon coordinates), in order to identify potential high fire risk areas under drought conditions. | C | [
"15.49%",
"18.64%",
"24.32%",
"31.65%"
] |
27 | Spectrum | On December 23, 2022, using land surface temperature (LST) derived from the Three-Temperature Method (TTM) applied to ASTER Bands 10β12 (acquired at 10:30 AM local time), calculate the mean LST difference (ΞLST) between two vertically aligned regions that partially overlap in longitude (74.4Β°β75.1Β°E). | A | [
"0.18 K",
"1.04 K",
"1.57 K",
"2.03 K"
] |
28 | Spectrum | Using ASTER bands 10-12 data, calculate the Land Surface Temperature (LST) using the Three-Temperature Method (TTM), and compute the average temperature difference between urban and rural areas to assess the Urban Heat Island effect. | C | [
"13.83 K",
"25.24 K",
"43.74 K",
"38.19 K"
] |
29 | Spectrum | Using ASTER Bands 10β12 data on April 13, 2022, the Three-Temperature Method (TTM) was applied to estimate Land Surface Temperature (LST) in two Australian Outback regions. Calculate the absolute difference in their average LST values. | A | [
"0.64 K",
"1.00 K",
"1.90 K",
"2.50 K"
] |
30 | Spectrum | Based on land surface temperature (LST) retrieved using the Three-Temperature Method (TTM) from ASTER Bands 10β12 on August 1, 2020, over the defined Mediterranean coastal area near Barcelona, calculate the average daytime LST specifically within urban areas. | D | [
"302.57 K",
"305.84 K",
"308.25 K",
"311.21 K"
] |
31 | Spectrum | Calculate the average land surface temperature in the Taklamakan Desert area at 05:50 on February 23, 2020. | C | [
"289.39 K",
"294.65 K",
"301.22 K",
"285.07 K"
] |
32 | Spectrum | Define an extreme temperature event as any day when the surface temperature derived from Band 31 and Band 32 using the split-window algorithm exceeds the overall monthly mean by more than 10%. Based on thermal data for the region surrounding Taklamakan, Xinjiang, from June 3 to June 30, 2021, list the relevant TIFF fil... | C | [
"5 days",
"12 days",
"17 days",
"25 days"
] |
33 | Spectrum | Based on thermal Band 31 and 32 data acquired over irrigated farmland in northern Hebei on August 5, 2021, apply the split-window algorithm to estimate land surface temperature (LST). Classify the resulting temperature map into three thermal zones: low (< 295 K), medium (295β305 K), and high (> 305 K). Finally, calcula... | D | [
"21.39%",
"34.75%",
"47.04%",
"63.17%"
] |
34 | Spectrum | Based on land surface temperature (LST) retrieved using the split-window algorithm from thermal Bands 31 and 32 over the urban area of Guangzhou between 2018 and 2023, calculate the annual average LST for each year. This includes listing the relevant TIFF files, applying the split-window algorithm to derive daily LST, ... | B | [
"2018, 296.46K",
"2019, 297.86K",
"2021, 300.46K",
"2023, 296.93K"
] |
35 | Spectrum | Based on thermal Bands 31 and 32 from the central urban area of Wuhan on July 15, 2022, apply the split-window algorithm to retrieve land surface temperature (LST). Define high-temperature zones as areas where LST exceeds 310 K, then calculate the percentage of high-temperature area. | A | [
"13.23%",
"5.29%",
"33.43%",
"20.77%"
] |
36 | Spectrum | Based on MODIS daytime and nighttime brightness temperature and emissivity data from Band 31 over the North American Great Plains in July 2023, identify extreme heat days as those with daytime land surface temperature (LST) exceeding 315 K. Calculate the percentage of extreme heat days during the month. | A | [
"12.9%",
"21.9%",
"29.3%",
"36.1%"
] |
37 | Spectrum | Using MODIS daytime and nighttime brightness temperature and emissivity data from Band 31 over the Ganges River Basin during January 2021, identify nights when the nighttime land surface temperature (LST) dropped below 305 K. | D | [
10,
16,
19,
27
] |
38 | Spectrum | Using thermal Bands 31 and 32 over the Sahara Desert for June 2020 and June 2021, estimate LST via the split-window algorithm. Compute the monthly average LST for each year and calculate the absolute difference. | C | [
"4.53 K",
"5.88 K",
"8.0 K",
"8.91 K"
] |
39 | Spectrum | Using MODIS daytime brightness temperature and emissivity (Band 31) data over the southern edge of the Sahara during July 2023, calculate the number of days on which more than 30% of the region's pixels recorded daytime land surface temperatures (LST) exceeding 325 K. | D | [
"3 days",
"8 days",
"14 days",
"22 days"
] |
40 | Spectrum | Using MODIS daytime brightness temperature and emissivity (Band 31) data over Central California during July of 2015 and 2023, calculate the change in the percentage of days when more than 40% of the region's pixels exhibited daytime land surface temperatures (LST) exceeding 310 K. | C | [
"Increase of 7.86%",
"Decrease of 4.84%",
"No significant change (<1%)",
"Increase of 3.50%"
] |
41 | Spectrum | Calculate and analyze the Apparent Thermal Inertia (ATI) changes in Cyprus between July 1st and July 15th, 2020. | C | [
"Increase by 0.39",
"Decrease by 0.58",
"Increase by 0.59",
"Decrease by 0.22"
] |
42 | Spectrum | Using Apparent Thermal Inertia (ATI) derived from satellite thermal bands and surface albedo, identify and visualize areas with the lowest ATI values (below 1.0), indicating potential drought stress across the Sahel region in May 2023. Then calculate the proportion of the region affected by these low ATI values. | D | [
"10.47%",
"25.48%",
"40.87%",
"53.39%"
] |
43 | Spectrum | Based on Apparent Thermal Inertia (ATI) data derived from daytime and nighttime brightness temperature and albedo in the agricultural region of California's Central Valley during July 2022, thermal anomalies are defined as areas with ATI values below 1.2. The analysis involves listing the input TIFF files, calculating ... | A | [
"2 days",
"12 days",
"18 days",
"24 days"
] |
44 | Spectrum | Based on Apparent Thermal Inertia (ATI) calculated from daytime and nighttime brightness temperature and surface albedo over the urban area of Beijing, China from June 1 to September 30, 2019, list the input TIFF files, compute ATI for each pixel, analyze the monthly trend of ATI, and identify the month with the larges... | A | [
"June",
"July",
"August",
"September"
] |
45 | Spectrum | Based on Apparent Thermal Inertia (ATI) and daytime/nighttime brightness temperatures over California during the August 2022 wildfire events, the input TIFF files are first listed, followed by the calculation of ATI to estimate surface conditions, and then the percentage of the region with ATI values below 0.4 is ident... | D | [
"9.89%",
"15.66%",
"22.44%",
"55.42%"
] |
46 | Spectrum | Based on temperature and vegetation reflectance data (NDVI and LST) from the agricultural region near Urumqi, Xinjiang in 2019, calculate the daily and annual average of the dryness indicator (TVDI), and describe the overall dryness characteristics for the year. | B | [
"Annual Mean TVDI: 0.7123",
"Annual Mean TVDI: 0.6897",
"Annual Mean TVDI: 0.6543",
"Annual Mean TVDI: 0.7245"
] |
47 | Spectrum | Using MODIS LST and NDVI data over the Chengdu Plain on July 12, 2022, calculate TVDI and determine the mean TVDI value in areas where the LST exceeds 300 K. | A | [
0.6382,
0.6848000000000001,
0.7156,
0.8024
] |
48 | Spectrum | Based on temperature and vegetation indicators (NDVI and LST) in the Yellow River Basin from June to September 2023, calculate the Temperature-Vegetation Dryness Index (TVDI) for each time point, and identify and count the number of spikes in the drought index. | D | [
0.012,
0.023,
0.045,
0.061
] |
49 | Spectrum | Using temperature and vegetation data (NDVI and LST) on August 13, 2022, first list the input TIFF files, then calculate the spatial distribution of the Temperature-Vegetation Dryness Index (TVDI) in the urban area of Chengdu and its surroundings. Finally, classify the pixels into four drought severity levels based on ... | B | [
"No Drought (TVDI < 0.4): 28.92%; Mild Drought (0.4 β€ TVDI < 0.75): 34.56%; Severe Drought (TVDI β₯ 0.75): 11.85%",
"No Drought (TVDI < 0.4): 30.35%; Mild Drought (0.4 β€ TVDI < 0.75): 54.67%; Severe Drought (TVDI β₯ 0.75): 14.98%",
"No Drought (TVDI < 0.4): 25.45%; Mild Drought (0.4 β€ TVDI < 0.75): 42.33%; Severe... |
50 | Spectrum | Based on NDVI and LST data from June and August 2021 in the Central Valley of California, U.S., first list all the input TIFF files for these two months. Then, calculate the daily Temperature-Vegetation Dryness Index (TVDI) images. For each daily TVDI image, compute the proportion of pixels where TVDI exceeds 0.7. Next... | A | [
"8.11%",
"12.45%",
"6.23%",
"15.78%"
] |
51 | Spectrum | Using Landsat 8 thermal and reflectance data in 2022 over New York City, estimate LST based on NDVI and thermal band 10 using the single-channel method, then calculate the average LST for summer and autumn, and determine the mean difference to assess seasonal temperature variation between these two periods. | C | [
"8.65K",
"10.89K",
"12.42K",
"14.75K"
] |
52 | Spectrum | Using Landsat 8 TOA data (Band 10) in Death Valley National Park during June 2021, first list the input TIFF files, then calculate NDVI and estimate land surface temperature (LST) using the single-channel method. For each image, compute the proportion of pixels with LST values exceeding 315 K, and finally calculate the... | D | [
"12.34%",
"25.67%",
"36.89%",
"43.47%"
] |
53 | Spectrum | Based on brightness temperature and reflectance data from Landsat 8 Band 10, Band 4, and Band 5 on August 11, 2021, in the Okavango Delta, first list the input TIFF files, then calculate NDVI and estimate land surface temperature (LST) using the single-channel method. Finally, compute the proportion of the area where L... | C | [
"2.15%",
"12.87%",
"6.34%",
"18.42%"
] |
54 | Spectrum | Based on Landsat 8 Band 10 (brightness temperature) data from June to August 2021 in the Chicago metropolitan area, first list the input TIFF files, then calculate NDVI and estimate land surface temperature (LST) using the single-channel method. For each image, calculate the proportion of pixels with LST greater than 3... | B | [
"2 days",
"3 days",
"4 days",
"5 days"
] |
55 | Spectrum | Based on brightness temperature and reflectance values from Landsat 8 Band 10, Band 4, and Band 5 over the Black Forest region in Germany on July 29, 2021, first list the input TIFF files, then calculate NDVI and estimate land surface temperature (LST) using the single-channel method. Next, compute the maximum LST with... | B | [
"2.12 K",
"3.83 K",
"5.01 K",
"6.24 K"
] |
56 | Spectrum | Based on thermal Band 31 and Band 32 data over the Tokyo metropolitan area on August 10, 2022, first list the TIFF files, then estimate land surface temperature (LST) using the split-window method, and finally calculate the proportion of the area where LST is below 300K. | A | [
"8.82%",
"15.27%",
"23.41%",
"31.09%"
] |
57 | Spectrum | Based on thermal Band 31 and Band 32 data over the MurrayβDarling Basin in Australia during January 2023, first list the input TIFF files, then estimate land surface temperature (LST) using the split-window method. For each day, calculate the proportion of the area with LST values exceeding 310 K, and finally compute t... | B | [
"19.82%",
"29.75%",
"24.68%",
"21.05%"
] |
58 | Spectrum | Based on thermal Band 31 and Band 32 data over the Sahara Desert region in 2023, list the input TIFF files, estimate land surface temperature (LST) using the split-window algorithm, calculate the daily average LST, and count the number of days when the daily average LST exceeds 310K (extreme heat events). | C | [
"8 days",
"15 days",
"12 days",
"20 days"
] |
59 | Spectrum | Based on thermal Band 31 and Band 32 data over the Ganges Delta region in 2020, first list the input TIFF files, then estimate land surface temperature (LST) using the split-window method. Next, classify the data by season based on acquisition dates, and calculate the average LST for the autumn period (September to Nov... | C | [
"281.72 K",
"286.13 K",
"284.05 K",
"288.67 K"
] |
60 | Spectrum | Based on thermal Band 31 and Band 32 data over the Sahara Desert region from June to September 2018, list the input TIFF files, estimate land surface temperature (LST) using the split-window algorithm, and calculate the average LST over the entire four-month period. | C | [
"310.12 K",
"312.56 K",
"314.02 K",
"316.88 K"
] |
61 | Spectrum | Based on MODIS surface reflectance data of bands b02, b05, b17, b18, and b19 in Turpan, Xinjiang in July 2020, first list the input TIFF files, then estimate daily atmospheric water vapor using the band ratio method, and finally calculate the monthly mean for July. | C | [
8.7623,
13.5821,
11.391,
9.4456
] |
62 | Spectrum | Using MODIS surface reflectance from bands b02 (0.865 ΞΌm), b05 (1.240 ΞΌm), b17 (0.905 ΞΌm), b18 (0.936 ΞΌm), and b19 (0.940 ΞΌm), first list the input TIFF files, then estimate atmospheric absorption levels over the urban region of Hangzhou on August 10, 2021, using the band ratio method. Calculate the average atmospheric... | D | [
"12.47%",
"23.25%",
"44.13%",
"61.98%"
] |
63 | Spectrum | Using MODIS surface reflectance bands b02, b05, b17, b18, and b19 over the Loess Plateau region in July 2022, first list the input TIFF files, then apply the band ratio method to estimate daily atmospheric water vapor. Calculate the daily average values and finally compute the mean atmospheric water vapor for the entir... | C | [
8.4721,
12.3847,
10.9304,
9.6582
] |
64 | Spectrum | Using MODIS bands b02 (0.865 ΞΌm), b05 (1.240 ΞΌm), b17 (0.905 ΞΌm), b18 (0.936 ΞΌm), and b19 (0.940 ΞΌm), estimate daily atmospheric absorption over the coast of Guangdong from July 20 to 29, 2023, using the band ratio method. Calculate the daily average absorption, determine the mean absorption for the period, and count t... | B | [
2,
5,
6,
8
] |
65 | Spectrum | Using daily atmospheric absorption data derived from MODIS bands b02, b05, b17, b18, and b19 over the Huang-Huai-Hai Plain in 2023, first list the input TIFF files, then apply the band ratio method to estimate daily atmospheric water vapor. Calculate the average atmospheric water vapor for each month, group the months ... | D | [
2.5874,
3.2123,
4.0186,
5.1057
] |
66 | Spectrum | Process the TIF files in the working directory and calculate the percentage of pixels meeting the conditions. | C | [
"15.34%",
"28.67%",
"35.98%",
"41.13%"
] |
67 | Spectrum | On June 15, 2022, over the Los Angeles metropolitan area, use TES-derived LST and surface emissivity from ASTER Bands 10β14 to construct a pixel-wise thermal response index (LST/Ξ΅). Then calculate the regional average of this index to assess the typical heat retention characteristics of surface materials in the area. | B | [
338.15,
349.27,
"351,86",
355.82
] |
68 | Spectrum | Based on TES output from ASTER thermal bands on March 30, 2020, in the Sahara Desert region near Tamanrasset, Algeria, calculate the proportion of the area where emissivity variation (ΞΞ΅) exceeds 0.07. | D | [
"18.77%",
"59.87%",
"88.55%",
"100%"
] |
69 | Spectrum | Apply the TVDI method to NDVI and LST data from 2022 to detect dry areas (TVDI > 0.75) and compute their average land surface temperature. | B | [
"303.74 K (15187.00 * 0.02)",
"306.65 K (15332.75 * 0.02)",
"309.56 K (15478.00 * 0.02)",
"312.47 K (15623.50 * 0.02)"
] |
70 | Spectrum | Using temperature and vegetation data (NDVI and LST) from the agricultural region near Urumqi, Xinjiang in February 2022, first construct NDVIβLST scatter plots and apply the Temperature-Vegetation Dryness Index (TVDI) method to compute pixel-level dryness. Then, identify pixels where NDVI > 0.7 and calculate the avera... | A | [
"0.1066 (1066.16* 0.0001)",
"0.2056 (2056.32* 0.0001)",
"0.3182 (3182.45* 0.0001)",
"0.4548 (4548.12* 0.0001)"
] |
71 | Spectrum | Using ASTER Bands 10β12 data from December 23, 2022, apply the Three-Temperature Method (TTM) to retrieve pixel-wise LST over the specified region. Then calculate the 70th percentile temperature of all LST values in that region. | B | [
"275.15 K",
"277.90 K",
"279.34 K",
"281.79 K"
] |
72 | Spectrum | On December 23, 2022, using land surface temperature (LST) derived from the Three-Temperature Method (TTM) applied to ASTER Bands 10β12 (acquired at 10:30 AM local time), calculate the mean LST difference (ΞLST) between two vertically aligned regions that partially overlap in longitude (74.4Β°β75.1Β°E). | C | [
"21.69%",
"37.89%",
"41.71%",
"55.97% "
] |
73 | Spectrum | Using ASTER bands 10-12 data, calculate the Land Surface Temperature (LST) using the Three-Temperature Method (TTM) and calculate the maximum LST for the entire study area. | A | [
"307.70 K",
"308.70 K",
"309.70 K",
"310.70 K"
] |
74 | Spectrum | Using ASTER Bands 10β12 data on April 13, 2022, the Three-Temperature Method (TTM) was applied to estimate Land Surface Temperature (LST) in two Australian Outback regions. Calculate the absolute difference in the percentage of pixels where LST exceeds 295 K. | B | [
"1.51%",
"2.74%",
"3.96%",
"4.83%"
] |
75 | Spectrum | Based on land surface temperature (LST) retrieved using the Three-Temperature Method (TTM) from ASTER Bands 10β12 on August 1, 2020, over the defined Mediterranean coastal area near Barcelona, calculate the average daytime LST specifically within urban areas. | B | [
"292.69 K",
"293.31 K",
"295.93 K",
"296.84 K"
] |
76 | Spectrum | Calculate the average land surface temperature in the Taklamakan Desert area at 05:50 on February 23, 2020, and finally compute the percentage of pixels where LST exceeds 105% of this average. | B | [
"9.39%",
"13.09%",
"18.64%",
"23.67%"
] |
77 | Spectrum | Using split-window derived LST from Band 31 and Band 32 over Taklamakan, Xinjiang for June 2021, calculate the average surface temperature for early June (3β15) and late June (16β30), and determine the difference between these two averages. | D | [
"2.77K",
"5.64K",
"7.25K",
"8.22K"
] |
78 | Spectrum | Based on thermal Band 31 and 32 data acquired over irrigated farmland in northern Hebei on August 5, 2021, apply the split-window algorithm to estimate land surface temperature (LST). Classify the resulting temperature map into three thermal zones: low (< 295 K), medium (295β305 K), and high (> 305 K). Finally, calcula... | B | [
"31.39%",
"54.79%",
"62.74%",
"75.41%"
] |
79 | Spectrum | Using thermal Bands 31 and 32 over the urban area of Guangzhou during 2023, first list all relevant TIFF files from that year. Then, apply the split-window algorithm to compute daily land surface temperature (LST). Based on the results, calculate the average LST for each meteorological season (spring: MarchβMay, summer... | A | [
"2.33K",
"5.78K",
"7.75K",
"8.87K"
] |
80 | Spectrum | Based on thermal Bands 31 and 32 data from the central urban area of Wuhan on July 15, 2022, first list the relevant TIFF files, then apply the split-window algorithm to retrieve land surface temperature (LST). Define the high-temperature zone as pixels where LST exceeds 310 K, and the low-temperature zone as pixels wh... | C | [
"3.23%",
"5.29%",
"1.35%",
"10.52%"
] |
81 | Spectrum | Based on MODIS daytime and nighttime brightness temperature and emissivity data from Band 31 over the North American Great Plains in July 2023, calculate the average proportion of pixels each day where the daytime land surface temperature (LST) exceeds 315 K. This includes listing the relevant TIFF files, applying the ... | C | [
"8.94%",
"13.67%",
"16.01%",
"25.87%"
] |
82 | Spectrum | Using MODIS Day and Night brightness temperature and emissivity Band 31 data over the Ganges River Basin during January 2021, identify the number of days when over 35% of the region had daytime LST values greater than 310 K. | A | [
2,
5,
10,
13
] |
83 | Spectrum | Using MODIS daytime brightness temperature and emissivity (Band 31) data over Central California for July 5th in 2015 and 2023, list the relevant TIFF files, apply the MODIS daytime algorithm to derive land surface temperatures (LST) for each date, and compute the difference in average LST between the two years to asse... | B | [
"4.11 K",
"5.55 K",
"1.55 K",
"2.53 K"
] |
84 | Spectrum | Using MODIS daytime brightness temperature and emissivity (Band 31) data over the southern edge of the Sahara during July 2023, computing the daily proportion of pixels above 315 K, and finally calculating the average of these proportions over the month. | D | [
"18.94%",
"25.96%",
"37.86%",
"59.97%"
] |
85 | Spectrum | Calculate the monthly average LST for each year and then compute the difference in average monthly LST between July of 2015 and 2023 to analyze temperature changes over this period | A | [
"Increase of 6.93 K",
"Decrease of 6.93 K",
"No significant change (<0.2)",
"Increase of 3.47 K"
] |
86 | Spectrum | Calculate the difference in average Apparent Thermal Inertia (ATI) over the Mediterranean island of Cyprus between July 5 and July 10, 2020. | C | [
1.655,
2.697,
3.023,
4.844
] |
87 | Spectrum | Using Apparent Thermal Inertia (ATI) derived from satellite thermal bands and surface albedo, compute the monthly average ATI across the Sahel region for May 2023 | C | [
1.47,
2.52,
4.24,
5.82
] |
88 | Spectrum | Based on Apparent Thermal Inertia (ATI) derived from daytime and nighttime brightness temperatures and surface albedo in Californiaβs Central Valley during July 2022, calculate the proportion of pixels each day that exceed 115% of the monthly mean ATI value. | C | [
"15.87%",
"27.22%",
"33.01%",
"42.86%"
] |
89 | Spectrum | Based on Apparent Thermal Inertia (ATI) calculated from daytime and nighttime brightness temperature and surface albedo over the urban area of Beijing, China during July 2019, list the input TIFF files, compute ATI for each day, and calculate the average ATI value for the month. | C | [
1.8900000000000001,
2.25,
3.3,
4.75
] |
90 | Spectrum | Based on Apparent Thermal Inertia (ATI) calculated from daytime and nighttime brightness temperatures over California during the August 2022 wildfire events, list the input TIFF files, compute daily ATI, calculate the monthly mean ATI, and determine the average proportion of pixels with daily ATI values below 80% of th... | D | [
"9.89%",
"21.89%",
"33.59%",
"60.01%"
] |
91 | Spectrum | Calculate the proportion of pixels with TVDI > 0.7 in June and August 2023 over the Yellow River Basin, then compute the absolute difference between these two values. | C | [
"12.34%",
"23.45%",
"30.12%",
"45.67%"
] |
92 | Spectrum | Compute the average TVDI over the Central Valley of California during the summer months (June to August) of 2021 using NDVI and LST data. | C | [
0.3498,
0.5195000000000001,
0.6392,
0.7578
] |
93 | Spectrum | Using Landsat 8 Band 10 and reflectance bands (Red and NIR) over New York City in 2018, estimate land surface temperature with the NDVI-based single-channel method, and quantify the absolute difference between the overall mean LST and the mean LST in regions with NDVI greater than 0.7. | D | [
"8.92 K",
"10.50 K",
"14.54 K",
"18.75 K"
] |
94 | Spectrum | Using Landsat 8 Band 10 and reflectance bands (Red and NIR) over New York City for April 2018 and April 2019, estimate land surface temperature with the NDVI-based single-channel method. Calculate the mean LST for each April and determine the absolute difference between the two values. | C | [
"3.65 K",
"4.55 K",
"5.41 K",
"6.10 K"
] |
95 | Spectrum | Using MODIS bands over the Turpan region in March and August 2020, estimate atmospheric water vapor via the band ratio method and quantify the absolute difference between the monthly mean values. | B | [
3.6433,
4.2064,
4.9695,
5.1326
] |
96 | Spectrum | Estimate daily atmospheric water vapor using the band ratio method applied to MODIS surface reflectance bands b02, b05, b17, b18, and b19 over the Loess Plateau in January 2018 and January 2022. Determine the 70th percentile of daily averages for each year, and compute their absolute difference to quantify the interann... | B | [
1.3227,
2.8781,
3.5892,
4.6433
] |
97 | Spectrum | Based on daily atmospheric absorption indicators derived from MODIS b02, b05, b17, b18, and b19 over the Huang-Huai-Hai Plain in 2023, estimate daily atmospheric water vapor using the band ratio method. Compute the annual average and the summer (JuneβAugust) average, then calculate the absolute difference to assess sea... | B | [
1.67,
3.01,
5.94,
6.43
] |
98 | Spectrum | Over the Yellow River Basin in August 2023, calculate TVDI using NDVI and LST data. Identify all pixels with TVDI > 0.7, then compute the mean NDVI of these pixels to assess vegetation status in drought-affected regions. | C | [
"0.4588 (4588 * 0.0001)",
"0.5165 (5165 * 0.0001)",
"0.6121 (6121 * 0.0001)",
"0.7077 (7077 * 0.0001)"
] |
99 | Spectrum | Using Landsat 8 Band 10 and reflectance bands (Red and NIR) over New York City for JuneβJuly of 2020 and 2021, estimate LST using the NDVI-based single-channel method. Compute the proportion of pixels with LST > 305 K for each year, then calculate the absolute difference between the two yearly values. | A | [
"0.80%",
"0.50%",
"1.50%",
"1.80%"
] |
100 | Spectrum | Using Landsat 8 Band 10 and reflectance bands (Red and NIR) for October 22, 2021, estimate LST with the NDVI-based single-channel method. Then calculate the proportion of pixels meeting both conditions: LST > 290 K and NDVI > 0.6. | B | [
"1.35%",
"3.27%",
"4.15%",
"5.25%"
] |
Earth-Bench-V2
Earth-Bench-V2 evaluates Earth observation agents on 248 task cores with prepared observations, reference tool trajectories, and final-answer annotations. Tasks cover spectral analysis, remote sensing products, and RGB perception.
This release continues the Earth-Bench benchmark introduced in Earth-Agent. Its annotation file includes both Instruction Following (IF) and Autonomous Planning (AP) evaluation entries for each task. Earth-Agent-Pro studies these prepared-input regimes alongside Open-World Execution (OW). The companion OW release is Earth-Bench-OW.
The local release name is Earth-Bench-V2; the Pro paper calls the full three-regime benchmark Earth-Bench-Pro. This repository contains the prepared-input portion, with 248 task records and 496 IF/AP evaluation entries.
Papers and code
- Earth-Agent: Unlocking the Full Landscape of Earth Observation with Agents (ICLR 2026).
- Earth-Agent-Pro: Towards Real-World Full-Chain Earth Observation with Agents.
- Earth-Agent code and evaluation framework.
Task coverage
| Modality | Task IDs | Task cores |
|---|---|---|
| Spectrum | 1β100 | 100 |
| Products | 101β188 | 88 |
| RGB | 189β248 | 60 |
| Total | 1β248 | 248 |
Task IDs match the companion release. The number of local files reflects this snapshot; it is not the number of questions or evaluation instances.
Updated benchmark results
The following measurements use the updated Earth-Bench-V2 benchmark.
| Modality | Model | Acc (%) | Eff | TAO (%) | TIO (%) | TEM (%) | Param (%) |
|---|---|---|---|---|---|---|---|
| Spectrum | GPT-5 | 59.00 | 2.0121 | 66.65 | 61.64 | 32.39 | 21.61 |
| Spectrum | Qwen3-Max | 50.00 | 2.9887 | 70.10 | 57.14 | 8.02 | 11.36 |
| Products | GPT-5 | 83.54 | 1.4616 | 57.78 | 45.60 | 32.72 | 18.64 |
| Products | Qwen3-Max | 68.18 | 1.4877 | 70.10 | 73.85 | 38.62 | 25.89 |
| RGB | GPT-5 | 75.00 | 1.8253 | 82.89 | 77.82 | 48.13 | 42.21 |
| RGB | Qwen3-Max | 38.33 | 0.8607 | 59.67 | 38.33 | 35.25 | 36.67 |
| All | GPT-5 | 71.13 | 1.7716 | 67.43 | 59.86 | 36.31 | 25.54 |
| All | Qwen3-Max | 53.69 | 1.9370 | 68.90 | 54.85 | 25.54 | 21.20 |
Acc: Accuracy; Eff: Efficiency; TAO: Tool-Any-Order; TIO: Tool-In-Order; TEM: Tool-Exact-Match; Param: Parameter Accuracy.
Repository layout
Earth-Bench-V2/
βββ README.md
βββ LICENSE
βββ THIRD_PARTY_NOTICES.md
βββ task_index.jsonl
βββ question.json
βββ data/question1/ ... data/question248/
βββ model_results.csv
βββ model_out/
βββ tools/
| Component | Contents |
|---|---|
question.json |
A JSON object keyed by task IDs "1" through "248"; 248 records. |
data/ |
13,523 prepared input files, organized by task ID. |
dialogs |
User request, reference assistant/tool interactions, and final answer. |
choices |
Candidate answers for 247 tasks; task 163 has null and a numeric reference answer. |
evaluation |
Two entries per task: IF and AP; includes question, ground-truth whitelist/blacklist, metric, and regime. |
tools, files |
Reserved fields; both are null in this release. |
model_results.csv is a semicolon-delimited expert-model response table with columns file_path, model, text_prompt, bbox, and result. model_out/ holds 26 stored output masks used by the perception tools. These files support replay and are not leaderboard scores.
task_index.jsonl provides one derived row per task for browsing: question_id, modality, question, reference_answer, and choices. The original JSON file remains the source of truth for trajectories, acquisition specifications, and evaluation details. This release provides a single test index and no official training split.
Download
Install huggingface_hub, then download from the Hub. The full snapshot occupies approximately 15.1 GB.
from huggingface_hub import snapshot_download
snapshot_download(
repo_id="LvZTTTT/Earth-Bench-V2",
repo_type="dataset",
local_dir="benchmark",
)
For annotations only:
snapshot_download(
repo_id="LvZTTTT/Earth-Bench-V2",
repo_type="dataset",
local_dir="benchmark",
allow_patterns=["README.md", "question.json", "task_index.jsonl"],
)
Read the annotations
import json
from pathlib import Path
questions = json.loads(Path("benchmark/question.json").read_text())
example = questions["1"]
request = example["dialogs"][0]["content"]
reference_trajectory = example["dialogs"][1:-1]
reference_answer = example["dialogs"][-1]["content"]
evaluation = example["evaluation"]
Launch tools from a working directory where benchmark/ resolves to the downloaded repository. The bundled MCP configuration uses tools/... paths; either install those scripts under your framework's tools/ directory or update the configuration to their actual paths. Configure the output directory consistently with the reference benchmark/out/... paths.
Evaluation and reproducibility
Use the papers for the regime definitions, final-answer evaluation, and trajectory metrics. The original Earth-Agent framework provides evaluation code; integration of this snapshot requires selecting the correct annotation file, regime, data paths, and tool implementation. This dataset repository does not include an end-to-end evaluation runner.
- Use prepared inputs for IF/AP. For IF, expose the prescribed tool sequence according to the evaluation protocol; for AP, hide that sequence and let the agent plan. Never expose reference answers or reference tool outputs to the evaluated agent.
- Ground-truth regime labels vary in capitalization; normalize them when parsing.
- Task 163 requests 2022-09-12, but its reference input filenames contain 2020-09-12. The original annotation is preserved. Record any correction or exclusion when reporting scores.
Intended use
Use this benchmark to evaluate scientific Earth observation workflows, tool selection, argument grounding, and final-answer quality. The released trajectories and answers are evaluation references. Disclose any use of them for training or prompt construction before reporting benchmark performance.
License and sources
Benchmark annotations and release documentation are licensed under CC BY-NC 4.0. Attribute the benchmark and cite the relevant papers. Third-party satellite products, RGB imagery, and inherited code retain their original terms; see THIRD_PARTY_NOTICES.md. The benchmark license does not replace those terms.
Citation
Please cite both papers when using these matched benchmark releases.
@article{feng2025earthagent,
title = {Earth-Agent: Unlocking the Full Landscape of Earth Observation with Agents},
author = {Feng, Peilin and Lv, Zhutao and Ye, Junyan and Wang, Xiaolei and Huo, Xinjie and Yu, Jinhua and Xu, Wanghan and Zhang, Wenlong and Bai, Lei and He, Conghui and Li, Weijia},
journal = {arXiv preprint arXiv:2509.23141},
year = {2025},
url = {https://arxiv.org/abs/2509.23141}
}
@article{lv2026earthagentpro,
title = {Earth-Agent-Pro: Towards Real-World Full-Chain Earth Observation with Agents},
author = {Lv, Zhutao and Dang, Chenhao and Feng, Yi and Gong, Yanpei and Wang, Xiaolei and Ye, Junyan and He, Conghui and Li, Weijia},
journal = {arXiv preprint arXiv:2609.12533},
year = {2026},
url = {https://arxiv.org/abs/2609.12533}
}
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